text: Fort Mountain stands within the watershed of the Penobscot River, which drains into Penobscot Bay.  The south and east sides of Fort Mountain drain into Wassataquoik Stream, then into the East Branch of the Penobscot River.  The northeast side of Fort Mountain drains into Annis Brook, then into Wassataquoik Stream.  The northwest side of Fort drains into Little Nesowadnehunk Stream, then into Nesowadnehunk Stream, and the West Branch of the Penobscot River.

text: Fort Mountain stands within the

entity_name: Drainage basin

text: watershed

text: of the

entity_name: Penobscot River

text: Penobscot River

text: , which drains into

entity_name: Penobscot Bay

text: Penobscot Bay

text: .  The south and east sides of Fort Mountain drain into

text: Wassataquoik Stream

text: , then into the

entity_name: East Branch Penobscot River

text: East Branch

text: of the Penobscot River.  The northeast side of Fort Mountain drains into Annis Brook, then into Wassataquoik Stream.  The northwest side of Fort drains into Little Nesowadnehunk Stream, then into Nesowadnehunk Stream, and the

entity_name: West Branch Penobscot River

text: West Branch

text: of the Penobscot River.

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answers: NDQ_006069

answers: Wassataquoik Stream

text: Generally stream flows from north to the south. Most of the streams drain into Kabul river. Kalpani, an important stream of the district rises in the Baizai and flowing southwards join Kabul river. Other important streams which join Kalpani are Baghiari Khawar on the west and Muqam Khawar, coming from Sudham valley and Naranji Khawar from the Narangi hills on the left.

text: Generally stream flows from north to the south. Most of the streams drain into Kabul river. Kalpani, an important stream of the district rises in the Baizai and flowing southwards join Kabul river. Other important streams which join Kalpani are Baghiari Khawar on the west and Muqam Khawar, coming from Sudham valley and Naranji Khawar from the Narangi hills on the left.

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answers: Kabul river

text: The surveyed route crossed hundreds of streams and rivers. To cross these with the pipeline, engineers designed concrete "jackets" to surround the pipe and weight it down so it would sink to the bottom of the stream or river. Because oil is lighter than water, the pipeline would float without the concrete jackets. Dredging rivers and burying the pipeline in the streambed was not allowed due to environmental concerns. In several places—either out of fear of disturbing the river or because of the river's characteristics—pipeline bridges were constructed. The most notable of these are over the Yukon River and the Tanana River. To protect against corrosion in these wet environments, the pipeline was designed with cathodic protection.

text: The surveyed route crossed hundreds of streams and rivers. To cross these with the pipeline, engineers designed concrete "jackets" to surround the pipe and weight it down so it would sink to the bottom of the stream or river. Because oil is lighter than water, the pipeline would float without the concrete jackets. Dredging rivers and burying the pipeline in the streambed was not allowed due to environmental concerns. In several places—either out of fear of disturbing the river or because of the river's characteristics—pipeline bridges were constructed. The most notable of these are over the

entity_name: Yukon River

text: Yukon River

text: and the

entity_name: Tanana River

text: Tanana River

text: . To protect against corrosion in these wet environments, the pipeline was designed with

entity_name: Cathodic protection

text: cathodic protection

method: Bert-ConvKNRM

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answers: NDQ_006065

answers: because of the river's characteristics

answers: NDQ_006066

answers: west side of the continental divide

answers: NDQ_006067

answers: It was not allowed due to environmental concerns

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answers: Dredging rivers and burying the pipeline in the streambed was not allowed

text: The fluvial landforms of streams, stream beds, and river valleys have various landforms.

text: The

entity_name: Fluvial

text: fluvial landform

text: s of

entity_name: Stream

text: stream

text: s,

entity_name: Stream bed

text: stream bed

text: s, and

text: river valley

text: s have various landforms.

method: Bert-DRMMTKS

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text: The Heart River is a  river in the U.S. state of Wyoming, tributary to the Snake River. Its entire course is contained inside Yellowstone National Park. The river rises on the Continental Divide, in the Rocky Mountains, a few miles southeast of Yellowstone Lake. Its headwater streams flow into Heart Lake, from whose southeastern end the main Heart River issues, receiving two tributary streams from the northeast and flowing southwest into a short but steep gorge. It then continues generally south for roughly  before emptying into the Snake near the boundary with the Teton National Forest.

text: The Heart River is a  river in the

entity_name: U.S. state

text: U.S. state

text: of

entity_name: Wyoming

text: Wyoming

text: , tributary to the

entity_name: Snake River

text: Snake River

text: . Its entire course is contained inside

entity_name: Yellowstone National Park

text: Yellowstone National Park

text: . The river rises on the

entity_name: Continental Divide of the Americas

text: Continental Divide

text: , in the

entity_name: Rocky Mountains

text: Rocky Mountains

text: , a few miles southeast of

entity_name: Yellowstone Lake

text: Yellowstone Lake

text: . Its headwater streams flow into

entity_name: Heart Lake (Wyoming)

text: Heart Lake

text: , from whose southeastern end the main Heart River issues, receiving two tributary streams from the northeast and flowing southwest into a short but steep gorge. It then continues generally south for roughly  before emptying into the Snake near the boundary with the

entity_name: Teton National Forest

text: Teton National Forest

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text: New Jersey rivers includes streams formally designated as rivers.  There are also smaller streams (i.e., branches, creeks, drains, forks, licks, runs, etc.) in the state.  Major rivers include the Manasquan, Maurice, Mullica, Passaic, Rahway, Raritan, Musconetcong, and Delaware rivers.  Historically, the Delaware and Raritan rivers have provided transportation of goods and people inland from the Atlantic Ocean, and were once connected by the Delaware and Raritan Canal.  Today, these rivers, and the streams that feed them, provide sport and recreation for many people. The Raritan River in Middlesex County is often considered the borderline between North and South/Central Jersey, although it is not official.

text: New Jersey rivers includes streams formally designated as

entity_name: River

text: river

text: s.  There are also smaller streams (i.e., branches, creeks, drains, forks, licks, runs, etc.) in the state.  Major rivers include the

entity_name: Manasquan River

text: Manasquan

entity_name: Maurice River

text: Maurice

entity_name: Mullica River

text: Mullica

entity_name: Passaic River

text: Passaic

entity_name: Rahway River

text: Rahway

entity_name: Raritan River

text: Raritan

entity_name: Musconetcong River

text: Musconetcong

text: , and

entity_name: Delaware River

text: Delaware

text: rivers.  Historically, the Delaware and Raritan rivers have provided transportation of goods and people inland from the

entity_name: Atlantic Ocean

text: Atlantic Ocean

text: , and were once connected by the

entity_name: Delaware and Raritan Canal

text: Delaware and Raritan Canal

text: .  Today, these rivers, and the streams that feed them, provide sport and recreation for many people. The Raritan River in

entity_name: Middlesex County, New Jersey

text: Middlesex County

text: is often considered the borderline between North and South/Central Jersey, although it is not official.

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text: With the announcement of the line up change on 5 June 2012 the band released the first single from the album, "Bleed". The song was uploaded to their YouTube to stream as well as made a free download. BBC Radio 1 DJ Zane Lowe said the song is "Easlily the best thing the band have ever done." The second single "The Road" was streamed exclusively through Revolver magazine's website on 6 August 2012. Two days prior to the single's stream, the band released a video of the making of the music video for "The Road". The song was made Q magazine's "Track of the Day". On 30 August the band debuted a third track, "Golden Gate", as promotion for the album by making it available to stream on YouTube, but was released exclusively through German website Stage Load.

text: With the announcement of the line up change on 5 June 2012 the band released the first single from the album, "Bleed". The song was uploaded to their YouTube to stream as well as made a free download.

entity_name: BBC Radio 1

text: BBC Radio 1

text: DJ

entity_name: Zane Lowe

text: Zane Lowe

text: said the song is "Easlily the best thing the band have ever done." The second single "The Road" was streamed exclusively through

entity_name: Revolver (magazine)

text: Revolver

text: magazine's website on 6 August 2012. Two days prior to the single's stream, the band released a video of the making of the music video for "The Road". The song was made

entity_name: Q (magazine)

text: Q

text: magazine's "Track of the Day". On 30 August the band debuted a third track, "Golden Gate", as promotion for the album by making it available to stream on YouTube, but was released exclusively through German website Stage Load.

method: ICT-DRMMTKS

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answers: the band released the first single from the album, "Bleed"

text: Juarez Street is one of the few through streets on the surface. It is filled with stores and restaurants and has a constant flow of people and traffic. The other through streets of town are either partially or fully underground, following the old drainage ditches and tunnels dug during colonial times. Originally they were used for flood control, but modern dams have controlled flooding and left them dry, so they have been turned into thoroughfares in a city with little surface area. The most important of these roads is Miguel Hidalgo or Belaunzarán, which carried the runoff from the river that used to divide the city in two. Guanajuato’s version of the La Llorona story has the woman wandering the its tunnels, some of which had rivers or streams running through them.

text: Juarez Street is one of the few through streets on the surface. It is filled with stores and restaurants and has a constant flow of people and traffic. The other through streets of town are either partially or fully underground, following the old drainage ditches and tunnels dug during colonial times. Originally they were used for flood control, but modern dams have controlled flooding and left them dry, so they have been turned into thoroughfares in a city with little surface area. The most important of these roads is Miguel Hidalgo or Belaunzarán, which carried the runoff from the river that used to divide the city in two. Guanajuato’s version of the

entity_name: La Llorona

text: La Llorona

text: story has the woman wandering the its tunnels, some of which had rivers or streams running through them.

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answers: NDQ_006065

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answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: Guanajuato

answers: NDQ_006068

answers: rivers or streams

answers: NDQ_006069

answers: a city with little surface area

text: The South Branch Blackwater River is an  river in Aroostook County, Maine. From its source () in Maine Township 9, Range 3, WELS, the stream runs northwest to its confluence with the North Branch to form the Blackwater River in Squa Pan Township (T. 10, R. 4, WELS). Via the Blackwater River, St. Croix Stream, and the Aroostook River, the South Branch is part of the Saint John River watershed.

text: The South Branch Blackwater River is an  river in

entity_name: Aroostook County, Maine

text: Aroostook County

entity_name: Maine

text: Maine

text: . From its source () in Maine Township 9, Range 3, WELS, the stream runs northwest to its

entity_name: Confluence

text: confluence

text: with the

entity_name: North Branch Blackwater River (Maine)

text: North Branch

text: to form the

entity_name: Blackwater River (Maine)

text: Blackwater River

text: in Squa Pan Township (T. 10, R. 4, WELS). Via the Blackwater River,

entity_name: St. Croix Stream

text: St. Croix Stream

text: , and the

entity_name: Aroostook River

text: Aroostook River

text: , the South Branch is part of the

entity_name: Saint John River (Bay of Fundy)

text: Saint John River

text: watershed.

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answers: Blackwater River

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Saint John River

answers: NDQ_006063

answers: WELS

answers: NDQ_006064

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answers: from its source

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answers: NDQ_006067

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answers: NDQ_006068

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answers: NDQ_006069

answers: Blackwater River

text: The river banks are extensively landscaped and act as an urban green space for communities along its length.  Close to the source of the river in Setagaya, the river is divided vertically between a large underground storm drain and surface level landscaped ornamental stream. At Ōhashi Junction where the river passes under the Route 246 and the Tōmei Expressway, the river re-emerges as a broader, surface level water channel.

text: The river banks are extensively landscaped and act as an urban green space for communities along its length.  Close to the source of the river in

entity_name: Setagaya

text: Setagaya

text: , the river is divided vertically between a large underground storm drain and surface level landscaped ornamental stream. At

entity_name: Meguro Sky Garden

text: Ōhashi Junction

text: where the river passes under the

entity_name: Japan National Route 246

text: Route 246

text: and the

entity_name: Tōmei Expressway

text: Tōmei Expressway

text: , the river re-emerges as a broader, surface level water channel.

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answers: underground

answers: NDQ_006064

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answers: NDQ_006065

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answers: NDQ_006066

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answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: urban green space

answers: NDQ_006069

answers: the Central Valley of California

text: The eastern drainage divide of the Sweetwater watershed lies on the main divide of the Cuyamacas, which also separates streams of the Pacific slope from streams draining to the endorheic basin of the Salton Sea farther to the east. To the north, the Sweetwater basin shares borders with those of the San Diego River and the smaller streams that drain portions of National City and San Diego. On the south, it is bordered by the Otay River and Tijuana River drainages – specifically for the Tijuana, the subwatershed of Cottonwood Creek, the river's main tributary in the U.S.

text: The eastern drainage divide of the Sweetwater watershed lies on the main divide of the Cuyamacas, which also separates streams of the Pacific slope from streams draining to the

entity_name: Endorheic basin

text: endorheic basin

text: of the

entity_name: Salton Sea

text: Salton Sea

text: farther to the east. To the north, the Sweetwater basin shares borders with those of the

entity_name: San Diego River

text: San Diego River

text: and the smaller streams that drain portions of National City and San Diego. On the south, it is bordered by the

entity_name: Otay River

text: Otay River

text: and

entity_name: Tijuana River

text: Tijuana River

text: drainages – specifically for the Tijuana, the subwatershed of Cottonwood Creek, the river's main tributary in the U.S.

method: UNH-tfidf-stem

method: UNH-tfidf-ptsim

method: UNH-tfidf-lem

method: UNH-qee

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answers: the eastern drainage divide

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Salton Sea

answers: NDQ_006063

answers: Pacific slope

answers: NDQ_006064

answers: watershed

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answers: Pacific

answers: NDQ_006067

answers: Salton Sea

answers: NDQ_006068

answers: San Diego River

answers: NDQ_006069

answers: San Diego

text: This fish is silvery in colour and can grow to 80 cm length. It lives in clear, flowing water, particularly in middle stretches of the main branches of rivers and streams. On the other hand, it is also found in short coastal streams. After spawning it moves to the sea but stays near the river mouths, or in the lower stretches of rivers. It migrates upstream to breed in October-Nowember.

text: This fish is silvery in colour and can grow to 80 cm length. It lives in clear, flowing water, particularly in middle stretches of the main branches of rivers and streams. On the other hand, it is also found in short coastal streams. After spawning it moves to the sea but stays near the river mouths, or in the lower stretches of rivers. It migrates upstream to breed in October-Nowember.

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answers: rivers and streams

answers: NDQ_006069

answers: It lives in clear, flowing water

text: Lake Rotorua is fed with water from a number of rivers and streams; some such as the Utuhina flow water of a water temperature warmer than the lake due to the thermal activity in the Rotorua area. Conversely streams on the northern shore such as the Hamurana Spring and the Awahou stream flow crystal clear water that has a constant temperature of 10 degrees Celsius. Other notable tributaries include the Ngongotaha stream, famous for trout fishing.

text: Lake Rotorua is fed with water from a number of rivers and streams; some such as the Utuhina flow water of a water temperature warmer than the lake due to the thermal activity in the Rotorua area. Conversely streams on the northern shore such as the

entity_name: Hamurana Springs

text: Hamurana Spring

text: and the Awahou stream flow crystal clear water that has a constant temperature of 10 degrees Celsius. Other notable tributaries include the

entity_name: Ngongotaha

text: Ngongotaha

text: stream, famous for trout fishing.

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answers: NDQ_006063

answers: 10 degrees Celsius

answers: NDQ_006064

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answers: NDQ_006065

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answers: NDQ_006066

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answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: rivers and streams

answers: NDQ_006069

answers: Lake Rotorua

text: Mathematically, the process of constructing a flownet consists of contouring the two harmonic or analytic functions of potential and stream function. These functions both satisfy the Laplace equation and the contour lines represent lines of constant head (equipotentials) and lines tangent to flowpaths (streamlines).  Together, the potential function and the stream function form the complex potential, where the potential is the real part, and the stream function is the imaginary part.

text: Mathematically, the process of constructing a flownet consists of

entity_name: Contour line

text: contour

text: ing the two harmonic or

entity_name: Analytic function

text: analytic function

text: s of potential and

text: stream function

text: . These functions both satisfy the

text: Laplace equation

text: and the contour lines represent lines of constant head (equipotentials) and lines tangent to flowpaths (streamlines).  Together, the potential function and the stream function form the

text: complex potential

text: , where the potential is the real part, and the stream function is the imaginary part.

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answers: streamlines

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answers: NDQ_006066

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answers: NDQ_006067

answers: These functions both satisfy the Laplace equation

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: These functions both satisfy the Laplace equation

text: Pacific Creek is a stream in the U.S. state of Wyoming.  The approximately  long stream rises on the western side of South Pass and flows into the Little Sandy Creek near Farson, Wyoming.  As the name implies, the stream starts just to the west of the Continental Divide and so is on the "Pacific" side of the divide.  The waters from the stream eventually flow into the Pacific ocean via the Green River and Colorado River.  The stream is a notable landmark on the Oregon, California and Mormon emigration trails.

text: Pacific Creek is a stream in the

text: U.S. state

text: of

text: Wyoming

text: .  The approximately  long stream rises on the western side of

text: South Pass

text: and flows into the Little Sandy Creek near

text: Farson, Wyoming

text: .  As the name implies, the stream starts just to the west of the

text: Continental Divide

text: and so is on the "

text: Pacific

text: " side of the divide.  The waters from the stream eventually flow into the Pacific ocean via the

text: Green River

text: and

text: Colorado River

text: .  The stream is a notable landmark on the

text: Oregon

text: California

text: and

text: Mormon

text: emigration trails.

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text: This is a list of streams and rivers in the U.S. state of Pennsylvania.

text: This is a list of streams and rivers in the

text: U.S. state

text: of

text: Pennsylvania

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answers: List of streams and rivers in the United States

text: The northeast side of Mt. Abraham is drained by Rapid Stream, then into the West Branch of the Carrabassett River, the Kennebec River, and into the Gulf of Maine. The southern half of the southwest side drains into Quick Stream, then into the West Branch. The northern half drains into Perham Stream, then into Orbeton Stream, and the Sandy River, another tributary of the Kennebec.

text: The northeast side of Mt. Abraham is drained by Rapid Stream, then into the

text: West Branch

text: of the

text: Carrabassett River

text: , the

text: Kennebec River

text: , and into the

text: Gulf of Maine

text: . The southern half of the southwest side drains into Quick Stream, then into the West Branch. The northern half drains into Perham Stream, then into Orbeton Stream, and the

text: Sandy River

text: , another

text: tributary

text: of the Kennebec.

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answers: the Kennebec River

text: Water the town river Las Cañas, Acelhuate, Tapachula, Chantecuán, El Sauce, and Chagiiite Sumpa and Arenal streams, and other unnamed Aposento. The main rivers are the reeds and the Acelhuate.The river Las Cañas was born in the town of Ilopango, and enters Soyapango to 2.4 miles east of the city, describing a path from south to north. Its course and divided the territory and Tonacatepeque Ilopango. Its rivers tributaries Chantecuán, El Sauce, Zapotitán, bananas and Sumpa, and streams and Arenal The Pavas Seco. It has a length within the municipality of 5.5 kilometers.Acelhuate River rises in the municipality of San Salvador. Enter Soyapango to 2.3 miles west of the city, describing a course from south to north. Its course divides this territory and those of Delgado and San Salvador. Its tributaries to the river gorge Tapachula and El Arenal. Describes a trip within the municipality of 3.5 kilometers.

text: Water the town river Las Cañas, Acelhuate, Tapachula, Chantecuán, El Sauce, and Chagiiite Sumpa and Arenal streams, and other unnamed Aposento. The main rivers are the reeds and the Acelhuate.The river Las Cañas was born in the town of Ilopango, and enters Soyapango to 2.4 miles east of the city, describing a path from south to north. Its course and divided the territory and Tonacatepeque Ilopango. Its rivers tributaries Chantecuán, El Sauce, Zapotitán, bananas and Sumpa, and streams and Arenal The Pavas Seco. It has a length within the municipality of 5.5 kilometers.Acelhuate River rises in the municipality of San Salvador. Enter Soyapango to 2.3 miles west of the city, describing a course from south to north. Its course divides this territory and those of Delgado and San Salvador. Its tributaries to the river gorge Tapachula and El Arenal. Describes a trip within the municipality of 3.5 kilometers.

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answers: Acelhuate River rises in the municipality of San Salvador

text: C++ input/output streams are primarily defined by iostream, a header file that is part of the C++ standard library (the name stands for Input/Output Stream).  In C++ and its predecessor, the C programming language, there is no special syntax for streaming data input or output. Instead, these are combined as a library of functions. Like the cstdio header inherited from C's stdio.h, iostream provides basic input and output services for C++ programs. iostream uses the objects cin, cout, cerr, and clog for sending data to and from the standard streams input, output, error (unbuffered), and log (buffered) respectively. As part of the C++ standard library, these objects are a part of the std namespace.

text: C++

text: input/output

text: streams are primarily defined by iostream, a

text: header file

text: that is part of the

text: C++ standard library

text: (the name stands for Input/Output Stream).  In C++ and its predecessor, the

text: C programming language

text: , there is no special syntax for streaming data input or output. Instead, these are combined as a

text: library

text: of

text: functions

text: . Like the cstdio header inherited from C's

text: stdio.h

text: , iostream provides basic input and output services for C++ programs. iostream uses the

text: object

text: s cin, cout, cerr, and clog for sending data to and from the

text: standard streams

text: input, output, error (unbuffered), and log (buffered) respectively. As part of the C++

text: standard library

text: , these objects are a part of the std

text: namespace

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text: The spring marks the southern end of a cave system which transports water from the western end of the Swabian Jura. Most of the water is derived from the River Danube and is obtained where the latter river disappears underground at the Donauversickerung (Danube Sinkhole) near Immendingen and Fridingen. Strangely, the Danube flows eastwards into the Black Sea, whereas the Rhine flows northwards to the North Sea. Therefore the water of the Aach flows under the European continental divide. This is a relatively common feature of karst stream captures.

text: The spring marks the southern end of a cave system which transports water from the western end of the Swabian Jura. Most of the water is derived from the

text: River Danube

text: and is obtained where the latter river disappears underground at the Donauversickerung (

text: Danube Sinkhole

text: ) near

text: Immendingen

text: and

text: Fridingen

text: . Strangely, the

text: Danube

text: flows eastwards into the

text: Black Sea

text: , whereas the Rhine flows northwards to the

text: North Sea

text: . Therefore the water of the Aach flows under the European continental divide. This is a relatively common feature of karst

text: stream capture

text: s.

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text: In addition to many small unnamed streams, the Fresno River receives the water from the following streams:

text: In addition to many small unnamed streams, the Fresno River receives the water from the following streams:

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text: The Grebe River is a river in Fiordland, New Zealand. It arises north-west of Lake Monowai in an area once part of the lake but cut off by an enormous landslide about 13,000 years ago. The river now flows north, between the Townley Mountains to the west, and the Hunter Mountains to the east, and into Lake Manapouri's South Arm. Its major tributaries are Jaquiery Stream, Florence Stream, Emerald Stream, and Percy Stream, all from the west.

text: The Grebe River is a river in

text: Fiordland

text: New Zealand

text: . It arises north-west of

text: Lake Monowai

text: in an area once part of the lake but cut off by an enormous landslide about 13,000 years ago. The river now flows north, between the

text: Townley Mountains

text: to the west, and the

text: Hunter Mountains

text: to the east, and into

text: Lake Manapouri

text: 's South Arm. Its major tributaries are Jaquiery Stream, Florence Stream, Emerald Stream, and Percy Stream, all from the west.

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answers: Lake Manapouri's South Arm

text: Visual stimuli have been known to process through the brain via two streams: the dorsal stream and the ventral stream.  The dorsal pathway is commonly referred to as the ‘where’ system; this allows the processing of location, distance, position, and motion.  This pathway spreads from the primary visual cortex dorsally to the parietal lobe.  Information then feeds into the motor cortex of the frontal lobe.  The second pathway, the ventral stream, processes information relating to shape, size, objects, orientation, and text.  This is commonly known as the ‘what’ system.  Visual stimuli in this system process ventrally from the primary visual cortex to the medial temporal lobe.  In childhood development, vision for action and vision for perception develop at different rates, proving the hypothesis of two distinct, linear streams for visual processing.  This acknowledges the potential of having two, independent streams.

text: Visual stimuli have been known to process through the brain via two streams: the

text: dorsal stream

text: and the

text: ventral stream

text: .  The dorsal pathway is commonly referred to as the ‘where’ system; this allows the processing of location, distance, position, and motion.  This pathway spreads from the

text: primary visual cortex

text: dorsally to the

text: parietal lobe

text: .  Information then feeds into the

text: motor cortex

text: of the frontal lobe.  The second pathway, the ventral stream, processes information relating to shape, size, objects, orientation, and text.  This is commonly known as the ‘what’ system.  Visual stimuli in this system process ventrally from the primary visual cortex to the

text: medial temporal lobe

text: .  In childhood development, vision for action and vision for perception develop at different rates, proving the hypothesis of two distinct, linear streams for visual processing.  This acknowledges the potential of having two, independent streams.

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answers: Visual stimuli have been known to process through the brain via two streams

text: Abura-Dunkwa is low-lying with loose quaternary sands and it rises up to 80 metres above sea level. The town is drained by a number of rivers and streams, including the Offin River, Birim River and small streams.

text: Abura-Dunkwa is low-lying with loose quaternary sands and it rises up to 80 metres above sea level. The town is drained by a number of rivers and

text: stream

text: s, including the

text: Offin River

text: Birim River

text: and small streams.

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answers: rivers and streams

text: Another meaning for "gut" in geography is a small creek, and this is seen in proper names in eastern North America from the Mid-Atlantic states (for instance, The Gut in Pennsylvania, Ash Gut in Delaware, and other streams) down into the Caribbean (for instance Guinea Gut, Fish Bay Gut, Cob Gut, Battery Gut and other rivers and streams in the United States Virgin Islands, in many rivers and streams of the Dutch Caribbean, and in Jamaica (Sandy Gut, Bens Gut River, White Gut River)).

text: Another meaning for "gut" in geography is a small creek, and this is seen in proper names in eastern North America from the Mid-Atlantic states (for instance,

entity_name: Spring Run (West Branch Susquehanna River)

text: The Gut

text: in Pennsylvania, Ash Gut in Delaware, and other streams) down into the Caribbean (for instance

text: Guinea Gut

text: Fish Bay Gut

text: Cob Gut

text: Battery Gut

text: and

entity_name: List of rivers of the United States Virgin Islands

text: other rivers and streams

text: in the

text: United States Virgin Islands

text: , in

entity_name: List of rivers of the Netherlands Antilles

text: many rivers and streams

text: of the

text: Dutch Caribbean

text: , and in Jamaica (Sandy Gut, Bens Gut River, White Gut River)).

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text: In the application of the Strahler stream order to hydrology, each segment of a stream or river within a river network is treated as a node in a tree, with the next segment downstream as its parent. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream. Streams of lower order joining a higher order stream do not change the order of the higher stream.  Thus, if a first-order stream joins a second-order stream, it remains a second-order stream. It is not until a second-order stream combines with another second-order stream that it becomes a third-order stream. As with mathematical trees, a segment with index i must be fed by at least 2 different tributaries of index 1. Shreve noted that Horton’s and Strahler’s Laws should be expected from any topologically random distribution. A later review of the relationships confirmed this argument, establishing that, from the properties the laws describe, no conclusion can be drawn to explain the structure or origin of the stream network.

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answers: downstream

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answers: treated as a node in a tree

answers: NDQ_006066

answers: Strahler stream order

answers: NDQ_006067

answers: no conclusion can be drawn to explain the structure or origin of the stream network

answers: NDQ_006068

answers: Strahler’s Laws

answers: NDQ_006069

answers: no conclusion can be drawn to explain the structure or origin of the stream network

text: Pocheon has two main water sources; Yeongpyeongcheon stream and Sannaecheon stream. The tributaries of Yeongpyeongcheon stream are the Pocheoncheon stream running through Pocheon-dong and Seondan-dong areas and the Ildongcheon stream passing through Ildong-myeon. The two streams merge into Yeongpyeongcheon which passes Auraji Ferry in Sindap-ri, Yeoncheon county and finally ends up to reach Hantan River. The other main water source, Sannaecheonm, runs through Choseong-ri village, Yeoncheon county and also reaches Hantan River. The two stream areas are relatively wide, so that it enables for the residents to use as cultivation places and resident places.

text: Pocheon has two main water sources;

text: Yeongpyeongcheon

text: stream and

text: Sannaecheon

text: stream. The tributaries of

text: Yeongpyeongcheon

text: stream are the Pocheoncheon stream running through Pocheon-dong and Seondan-dong areas and the Ildongcheon stream passing through Ildong-myeon. The two streams merge into Yeongpyeongcheon which passes

text: Auraji Ferry

text: in Sindap-ri,

text: Yeoncheon

text: county and finally ends up to reach

text: Hantan River

text: . The other main water source, Sannaecheonm, runs through Choseong-ri village, Yeoncheon county and also reaches Hantan River. The two stream areas are relatively wide, so that it enables for the residents to use as cultivation places and resident places.

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text: Parma   () is a city in the northern Italian region of Emilia-Romagna famous for its prosciutto (ham), cheese,  architecture, music and surrounding countryside. It is home to the University of Parma, one of the oldest universities in the world.Parma is divided into two parts by the stream of the same name. The district on the far side of the river is Oltretorrente. Parma's Etruscan name was adapted by Romans to describe the round shield called Parma.

text: Parma   () is a

text: city

text: in the northern Italian region of

text: Emilia-Romagna

text: famous for its

text: prosciutto

text: (ham),

text: cheese

text: architecture

text: music

text: and surrounding countryside. It is home to the

text: University of Parma

text: , one of the oldest universities in the world.Parma is divided into two parts by the

text: stream of the same name

text: . The district on the far side of the river is Oltretorrente. Parma's Etruscan name was adapted by Romans to describe the round shield called

text: Parma

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answers: Emilia-Romagna

text: Islamabad Highway crosses this stream near Sihala where the famous Kak Pul bridge is constructed over it. The Ling Stream joins the Soan river just before the Kak Pul. Two other famous streams, the Korang River joins it just before the Soan Bridge and Lai stream, joins this stream after the Soan Bridge. After following a tortuous path along a big curve, the stream reaches Kalabagh proposed Dam Site close to Pirpiyahi where it falls into the Indus river. There is a famous railway station by the name of Sohan and a beautiful railway bridge very close to it.  This relatively small stream is more than 250 kilometers long. Due to its mountainous course and shallow bed, it is hardly used for irrigation purposes. There are many species  of fish in this river like China Rahu, Mahasher, Snakehead, Balm and Catfish are the main species of fish in this stream and Kingfisher birds hunt here too. In addition, there are many species of tortoises and turtles. The marine life of this river has been endangered due to drainage of chemicals of Sihala Industrial State and effluent water of Rawalpindi city into it. There was a time when peoples used to fish in this stream with nets and hooks and bring home handsome catch but now, not only the above species of fish have diminished but also peoples avoid to eat Soan River's fish as it feeds on contaminated water, which can cause different diseases. Ministry of Environment must take action and treat the effluent water of Rawalpindi city before releasing it into Soan River and also punish and fine those industrialists who are releasing chemicals and other industrial waste into the river and destroying the beautiful marine life of Soan River.

text: Islamabad Highway

text: crosses this stream near

text: Sihala

text: where the famous Kak Pul bridge is constructed over it. The Ling Stream joins the Soan river just before the

text: Kak Pul

text: . Two other famous streams, the Korang River joins it just before the Soan Bridge and Lai stream, joins this stream after the Soan Bridge. After following a tortuous path along a big curve, the stream reaches Kalabagh proposed Dam Site close to Pirpiyahi where it falls into the

text: Indus river

text: . There is a famous railway station by the name of Sohan and a beautiful railway bridge very close to it.  This relatively small stream is more than 250 kilometers long. Due to its mountainous course and shallow bed, it is hardly used for irrigation purposes. There are many species  of fish in this river like China Rahu, Mahasher, Snakehead, Balm and Catfish are the main species of fish in this stream and

text: Kingfisher

text: birds hunt here too. In addition, there are many species of tortoises and turtles. The marine life of this river has been endangered due to drainage of chemicals of Sihala Industrial State and effluent water of Rawalpindi city into it. There was a time when peoples used to fish in this stream with nets and hooks and bring home handsome catch but now, not only the above species of fish have diminished but also peoples avoid to eat Soan River's fish as it feeds on contaminated water, which can cause different diseases. Ministry of Environment must take action and treat the effluent water of Rawalpindi city before releasing it into Soan River and also punish and fine those industrialists who are releasing chemicals and other industrial waste into the river and destroying the beautiful marine life of Soan River.

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answers: The marine life of this river has been endangered

text: Oracle Streams is the flow of information either within a single database or from one database to another. Oracle Streams can be set up in homogeneous (all Oracle databases) or heterogeneous (non-Oracle and Oracle databases) environments. The Streams setup uses a set of processes and database objects to share data and messages. The database changes (DDL and DML) are captured at the source; those are then staged and propagated to one or more destination databases to be applied there. Message propagation uses Advanced Queuing mechanism within the Oracle databases.

text: Oracle Streams is the flow of information either within a single database or from one database to another. Oracle Streams can be set up in homogeneous (all Oracle databases) or heterogeneous (non-Oracle and Oracle databases) environments. The Streams setup uses a set of processes and database objects to share data and messages. The database changes (

text: DDL

text: and

text: DML

text: ) are captured at the source; those are then staged and propagated to one or more destination databases to be applied there. Message propagation uses Advanced Queuing mechanism within the Oracle databases.

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answers: Oracle databases

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answers: Stream

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answers: propagated to one or more destination databases

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answers: The database changes (DDL and DML)

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answers: Streams setup uses a set of processes and database objects to share data and messages

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answers: The database changes (DDL and DML) are captured at the source; those are then staged and propagated to one or more destination databases

text: Lost Creek is a stream located entirely within Miami County, Ohio. The  long stream is a tributary of the Great Miami River.

text: Lost Creek is a

text: stream

text: located entirely within

text: Miami County, Ohio

text: . The  long stream is a tributary of the

text: Great Miami River

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text: A separate product, River and Small Stream Observations, is broadcast in areas in and outside of the 13 River Forecast Centers and is only broadcast following a significant hydrological event featuring information on crests, and present and forecasted flood stages.

text: A separate product, River and Small Stream Observations, is broadcast in areas in and outside of the 13 River Forecast Centers and is only broadcast following a significant hydrological event featuring information on crests, and present and forecasted

text: flood stage

text: s.

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answers: 13 River Forecast Centers

text: As you enter Havelock North from Hastings you cross a bridge over the Karamu Stream. The deeply incised channel provides a hint that this was once a much larger stream. In the early 1800s this stream was part of the much larger Ngaruroro River system, and was once called the "River Plassey", the same name also being applied to a street in the village after the battle of Plassey of 1757 near Calcutta in India where British Empire hero Robert Clive defeated the Mughal Nawab Siraj ud Daulla. Early survey plans of Havelock North show Ferry landings where boats would sail up and down the river to collect and deliver supplies. Unfortunately a number of large floods during the mid 1800s diverted the Ngaruroro River to its current course further north away from Havelock North and is now referred to as the Karamu Stream.

text: As you enter Havelock North from Hastings you cross a bridge over the Karamu Stream. The deeply incised channel provides a hint that this was once a much larger stream. In the early 1800s this stream was part of the much larger

text: Ngaruroro River

text: system, and was once called the "River Plassey", the same name also being applied to a street in the village after the

text: battle of Plassey

text: of 1757 near

text: Calcutta

text: in India where British Empire hero

text: Robert Clive

text: defeated the Mughal

text: Nawab Siraj ud Daulla

text: . Early survey plans of Havelock North show Ferry landings where boats would sail up and down the river to collect and deliver supplies. Unfortunately a number of large floods during the mid 1800s diverted the

text: Ngaruroro River

text: to its current course further north away from Havelock North and is now referred to as the Karamu Stream.

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answers: Karamu Stream

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answers: rivers

answers: NDQ_006069

answers: a number of large floods

text: The river is joined by a small stream from the south at small village #2. 2 km east of the NH 17 road bridge the river is joined from the south by the Pambar River at Koottar. The western part of the Manjampatti Valley catchment basin drains into the end of the Chinnar River. This Valley is drained by the stream Ten Ar and a smaller unnamed stream 2 km to its west. The unnamed stream is the N-S political boundary between Tamil Nadu and Kerala. The top of the ridge above this stream to the west is the western limit of the catchment.  This unnamed stream joins the Pambar River at the point they both join the Chinnar River at the north west corner of the Valley.

text: The river is joined by a small stream from the south at small village #2. 2 km east of the NH 17 road bridge the river is joined from the south by the

text: Pambar River

text: at

text: Koottar

text: . The western part of the

text: Manjampatti Valley

text: catchment basin drains into the end of the Chinnar River. This Valley is drained by the stream Ten Ar and a smaller unnamed stream 2 km to its west. The unnamed stream is the N-S political boundary between Tamil Nadu and Kerala. The top of the ridge above this stream to the west is the western limit of the catchment.  This unnamed stream joins the Pambar River at the point they both join the Chinnar River at the north west corner of the Valley.

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text: Zegama's main characteristic is its natural location as the last Gipuzkoan town up the valley of river Oria, very close to the Aizkorri-Aratz Natural Park, in which the highest mountain in the Basque Autonomous Community can be found, the popular Aizkorri summit (1,528 m), located at the same name mountain range towering over the whole area. The Oria river, the longest one in the province of Gipuzkoa, rises in several springs and their corresponding streams flowing down the dramatic slopes of the valley that merge in a main stream before the nucleus of the town. The southern Otzaurte hamlet (IPA: /o'tsaurte/) stands on the dividing line of the waters running onto the Mediterranean watershed and those flowing north to the Atlantic through the Oria river.

text: Zegama's main characteristic is its natural location as the last

text: Gipuzkoa

text: n town up the valley of river

text: Oria

text: , very close to the

text: Aizkorri-Aratz Natural Park

text: , in which the highest mountain in the

text: Basque Autonomous Community

text: can be found, the popular

text: Aizkorri

text: summit (1,528 m), located at the same name mountain range towering over the whole area. The

text: Oria

text: river, the longest one in the province of

text: Gipuzkoa

text: , rises in several springs and their corresponding streams flowing down the dramatic slopes of the valley that merge in a main stream before the nucleus of the town. The southern Otzaurte hamlet (IPA: /o'tsaurte/) stands on the dividing line of the waters running onto the Mediterranean watershed and those flowing north to the Atlantic through the Oria river.

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text: Islands in the Stream (1970) is the first of the posthumously published works of Ernest Hemingway. The book was originally intended to revive Hemingway’s reputation after the negative reviews of Across the River and Into the Trees. He began writing it in 1950 and advanced greatly through 1951. The work, rough but seemingly finished, was found by Mary Hemingway among 332 works Hemingway left behind at his death. Islands in the Stream was meant to encompass three stories to illustrate different stages in the life of its main character, Thomas Hudson. The three different parts of the novel were originally to be titled "The Sea When Young", "The Sea When Absent" and "The Sea in Being". These titles were changed, however, into what are now its three acts: "Bimini", "Cuba", and "At Sea".

text: Islands in the Stream (1970) is the first of the

text: posthumously published works

text: of

text: Ernest Hemingway

text: . The book was originally intended to revive Hemingway’s reputation after the negative reviews of

text: Across the River and Into the Trees

text: . He began writing it in 1950 and advanced greatly through 1951. The work, rough but seemingly finished, was found by

text: Mary Hemingway

text: among 332 works Hemingway left behind at his death. Islands in the Stream was meant to encompass three stories to illustrate different stages in the life of its main character, Thomas Hudson. The three different parts of the novel were originally to be titled "The Sea When Young", "The Sea When Absent" and "The Sea in Being". These titles were changed, however, into what are now its three acts: "Bimini", "Cuba", and "At Sea".

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answers: Islands in the Stream

text: On May 14, 1970 the local area was subjected to a significant flood on the Deep River which was assessed as having a greater than 50 year recurrence interval. The stream gage on the Deep River station measured a record stage of  and with a stream flow of

text: On May 14, 1970 the local area was subjected to a significant flood on the Deep River which was assessed as having a greater than 50 year

text: recurrence interval

text: . The

text: stream gage

text: on the Deep River station measured a record stage of  and with a stream flow of

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answers: NDQ_006069

answers: Deep River

text: The Inuit name for the river probably means "fairly large stream" or "a stream." A late 19th-century variant was "Kook Pow ruk."

text: The

text: Inuit

text: name for the river probably means "fairly large stream" or "a stream." A late 19th-century variant was "Kook Pow ruk."

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answers: NDQ_006067

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answers: NDQ_006068

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answers: NDQ_006069

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answers: NDQ_006060

answers: river

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Pacific Ocean

answers: NDQ_006063

answers: Inuit

answers: NDQ_006064

answers: river

answers: NDQ_006065

answers: fairly large

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Kook Pow Ruk

answers: NDQ_006068

answers: rivers provided water

answers: NDQ_006069

answers: Kook Pow ruk

text: When two streams or rivers merge or water is discharged to a stream it is possible to determine the BOD and DO after mixing assuming steady state conditions and instantaneous mixing.  The two streams are considered as dilutions of each other thus the initial BOD and DO will be

text: When two streams or rivers merge or water is discharged to a stream it is possible to determine the BOD and DO after mixing assuming

text: steady state

text: conditions and instantaneous mixing.  The two streams are considered as dilutions of each other thus the initial BOD and DO will be

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answers: NDQ_006069

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answers: NDQ_006060

answers: instantaneous mixing

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: dilution

answers: NDQ_006063

answers: BOD

answers: NDQ_006064

answers: River

answers: NDQ_006065

answers: determined

answers: NDQ_006066

answers: BOD

answers: NDQ_006067

answers: BOD

answers: NDQ_006068

answers: BOD

answers: NDQ_006069

answers: BOD

text: One of the important areas of hydrology is the interchange between rivers and aquifers. Groundwater/surface water interactions in streams and aquifers can be complex and the direction of net water flux (into surface water or into the aquifer) may vary spatially along a stream channel and over time at any particular location, depending on the relationship between stream stage and groundwater levels.

text: One of the important areas of hydrology is the interchange between rivers and aquifers. Groundwater/surface water interactions in streams and aquifers can be complex and the direction of net water flux (into surface water or into the aquifer) may vary spatially along a stream channel and over time at any particular location, depending on the relationship between stream stage and groundwater levels.

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answers: groundwater levels

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: aquifer

answers: NDQ_006063

answers: groundwater

answers: NDQ_006064

answers: particular location

answers: NDQ_006065

answers: depending on the relationship between stream stage

answers: NDQ_006066

answers: groundwater

answers: NDQ_006067

answers: groundwater

answers: NDQ_006068

answers: aquifers

answers: NDQ_006069

answers: groundwater

text: The Aller Canal was completed in 1863 after a three year construction period. It begins near Weyhausen just beyond the city of Wolfsburg, where it is joined by the tributary of the Kleine Aller. Here the Aller divides itself between its natural river channel and the canal. The canal runs in an almost straight line through the wetland of the Barnbruch as far as Gifhorn where it passes the town to the south. West of Gifhorn the canal uses the upgraded and widened stream bed of the Hehlenriede and, 5 km west of Gifhorn, near Brenneckenbrück on the B 188, it rejoins the Aller. About a kilometre before that the water of the canal drops by about a metre over a weir. The river flows parallel and north of the canal by several kilometres and, in this flat area of the Aller's old glacial valley, forms tightly-spaced meanders which reduce the water velocity in the river.

text: The Aller Canal was completed in 1863 after a three year construction period. It begins near

text: Weyhausen

text: just beyond the city of

text: Wolfsburg

text: , where it is joined by the tributary of the

text: Kleine Aller

text: . Here the Aller divides itself between its natural river channel and the canal. The canal runs in an almost straight line through the wetland of the

text: Barnbruch

text: as far as

text: Gifhorn

text: where it passes the town to the south. West of Gifhorn the canal uses the upgraded and widened stream bed of the

text: Hehlenriede

text: and, 5 km west of Gifhorn, near Brenneckenbrück on the

text: B 188

text: , it rejoins the Aller. About a kilometre before that the water of the canal drops by about a metre over a

text: weir

text: . The river flows parallel and north of the canal by several kilometres and, in this flat area of the Aller's old

text: glacial valley

text: , forms tightly-spaced

text: meanders

text: which reduce the water velocity in the river.

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text: Divided government is seen by different groups as a benefit or as an undesirable product of the model of governance used in the U.S. political system. Under said model, known as the separation of powers, the state is divided into different branches. Each branch has separate and independent powers and areas of responsibility so that the powers of one branch are not in conflict with the powers associated with the others. The model can be contrasted with the fusion of powers in a parliamentary system where the executive and legislature (and sometimes parts of the judiciary) are unified. Those in favor of divided government believe that such separations encourage more policing of those in power by the opposition, as well as limiting spending and the expansion of undesirable laws. Opponents, however, argue that divided governments become lethargic, leading to many gridlocks. In the late 1980s, Terry M. Moe, a professor of political science at Stanford University, examined the issue. He concluded that divided governments lead to compromise which can be seen as beneficial. But he also noticed that divided governments subvert performance and politicize the decisions of executive agencies.

text: Divided government is seen by different groups as a benefit or as an undesirable product of the model of governance used in the U.S. political system. Under said model, known as the

text: separation of powers

text: , the

text: state

text: is divided into different branches. Each branch has separate and independent powers and areas of responsibility so that the powers of one branch are not in conflict with the powers associated with the others. The model can be contrasted with the

text: fusion of powers

text: in a

text: parliamentary system

text: where the executive and legislature (and sometimes parts of the judiciary) are unified. Those in favor of divided government believe that such separations encourage more policing of those in power by the opposition, as well as limiting spending and the expansion of undesirable laws. Opponents, however, argue that divided governments become lethargic, leading to many gridlocks. In the late 1980s,

text: Terry M. Moe

text: , a professor of political science at

text: Stanford University

text: , examined the issue. He concluded that divided governments lead to compromise which can be seen as beneficial. But he also noticed that divided governments subvert performance and politicize the decisions of executive agencies.

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answers: Each branch has separate and independent powers and areas of responsibility

text: The Asan river is a river fed by the streams of the western part of the Doon valley. The northern section of the river is known locally as the 'Tons nadi' (a misnomer, the actual Tons nadi is much larger and flows into the Yamuna in the Jaunsar Bawar region at Kalsi); originates from the southern slopes of Mussorie. There are several streams here, that gradually merge into one river that emerges from Robber's cave. The river here is in a U-shaped valley meandering slightly in a south-westerly direction. The river flows through Bijapur canal; a major water pumping site of Dehradun that provides water to houses in the western part of the town through two water canals. It then moves on to Tapkeshwar Mahadev, a popular Shiva shrine before becoming a more shallow, broad valley near Premnagar. The river proceeds south-west, receiving the waters of several streams flowing southward from the northern range spanning Vikas Nagar - Mussorie; and northward from the lower Shiwalik forest hills that separate The Doon valley from Saharanpur district. In the lower section it is known as the 'Asan'.  It flows into a relatively flat section which feeds the Asan barrage, the waters of which drain into the Yamuna at Poanta Sahib.

text: The Asan river is a river fed by the streams of the western part of the Doon valley. The northern section of the river is known locally as the 'Tons nadi' (a misnomer, the actual Tons nadi is much larger and flows into the

text: Yamuna

text: in the

text: Jaunsar Bawar

text: region at Kalsi); originates from the southern slopes of

text: Mussorie

text: . There are several streams here, that gradually merge into one river that emerges from Robber's cave. The river here is in a U-shaped valley meandering slightly in a south-westerly direction. The river flows through Bijapur canal; a major water pumping site of Dehradun that provides water to houses in the western part of the town through two water canals. It then moves on to

text: Tapkeshwar Mahadev

text: , a popular

text: Shiva

text: shrine before becoming a more shallow, broad valley near Premnagar. The river proceeds south-west, receiving the waters of several streams flowing southward from the northern range spanning Vikas Nagar - Mussorie; and northward from the lower

text: Shiwalik forest hills

text: that separate The Doon valley from

text: Saharanpur district

text: . In the lower section it is known as the 'Asan'.  It flows into a relatively flat section which feeds the Asan barrage, the waters of which drain into the Yamuna at Poanta Sahib.

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text: Black Nubble stands within the watershed of the Kennebec River, which drains into the Gulf of Maine. The east side of Black Nubble drains into Nash Stream, then into the South Branch of the Dead River, Flagstaff Lake, the Dead River and the Kennebec. The west side of Black Nubble drains into the West Branch of Nash Stream. The south end of Black Nubble drains into Orbeton Stream, then into the Sandy River, another tributary of the Kennebec River.

text: Black Nubble stands within the

text: watershed

text: of the

text: Kennebec River

text: , which drains into the

text: Gulf of Maine

text: . The east side of Black Nubble drains into Nash Stream, then into the

text: South Branch

text: of the Dead River,

text: Flagstaff Lake

text: , the

text: Dead River

text: and the Kennebec. The west side of Black Nubble drains into the West Branch of Nash Stream. The south end of Black Nubble drains into Orbeton Stream, then into the

text: Sandy River

text: , another

text: tributary

text: of the Kennebec River.

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answers: Kennebec River

text: Indian Creek is a stream in the U.S. state of Missouri. It is a tributary of the Meramec River.

text: Indian Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the

text: Meramec River

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answers: Meramec River

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Indian Creek

answers: NDQ_006063

answers: U.S.

answers: NDQ_006064

answers: tributary

answers: NDQ_006065

answers: tributary

answers: NDQ_006066

answers: Indian Creek

answers: NDQ_006067

answers: Indian Creek is a stream

answers: NDQ_006068

answers: Indian Creek

answers: NDQ_006069

answers: Indian Creek

text: Little Massabesic Brook and Sucker Brook form a  stream located in southern New Hampshire in the United States.  They are tributaries of Massabesic Lake, part of the Merrimack River and Gulf of Maine watersheds.  Despite the streams' short length, they are subject to the New Hampshire Comprehensive Shoreland Protection Act, because of their fourth order stream status (indicating a high number of upstream tributary sets).

text: Little Massabesic Brook and Sucker Brook form a

text: stream

text: located in southern

text: New Hampshire

text: in the

text: United States

text: .  They are

text: tributaries

text: of

text: Massabesic Lake

text: , part of the

text: Merrimack River

text: and

text: Gulf of Maine

text: watersheds

text: .  Despite the streams' short length, they are subject to the New Hampshire Comprehensive Shoreland Protection Act, because of their fourth order stream status (indicating a high number of upstream tributary sets).

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answers: NDQ_006060

answers: fourth order stream status

answers: NDQ_006061

answers: a high number of upstream tributary sets

answers: NDQ_006062

answers: Gulf of Maine

answers: NDQ_006063

answers: New Hampshire

answers: NDQ_006064

answers: New Hampshire

answers: NDQ_006065

answers: high number of upstream tributary sets

answers: NDQ_006066

answers: Gulf of Maine

answers: NDQ_006067

answers: Gulf of Maine

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: Little Massabesic Brook and Sucker Brook

text: Kääpa - Kalita stream- Kalli - Kargaja- Kärla - Käru- Kasari - Kata- Katku stream- Kavilda- Keila - Kloostri- Kodila- Kohtra - Kolga- Kolga stream- Kõpu- Koosa- Kroodi stream- Kuivajõgi- Kuke- Külge stream- Kulgu- Kullavere - Kunda - Kurina- Kurna stream- Kuura

text: Kääpa - Kalita stream- Kalli - Kargaja- Kärla - Käru-

text: Kasari

text: - Kata- Katku stream- Kavilda-

text: Keila

text: - Kloostri- Kodila- Kohtra - Kolga- Kolga stream- Kõpu- Koosa- Kroodi stream- Kuivajõgi- Kuke- Külge stream- Kulgu- Kullavere -

text: Kunda

text: - Kurina- Kurna stream- Kuura

answers: tqa2:L_0319/T_1733/7a9bad61818ee23e2e174470b89843f5

answers: 3: The answer has limited relevance and completeness, with noticeable gaps or inaccuracies.

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answers: 4: The answer has limited relevance and completeness, with noticeable gaps or inaccuracies.

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answers: 1

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answers: NDQ_006060

answers: Kuura

answers: NDQ_006061

answers: Külge

answers: NDQ_006062

answers: Pacific Ocean

answers: NDQ_006063

answers: Kavilda

answers: NDQ_006064

answers: Kuura

answers: NDQ_006065

answers: Külge

answers: NDQ_006066

answers: Külge stream- Kulgu

answers: NDQ_006067

answers: Külge stream

answers: NDQ_006068

answers: Koosa

answers: NDQ_006069

answers: Kuivaj gi

text: Region 1 is known for moose and big meadows and is located on the west, or Grand Lake, side of the Continental Divide.  Thirty miles of the Continental Divide National Scenic Trail loop through the park and pass through alpine tundra and scenery. A geographical anomaly is found along the slopes of the Never Summer Mountains, where the Continental Divide forms a horseshoeshaped bend for about  from north to south and then west out of the park. The sharp bend results in streams on the eastern slopes of the range joining the headwaters of the Colorado River that flow south and west, eventually reaching the Pacific Ocean via the Gulf of California. Meanwhile, streams on the western slopes join rivers that flow north and then east and south eventually reaching the Atlantic Ocean via the Gulf of Mexico. Baker Pass crosses the Continental Divide through the Never Summer Mountains and into the Michigan River drainage to the west of Mount Nimbusa drainage that feeds streams and rivers that drain into the Gulf of Mexico.

text: Region 1 is known for moose and big meadows and is located on the west, or Grand Lake, side of the Continental Divide.  Thirty miles of the

text: Continental Divide National Scenic Trail

text: loop through the park and pass through alpine tundra and scenery. A geographical anomaly is found along the slopes of the

text: Never Summer Mountains

text: , where the Continental Divide forms a

text: horseshoe

text: shaped bend for about  from north to south and then west out of the park. The sharp bend results in streams on the eastern slopes of the range joining the headwaters of the

text: Colorado River

text: that flow south and west, eventually reaching the Pacific Ocean via the

text: Gulf of California

text: . Meanwhile, streams on the western slopes join rivers that flow north and then east and south eventually reaching the Atlantic Ocean via the

text: Gulf of Mexico

text: . Baker Pass crosses the Continental Divide through the Never Summer Mountains and into the

text: Michigan River

text: drainage to the west of Mount Nimbusa drainage that feeds streams and rivers that drain into the Gulf of Mexico.

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answers: 0

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answers: 0

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answers: 4

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answers: 4

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answers: 4

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answers: 0

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answers: 0

answers: NDQ_006069

answers: 0

answers: NDQ_006060

answers: Mount Nimbusa drainage

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: A geographical anomaly

answers: NDQ_006063

answers: Grand Lake

answers: NDQ_006064

answers: drainage

answers: NDQ_006065

answers: flow south and west

answers: NDQ_006066

answers: Gulf of California

answers: NDQ_006067

answers: Gulf of Mexico

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: the Gulf of California

text: Blackhoof Creek is a stream located entirely within Auglaize County, Ohio. The  long stream is a tributary of the Auglaize River.

text: Blackhoof Creek is a stream located entirely within

text: Auglaize County, Ohio

text: . The  long stream is a tributary of the

text: Auglaize River

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answers: 0

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answers: It is a tributary

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text: The source or headwaters of a river or stream is the furthest place in that river or stream from its estuary or confluence with another river, as measured along the course of the river.

text: The source or headwaters of a

text: river

text: or

text: stream

text: is the furthest place in that river or stream from its

text: estuary

text: or

text: confluence

text: with another river, as measured along the course of the river.

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text: Frequents rocky streams, rivers, river-pools. Typically perches on mid-stream rocks

text: Frequents rocky streams, rivers, river-pools. Typically perches on mid-stream rocks

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answers: NDQ_006064

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answers: NDQ_006065

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answers: NDQ_006067

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answers: NDQ_006068

answers: river-pools

answers: NDQ_006069

answers: river-pools

text: The stream's watershed is part of the Piedmont region, characterized by rolling hills. The lower  of the stream is designated a Scenic River.

text: The stream's watershed is part of the

text: Piedmont

text: region, characterized by rolling hills. The lower  of the stream is designated a Scenic River.

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answers: NDQ_006064

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answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: rolling hills

answers: NDQ_006069

answers: rolling hills

text: The Oct 1947 Lands and Survey one inch map shows the name 'Opotoru R' applied to the tidal creek of the harbour and 'Opotoru S' to the stretch through Te Mata. The 1971 2nd edition and current 1:50,000 maps (see http://www.topomap.co.nz/NZTopoMap/37544) show 'Opotoru River' for the lower part of the waterway, but 'Te Mata Stream' for the part up from the Te Hutewai Stream confluence. 'Te Mata Stream' appears to have been named 'Takapuanui Stream' in the 1910 postcards (see link below) and in the 1915 Bradbury's Illustrated Guide to The Raglan & Kawhia District.

text: The Oct 1947 Lands and Survey one inch map shows the name 'Opotoru R' applied to the tidal creek of the harbour and 'Opotoru S' to the stretch through

text: Te Mata

text: . The 1971 2nd edition and current 1:50,000 maps (see http://www.topomap.co.nz/NZTopoMap/37544) show 'Opotoru River' for the lower part of the waterway, but 'Te Mata Stream' for the part up from the Te Hutewai Stream confluence. 'Te Mata Stream' appears to have been named 'Takapuanui Stream' in the 1910 postcards (see link below) and in the 1915 Bradbury's Illustrated Guide to The Raglan & Kawhia District.

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text: The Neretva is largest karst river in the Dinaric Alps in the entire eastern part of the Adriatic basin, which belongs to the Adriatic river watershed. The total length is , of which  are in Bosnia and Herzegovina, while the final  are in the Dubrovnik-Neretva County of Croatia.The municipality of Konjic includes at least half of the area of the Upper Neretva (), which is the upper course of the Neretva river. Geographically and hydrologically the Neretva is divided into three sections.The upper course of the Neretva river is simply called the Upper Neretva (), and includes a vast area around the Neretva, numerous streams and well-springs, three major glacial lakes near the river (and even more lakes, outside the municipality of Konjic, scattered across the mountains of Treskavica and Zelengora in the wider area of the Upper Neretva), one artificial lake (Jablaničko), mountains and forests, and native flora and fauna. All this natural heritage together with the cultural heritage of the Upper Neretva, represent rich and valuable resources of Bosnia and Herzegovina as well as Europe.The Upper Neretva has water of Class I purity and is almost certainly the coldest river water in the world, often as low as  in the summer months.

text: The

text: Neretva

text: is largest

text: karst

text: river in the

text: Dinaric Alps

text: in the entire eastern part of the

text: Adriatic

text: basin, which belongs to the

text: Adriatic

text: river watershed. The total length is , of which  are in

text: Bosnia and Herzegovina

text: , while the final  are in the

text: Dubrovnik-Neretva County

text: of

text: Croatia

text: .The municipality of Konjic includes at least half of the area of the

text: Upper Neretva

text: (), which is the upper course of the

text: Neretva

text: river. Geographically and hydrologically the

text: Neretva

text: is divided into three sections.The upper course of the

text: Neretva

text: river is simply called the

text: Upper Neretva

text: (), and includes a vast area around the

text: Neretva

text: , numerous streams and well-springs, three major glacial lakes near the river (and even more lakes, outside the municipality of Konjic, scattered across the mountains of

text: Treskavica

text: and

text: Zelengora

text: in the wider area of the

text: Upper Neretva

text: ), one artificial lake (Jablaničko), mountains and forests, and native flora and fauna. All this natural heritage together with the cultural heritage of the Upper Neretva, represent rich and valuable resources of

text: Bosnia and Herzegovina

text: as well as

text: Europe

text: .The Upper Neretva has water of Class I purity and is almost certainly the coldest river water in the world, often as low as  in the summer months.

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text: Officially designated as a river, the Cooba Bulga Stream rises on the southern slopes of the Liverpool Range within the Great Dividing Range about  south of Omaleah Cliffs. The river flows generally southwest and then south before reaching its confluence with the Munmurra River near . Cooba Bulga Stream descends  over its  course.

text: Officially designated as a river, the Cooba Bulga Stream rises on the southern slopes of the

text: Liverpool Range

text: within the

text: Great Dividing Range

text: about  south of Omaleah Cliffs. The river flows generally southwest and then south before reaching its

text: confluence

text: with the

text: Munmurra River

text: near . Cooba Bulga Stream descends  over its

text: course

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answers: The river flows generally southwest

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answers: Cooba Bulga Stream

text: "Songpa District is a pleasant and beautiful area with nearby lake and streams."Songpa District will link four nearby streams (Han River, Seongnae stream, Jangji stream and Tan stream) to one another through the dubbed Waterway Project. Songpa will be a unique island-like district when Waterway Project is completed by 2012, which is aimed at building Songpa an eco-friendly district where water, nature and human being are harmonized with one another.Nature Eco Network is a 27 km long forest with a willow volley and a reserve of wild lives. In Walk Network, people can sense Songpa's history and culture while taking a walk, and feel the fresh air when riding a bicycle on Bicycle Network.The Seokchon lake, which was generated from the Han River as the result of the multiple purpose development of Jamsil in the 1970s, had been averted by the residents because of a nasty smell, in spite of the fact that it's the only lake in the downtown of Seoul. The smell came from water pollution from concrete materials. But, in the 2000s, it was reborn as the real rest area where attract the visitors of 20,000~30,000 on weekdays, over 50,000 on weekends and are the nests for animals and plants including aquatic plants. And, this is the result of the development project for the natural ecology park.On June, 2005, Sungnae-chun was also resuscitated as a beautiful river through the development project for the ecology river. It was a dried river due to the low volume of water flow during the 1970s~the 1980s. But in 2009 it was selected as 'the most beautiful 100 rivers in Korea' by Land, Transport and Maritime Affairs.If the four rivers in 'waterway' are the main artery, a streamlet is a vessel. Songpa District developed a streamlet alongside South Beltway (1.5 km from Ogeum intersection ~ Olympic Park intersection ~ Seongnae Stream), easing hot island phenomena and reclaiming water at the same time.

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answers: Nature Eco Network

answers: NDQ_006069

answers: stream

text: The Mad River (Shawnee: Hathennithiipi ) is a stream located in the west central part of the U.S. state of Ohio.  It flows  from Logan County to downtown Dayton, where it meets the Great Miami River. The stream flows southwest from its source near Campbell Hill through West Liberty, along U.S. Route 68 west of Urbana, past Springfield (the point of confluence with Buck Creek), then along Ohio State Route 4 into Dayton. The stream's confluence with the Great Miami River is in Deeds Park.

text: The Mad River (

text: Shawnee

text: : Hathennithiipi ) is a stream located in the west central part of the U.S. state of Ohio.  It flows  from

text: Logan County

text: to downtown

text: Dayton

text: , where it meets the

text: Great Miami River

text: . The stream flows southwest from its

text: source

text: near

text: Campbell Hill

text: through

text: West Liberty

text: , along

text: U.S. Route 68

text: west of

text: Urbana

text: , past

text: Springfield

text: (the point of confluence with

text: Buck Creek

text: ), then along

text: Ohio State Route 4

text: into Dayton. The stream's confluence with the Great Miami River is in Deeds Park.

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answers: the Great Miami River

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answers: It flows southwest from its source near Campbell Hill

text: The colonization of the lordship of Sainte-Anne-de-la-Pérade began with a leading front on the north side of St. Lawrence river. Initially, the second row was not implemented because of the swampy (including peat) land. In a second stage of colonization, the settlers chose to settle along the Sainte-Anne river. Then, the expansion to the second row away from streams, rather orientation towards Charest River and its main branch the stream Gendron. This rises to the top the morraine in the territory of Saint-Stanislas (east side of the Batiscan river), descends into the morraine and through the village of Saint-Prosper before emptying into the Charest river, almost at its mouth. Charest river latter flows into the Sainte-Anne river.

text: The colonization of the lordship of Sainte-Anne-de-la-Pérade began with a leading front on the north side of

text: St. Lawrence river

text: . Initially, the second row was not implemented because of the swampy (including peat) land. In a second stage of colonization, the settlers chose to settle along the Sainte-Anne river. Then, the expansion to the second row away from streams, rather orientation towards

text: Charest River

text: and its main branch the

text: stream Gendron

text: . This rises to the top the morraine in the territory of

text: Saint-Stanislas

text: (east side of the

text: Batiscan river

text: ), descends into the morraine and through the village of

text: Saint-Prosper

text: before emptying into the

text: Charest river

text: , almost at its mouth.

text: Charest river

text: latter flows into the Sainte-Anne river.

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answers: NDQ_006063

answers: St. Lawrence river

answers: NDQ_006064

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answers: NDQ_006065

answers: rising to the top

answers: NDQ_006066

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answers: St. Lawrence river

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Charest River

text: Czech language distinguishes between larger (river) and smaller (stream, creek, brook etc.) watercourses; the respective nouns being řeka (feminine, "river") and potok (masculine, "stream"). River names are mostly self-standing nouns and not accompanied with the generic word for river (except when confusion might arose because name is shared with some towns, e.g. Jihlava; in such cases one sometimes says řeka Jihlava). In contrast, stream names mostly consist of two words because they contain an adjective (usually stemming from physical properties (e.g. Černý potok-"Black Stream"), usage (e.g. Mlýnský potok-"Mill Stream") or derived from location through which it flows (e.g. Rakovnický potok-"Rakovník Stream")). These two-word names are used as a whole, the word potok making an inseparable part of the name (i.e. Mlýnský potok, not just Mlýnský). There are also streams with one-word names (either masculine or feminine) akin to rivers (e.g. Botič or Modla) but they are simply considered streams due to their small size. In such cases the word potok is optional and precedes the name (potok Modla).

text: Czech language

text: distinguishes between larger (river) and smaller (stream, creek, brook etc.) watercourses; the respective nouns being

text: řeka

text: (feminine, "river") and

text: potok

text: (masculine, "stream"). River names are mostly self-standing nouns and not accompanied with the generic word for river (except when confusion might arose because name is shared with some towns, e.g.

text: Jihlava

text: ; in such cases one sometimes says řeka Jihlava). In contrast, stream names mostly consist of two words because they contain an adjective (usually stemming from physical properties (e.g. Černý potok-"Black Stream"), usage (e.g. Mlýnský potok-"Mill Stream") or derived from location through which it flows (e.g. Rakovnický potok-"Rakovník Stream")). These two-word names are used as a whole, the word potok making an inseparable part of the name (i.e. Mlýnský potok, not just Mlýnský). There are also streams with one-word names (either masculine or feminine) akin to rivers (e.g. Botič or Modla) but they are simply considered streams due to their small size. In such cases the word potok is optional and precedes the name (potok Modla).

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answers: brook

answers: NDQ_006061

answers: In such cases the word potok is optional and precedes the name

answers: NDQ_006062

answers: Black Stream

answers: NDQ_006063

answers: Czech language

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answers: Potok

answers: NDQ_006065

answers: due to their small size

answers: NDQ_006066

answers: River names are mostly self-standing nouns

answers: NDQ_006067

answers: River names are mostly self-standing nouns and not accompanied with the generic word for river

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The word potok making an inseparable part of the name

text: Subsequent uplift of the Colorado Plateau slowly raised these formations much higher than where they were deposited. This steepened the stream gradient of the ancestral rivers and other streams on the plateau. The faster-moving streams took advantage of uplift-created joints in the rocks to remove all Cenozoic-aged formations and cut gorges into the plateaus. Zion Canyon was cut by the North Fork of the Virgin River in this way. Lava flows and cinder cones covered parts of the area during the later part of this process.

text: Subsequent uplift of the

text: Colorado Plateau

text: slowly raised these formations much higher than where they were deposited. This steepened the

text: stream gradient

text: of the ancestral rivers and other streams on the

text: plateau

text: . The faster-moving streams took advantage of uplift-created joints in the rocks to remove all

text: Cenozoic

text: -aged formations and cut gorges into the plateaus. Zion Canyon was cut by the North Fork of the

text: Virgin River

text: in this way.

text: Lava

text: flows and

text: cinder cone

text: s covered parts of the area during the later part of this process.

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answers: NDQ_006067

answers: The faster-moving streams

answers: NDQ_006068

answers: gorges

answers: NDQ_006069

answers: Lava flows and cinder cones

text: If  is a prime number and  divides a product  of integers, then  divides  or  divides . This proposition is known as Euclid's lemma.  It is used in some proofs of the uniqueness of prime factorizations.

text: If  is a prime number and  divides a product  of integers, then  divides  or  divides . This proposition is known as

text: Euclid's lemma

text: .  It is used in some proofs of the uniqueness of prime factorizations.

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answers: Euclid's lemma

text: Several genetic studies have found that eastern freshwater cod, in the southernmost of these four rivers, and Mary River cod, in the northernmost of these four rivers, are more closely related to each other than to Murray cod. This suggests that Murray cod only managed to cross into east coast river systems once. It is not clear which of the four river systems was the original entry point, but geomorphological evidence suggests the headwaters of the Clarence River. The mechanism by which Murray cod crossed the Great Dividing Range are considered to be either river capture, where the headwaters of an easterly-flowing coastal river cuts back (in the erosional sense) and intercepts and "captures" the headwaters (and fish fauna) of a previously westerly flowing stream, or a "wet divide", where extreme flooding or a very wet climatic phase created swamps in a topographic low point that effectively connected the headwaters of western flowing and eastern flowing streams.

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answers: a topographic low point

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answers: No

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answers: NDQ_006063

answers: Great Dividing Range

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answers: NDQ_006066

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answers: NDQ_006067

answers: Murray cod

answers: NDQ_006068

answers: fish fauna

answers: NDQ_006069

answers: Murray cod only managed to cross into east coast river systems once

text: The river is a "consequent stream" or a "tidal river", which means that the Vermilion was formed from the bottom up.  The river was created by Vermilion Bay: tides and other natural actions in the bay slowly eroded the marshes and other features of the landscape as the river crept northward.  This process brought the channel that would one day become the Vermilion River as far north as Lafayette, Louisiana.  Much later a distributary of Bayou Teche made its way south and eventually linked up with the consequent stream, forming a true north-south flowing river. During times of heavy-rain events, parts of the Vermilion will reverse and flow north (Citation needed).  The reverse-flow phenomenon occurs because the watershed areas in the city of Lafayette are highly developed.  Rainfall runoff from this urban area enters the Vermilion River with larger volumes and at a faster rate than runoff upstream.  This raises the water level in the Vermilion River along the southern areas of Lafayette.  This rise in water levels sometimes exceeds the water level in reaches upstream of Lafayette, thus causing the reverse-flow effect.  Also, when water levels in the Vermilion River exceed certain stages, water begins to enter the Bayou Tortue Swamp Area. This swamp has a great capacity to hold water, which also contributes to the reverse flow effect. The water from the Vermilion River enters Bayou Tortue Swamp through two coulees. Coulee Crow and Bayou Tortue are located upstream of the Surrey Street bridge on the Vermilion River.

text: The river is a "consequent stream" or a "

text: tidal river

text: ", which means that the Vermilion was formed from the bottom up.  The river was created by Vermilion Bay: tides and other natural actions in the bay slowly eroded the marshes and other features of the landscape as the river crept northward.  This process brought the channel that would one day become the Vermilion River as far north as

text: Lafayette, Louisiana

text: .  Much later a distributary of

text: Bayou Teche

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answers: NDQ_006061

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answers: The reverse-flow phenomenon

answers: NDQ_006063

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answers: NDQ_006064

answers: Swamp

answers: NDQ_006065

answers: slowly

answers: NDQ_006066

answers: west side of the continental divide

answers: NDQ_006067

answers: Bayou Tortue Swamp

answers: NDQ_006068

answers: This swamp has a great capacity to hold water

answers: NDQ_006069

answers: The water from the Vermilion River enters Bayou Tortue Swamp through two coulees

text: The community lies on flat land extending from Colón. It is watered by the rivers Palmillias, Piedras, Las Ciegas and Jigüe. The La Palma River which enjoys considerable flow is fed by three streams, the first from the Lake of Banagüises, the second, known as the Piedra River originating in the Nueva Bermeja and Palmillas and fed by the Jigüe, Macagosa and other streams, and the third the creek of Potrerillo. The La Palmas River flows  from San José de los Ramos to its mouth in the Bay of Santa Clara. It can be navigated up to the landing stage known as La Palma.

text: The community lies on flat land extending from Colón. It is watered by the rivers Palmillias, Piedras, Las Ciegas and Jigüe. The

text: La Palma River

text: which enjoys considerable flow is fed by three streams, the first from the Lake of Banagüises, the second, known as the Piedra River originating in the Nueva Bermeja and Palmillas and fed by the Jigüe, Macagosa and other streams, and the third the creek of Potrerillo. The La Palmas River flows  from San José de los Ramos to its mouth in the Bay of Santa Clara. It can be navigated up to the landing stage known as La Palma.

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answers: Bay of Santa Clara

answers: NDQ_006061

answers: no

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answers: Bay of Santa Clara

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answers: flat land

answers: NDQ_006064

answers: Lake

answers: NDQ_006065

answers: considerable

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: The La Palmas River

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The community lies on flat land extending from Colón

text: Tiruchirappalli is situated in central south-eastern India, almost at the geographic centre of the state of Tamil Nadu. The Kaveri Delta begins to form  west of the city where the river divides into two streams—the Kaveri and the Kollidam—to form the island of Srirangam. By road it is  south of Hyderabad,  south-west of Chennai and  south-east of Bangalore. The topology of Tiruchirappalli is almost flat, with an average elevation of . A few isolated hillocks rise above the surface, the highest of which is the Rockfort; its estimated age of 3,800 million years makes it one of the oldest rocks in the world. Other prominent hillocks include the Golden Rock, Khajamalai, and one each at Uyyakondan Thirumalai and Thiruverumbur.

text: Tiruchirappalli is situated in central south-eastern India, almost at the geographic centre of the state of Tamil Nadu. The Kaveri Delta begins to form  west of the city where the river divides into two streams—the Kaveri and the Kollidam—to form the

text: island of Srirangam

text: . By road it is  south of

text: Hyderabad

text: ,  south-west of Chennai and  south-east of

text: Bangalore

text: . The topology of Tiruchirappalli is almost flat, with an average elevation of . A few isolated hillocks rise above the surface, the highest of which is the Rockfort; its estimated age of 3,800 million years makes it one of the oldest rocks in the world. Other prominent hillocks include the

text: Golden Rock

text: Khajamalai

text: , and one each at

text: Uyyakondan Thirumalai

text: and

text: Thiruverumbur

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answers: Kaveri Delta

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: the island of Srirangam

answers: NDQ_006063

answers: average elevation

answers: NDQ_006064

answers: Delta

answers: NDQ_006065

answers: average elevation

answers: NDQ_006066

answers: Kaveri Delta begins to form west of the city

answers: NDQ_006067

answers: Kaveri Delta

answers: NDQ_006068

answers: river

answers: NDQ_006069

answers: Tiruchirappalli

text: • the Mekinac River which course part start at the mouth of Mékinac Lake to flow into the Saint-Maurice River in Middle-Mauricie. The northern part of Lejeune Township flows to the Mekinac River, including Lake Button and Lake Lejeune. The latter joined the Thom stream via Lake Bouchard, Lake George and Lake Thom. The Thom stream flows into the Mékinac River in the village of Saint-Joseph-de-Mékinac.

text: • the

text: Mekinac River

text: which course part start at the mouth of

text: Mékinac Lake

text: to flow into the

text: Saint-Maurice River

text: in Middle-Mauricie. The northern part of

text: Lejeune Township

text: flows to the Mekinac River, including Lake Button and Lake Lejeune. The latter joined the Thom stream via Lake Bouchard, Lake George and Lake Thom. The Thom stream flows into the

text: Mékinac River

text: in the village of Saint-Joseph-de-Mékinac.

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answers: Mékinac River

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Mekinac River

answers: NDQ_006063

answers: Lake Lejeune

answers: NDQ_006064

answers: Mouth

answers: NDQ_006065

answers: erodes

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: The Thom stream

answers: NDQ_006068

answers: Lakes

answers: NDQ_006069

answers: Lake Lejeune

text: The calculation is just the difference in elevation between the river's source and the river's confluence or mouth divided by the total length of the river or stream. This gives the average drop in elevation per unit length of river.

text: The calculation is just the difference in

text: elevation

text: between the river's

text: source

text: and the river's

text: confluence

text: or

text: mouth

text: divided by the total

text: length

text: of the river or stream. This gives the average drop in elevation per unit length of river.

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text: When river water is used in surface irrigation, the part of water joining the stream is termed as ‘return flows’ and the part of water joining the aquifer is termed as ‘seepage loss’ or manmade ground water charging. The sum of primary water supplies and return (recycled) flows in a river basin is the total water available for use. The total available water for use in a river basin is almost one-and-half times the primary water supplies if net ground water use is also accounted.  If ground water use is intensive or close to ground water mining, the return flows would be during heavy rains period only which are below 10% of primary water supplies in the river basin. There would be negligible base flows into the river streams during the remaining period and  good chance of river turning in to losing stream due to unsustainable ground water exploitation.

text: When river water is used in surface irrigation, the part of water joining the stream is termed as ‘return flows’ and the part of water joining the aquifer is termed as ‘seepage loss’ or manmade ground water charging. The sum of primary water supplies and return (recycled) flows in a river basin is the total water available for use. The total available water for use in a river basin is almost one-and-half times the primary water supplies if net ground water use is also accounted.  If ground water use is intensive or close to ground water mining, the return flows would be during heavy rains period only which are below 10% of primary water supplies in the river basin. There would be negligible base flows into the river streams during the remaining period and  good chance of river turning in to

text: losing stream

text: due to unsustainable ground water exploitation.

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answers: If ground water use is intensive

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text: The catchment of a river above a certain location is determined by the surface area of all land which drains toward the river from above that point.  The river's discharge at that location depends on the rainfall on the catchment or drainage area and the inflow or outflow of groundwater to or from the area, stream modifications such as dams and irrigation diversions, as well as evaporation and evapotranspiration from the area's land and plant surfaces. In storm hydrology, an important consideration is the stream's discharge hydrograph, a record of how the discharge varies over time after a precipitation event.  The stream rises to a peak flow after each precipitation event, then falls in a slow recession.  Because the peak flow also corresponds to the maximum water level reached during the event, it is of interest in flood studies.  Analysis of the relationship between precipitation intensity and duration and the response of the stream discharge are aided by the concept of the unit hydrograph, which represents the response of stream discharge over time to the application of a hypothetical "unit" amount and duration of rainfall (e.g., half an inch over one hour).  The amount of precipitation correlates to the volume of water (depending on the area of the catchment) that subsequently flows out of the river. Using the unit hydrograph method, actual historical rainfalls can be modeled mathematically to confirm characteristics of historical floods, and hypothetical "design storms" can be created for comparison to observed stream responses.

text: The

text: catchment

text: of a river above a certain location is determined by the surface area of all land which drains toward the river from above that point.  The river's discharge at that location depends on the rainfall on the catchment or

text: drainage area

text: and the inflow or outflow of groundwater to or from the area, stream modifications such as dams and irrigation diversions, as well as evaporation and evapotranspiration from the area's land and plant surfaces. In

text: storm hydrology

text: , an important consideration is the stream's

text: discharge hydrograph

text: , a record of how the discharge varies over time after a precipitation event.  The stream rises to a peak flow after each precipitation event, then falls in a slow

text: recession

text: .  Because the peak flow also corresponds to the maximum water level reached during the event, it is of interest in flood studies.  Analysis of the relationship between precipitation intensity and duration and the response of the stream discharge are aided by the concept of the

text: unit hydrograph

text: , which represents the response of stream discharge over time to the application of a hypothetical "unit" amount and duration of rainfall (e.g., half an inch over one hour).  The amount of precipitation correlates to the volume of water (depending on the area of the catchment) that subsequently flows out of the river. Using the unit hydrograph method, actual historical rainfalls can be modeled mathematically to confirm characteristics of historical floods, and hypothetical "design storms" can be created for comparison to observed stream responses.

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answers: depends on the rainfall on the catchment or drainage area

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answers: evaporation and evapotranspiration

text: The 2-mile (3 km) portage at Portage, Wisconsin is not unique as a passage between the Great Lakes and Mississippi River watersheds.  Similar passages exist all along the watershed divide, for instance, at Chicago and in the northern Indiana area..  What is unique is that, while the Fox is a small stream—typical of such passages—the Wisconsin is a large river, already over 300 miles (500 km) long. The divide between the two rivers has little grade change, although it is marshy.  The Wisconsin occasionally flowed across the Portage into the Fox during high water.  The Fox and Wisconsin have modified their courses and outlets over geological time  and it is likely that either river has flowed into either watershed.  Only about 2 miles (3 km) separate the two rivers. The Fox River end of the canal is at about elevation 780 feet (238 m) msl. The Wisconsin River end is slightly higher, depending on Wisconsin River discharge levels.The Portage lies about 116 river miles (187 km) from the Mississippi River and 162 river miles (261 km) from Green Bay.

text: The 2-mile (3 km) portage at Portage, Wisconsin is not unique as a passage between the Great Lakes and Mississippi River watersheds.  Similar passages exist all along the watershed divide, for instance, at

text: Chicago

text: and in the northern Indiana area..  What is unique is that, while the Fox is a small stream—typical of such passages—the Wisconsin is a large river, already over 300 miles (500 km) long. The divide between the two rivers has little grade change, although it is marshy.  The Wisconsin occasionally flowed across the Portage into the Fox during high water.  The Fox and Wisconsin have modified their courses and outlets over geological time  and it is likely that either river has flowed into either watershed.  Only about 2 miles (3 km) separate the two rivers. The Fox River end of the canal is at about elevation 780 feet (238 m) msl. The Wisconsin River end is slightly higher, depending on Wisconsin River discharge levels.The Portage lies about 116 river miles (187 km) from the Mississippi River and 162 river miles (261 km) from

text: Green Bay

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answers: NDQ_006063

answers: 780 feet

answers: NDQ_006064

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answers: NDQ_006065

answers: little grade change

answers: NDQ_006066

answers: The divide between the two rivers has little grade change

answers: NDQ_006067

answers: It is marshy

answers: NDQ_006068

answers: rivers provided water, plus

answers: NDQ_006069

answers: The divide between the two rivers has little grade change

text: The many mountains, streams and rivers form a major spawning ground for several species of trout and salmon; yet recently, in the last 50 years, some of the fish stocks have fallen drastically, particularly salmon stocks. The ecoregion's rivers and streams are home to nine species of native salmonids. The depletions occur mainly because dams and clearcutting on the rugged slopes of the area contribute to large amounts of silt in the stream beds, which in turn interfere with spawning salmon, as they lay their eggs in exposed gravel beds. The notable fish species are king, kokanee, and silver salmon, brown, brook, and rainbow trout (including steelhead), and crappie, bluegill, catfish, and largemouth and smallmouth bass.

text: The many mountains, streams and rivers form a major spawning ground for several species of trout and salmon; yet recently, in the last 50 years, some of the fish stocks have fallen drastically, particularly salmon stocks. The ecoregion's rivers and streams are home to nine species of native

text: salmonid

text: s. The depletions occur mainly because dams and clearcutting on the rugged slopes of the area contribute to large amounts of silt in the stream beds, which in turn interfere with spawning salmon, as they lay their eggs in exposed gravel beds. The notable fish species are

text: king

text: kokanee

text: , and

text: silver salmon

text: brown

text: brook

text: , and

text: rainbow trout

text: (including steelhead), and

text: crappie

text: bluegill

text: catfish

text: , and

text: largemouth

text: and

text: smallmouth bass

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answers: major spawning ground

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answers: a major spawning ground

answers: NDQ_006063

answers: native salmonids

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answers: ecoregion

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answers: large amounts of silt

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: no

answers: NDQ_006068

answers: major spawning ground for several species of trout and salmon

answers: NDQ_006069

answers: The many mountains, streams and rivers form a major spawning ground for several species of trout and salmon

text: The river has five tributaries: Green Lanes Stream, Ewell Court Stream, Horton Stream, Bonesgate Stream and Tolworth Brook, as well as Hogsmill Stream, the main spring of the river just outside Bourne Hall Park in Ewell.

text: The river has five tributaries: Green Lanes Stream, Ewell Court Stream, Horton Stream,

text: Bonesgate Stream

text: and Tolworth Brook, as well as Hogsmill Stream, the main spring of the river just outside Bourne Hall Park in

text: Ewell

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answers: tributaries

answers: NDQ_006061

answers: no

answers: NDQ_006062

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answers: NDQ_006063

answers: Tolworth Brook

answers: NDQ_006064

answers: spring

answers: NDQ_006065

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answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Hogsmill Stream

text: In a flowing stream, a riffle-pool sequence (also known as a pool-riffle sequence)  develops as a stream's hydrological flow structure alternates from areas of relatively shallow to deeper water. This sequence is present only in streams carrying gravel or coarser sediments. Riffles are formed in shallow areas by coarser materials, such as gravel deposits, over which water flows. Pools are deeper, calmer areas whose bed load (in general) is made up of finer material such as silt. Streams with only sand or silt laden beds do not develop the feature. The sequence within a stream bed commonly occurs at intervals of from 5 to 7 stream widths. Meandering streams with relatively coarse bed load tend to develop a riffle-pool sequence with pools in the outsides of the bends and riffles in the crossovers between one meander to the next on the opposite margin of the stream. The pools are areas of active erosion and the material eroded tends to be deposited in the riffle areas between them.

text: In a flowing

text: stream

text: , a riffle-pool sequence (also known as a pool-riffle sequence)  develops as a stream's hydrological flow structure alternates from areas of relatively shallow to deeper water. This sequence is present only in

text: stream

text: s carrying gravel or coarser

text: sediment

text: s.

text: Riffle

text: s are formed in shallow areas by coarser materials, such as

text: gravel

text: deposits, over which water flows. Pools are deeper, calmer areas whose

text: bed load

text: (in general) is made up of finer material such as silt. Streams with only

text: sand

text: or

text: silt

text: laden beds do not develop the feature. The sequence within a stream bed commonly occurs at intervals of from 5 to 7 stream widths.

text: Meandering streams

text: with relatively coarse bed load tend to develop a riffle-pool sequence with

text: pools

text: in the outsides of the bends and riffles in the crossovers between one

text: meander

text: to the next on the opposite margin of the stream. The pools are areas of active erosion and the material eroded tends to be deposited in the riffle areas between them.

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answers: crossovers

answers: NDQ_006061

answers: It does not

answers: NDQ_006062

answers: a pool-riffle sequence

answers: NDQ_006063

answers: water

answers: NDQ_006064

answers: riffle

answers: NDQ_006065

answers: active

answers: NDQ_006066

answers: This sequence is present only in streams carrying gravel or coarser sediments

answers: NDQ_006067

answers: This sequence is present only in streams carrying gravel or coarser sediments

answers: NDQ_006068

answers: a riffle-pool sequence

answers: NDQ_006069

answers: This sequence is present only in streams carrying gravel or coarser sediments

text: A foreset bed is one of the main parts of a river delta. It is the inclined part of a delta that is found at the end of the stream channel as the delta sediment is deposited along the arcuate delta front. As the sediments are deposited on a sloping surface the resulting bedding is not horizontal, but dips in the direction of current flow toward deeper water. A cross-section of a delta shows the cross bedding in the direction of stream flow into the still water.

text: A foreset bed is one of the main parts of a

text: river delta

text: . It is the inclined part of a delta that is found at the end of the stream channel as the delta

text: sediment

text: is deposited along the

text: arcuate delta

text: front. As the sediments are deposited on a sloping surface the resulting bedding is not horizontal, but

text: dips

text: in the direction of current flow toward deeper water. A cross-section of a delta shows the

text: cross bedding

text: in the direction of stream flow into the still water.

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text: A current, in a river or stream, is the flow of water influenced by gravity as the water moves downhill to reduce its potential energy. The current varies spatially as well as temporally within the stream, dependent upon the flow volume of water, stream gradient, and channel geometrics. In tidal zones, the current in rivers and streams may reverse on the flood tide before resuming on the ebb tide.

text: A current, in a

text: river

text: or

text: stream

text: , is the flow of

text: water

text: influenced by

text: gravity

text: as the water moves

text: downhill

text: to reduce its

text: potential energy

text: . The current varies

text: spatially

text: as well as

text: temporally

text: within the stream, dependent upon the flow

text: volume

text: of water,

text: stream gradient

text: , and

text: channel

text: geometrics. In

text: tidal zone

text: s, the current in rivers and streams may reverse on the flood tide before resuming on the

text: ebb tide

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answers: current varies spatially as well as temporally within the stream

text: Westchester County is divided into six primary drainage basins or watersheds which are: the Upper and Lower Long Island Sound; and the Bronx, Upper Hudson, Lower Hudson, and Croton River basins. Within these primary drainage basins are approximately 60 smaller basins, or subwatersheds. The principal streams draining the southern part of the county include Beaver Swamp Brook, Blind Brook, Bronx River, Hutchinson River, Mamaroneck River, Saw Mill River, Sheldrake River, Stephenson Brook and Tibbetts Brook. The primary streams draining the central part of the county include Byram River, Kisco River, Mianus River, Mill River, Pocantico River and Silvermine River. The principal streams draining the northern part of the county include Dickey Brook, Furnace Brook, Hallocks Mill Brook, Hunter Brook, Muscoot River, Peekskill Hollow Brook, and Titicus River. The county contains several major reservoirs; The Croton system and the Kensico Reservoir are important components of the New York City water supply system. The system is a series of interconnected reservoirs and lakes in northern Westchester and Putnam Counties that provide 10% of New York City's water under normal conditions and up to 30% in times of drought. The components of the system include the New Croton Reservoir, the Cross River Reservoir, the Titicus Reservoir, the Amawalk Reservoir, and the Muscoot Reservoir. Other major reservoirs are the Kensico and Byram Lake Reservoir, while there are a number of smaller reservoirs throughout the county.

text: Westchester County is divided into six primary

text: drainage basin

text: s or watersheds which are: the Upper and Lower Long Island Sound; and the Bronx, Upper Hudson, Lower Hudson, and Croton River basins. Within these primary drainage basins are approximately 60 smaller basins, or subwatersheds. The principal streams draining the southern part of the county include Beaver Swamp Brook, Blind Brook,

text: Bronx River

text: Hutchinson River

text: Mamaroneck River

text: Saw Mill River

text: , Sheldrake River, Stephenson Brook and Tibbetts Brook. The primary streams draining the central part of the county include

text: Byram River

text: , Kisco River,

text: Mianus River

text: , Mill River,

text: Pocantico River

text: and Silvermine River. The principal streams draining the northern part of the county include Dickey Brook, Furnace Brook, Hallocks Mill Brook, Hunter Brook, Muscoot River, Peekskill Hollow Brook, and

text: Titicus River

text: . The county contains several major reservoirs; The

text: Croton system

text: and the

text: Kensico Reservoir

text: are important components of the New York City water supply system. The system is a series of interconnected reservoirs and lakes in northern Westchester and Putnam Counties that provide 10% of New York City's water under normal conditions and up to 30% in times of drought. The components of the system include the

text: New Croton Reservoir

text: , the

text: Cross River Reservoir

text: , the

text: Titicus Reservoir

text: , the

text: Amawalk Reservoir

text: , and the

text: Muscoot Reservoir

text: . Other major reservoirs are the

text: Kensico

text: and Byram Lake Reservoir, while there are a number of smaller reservoirs throughout the county.

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answers: Croton River

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answers: no

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answers: Upper and Lower Long Island Sound

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answers: Long Island Sound

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answers: watershed

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answers: up to 30% in times of drought

answers: NDQ_006066

answers: The Croton system and the Kensico Reservoir

answers: NDQ_006067

answers: Lower Long Island Sound

answers: NDQ_006068

answers: New York City water supply system

answers: NDQ_006069

answers: The Croton system and the Kensico Reservoir are important components of the New York City water supply system

text: Flood stage is the water level, as read by a stream gauge or tide gauge, for a body of water at a particular location, measured from the level at which a body of water threatens lives, property, commerce, or travel. The term "at flood stage" is commonly used to describe the point at which this occurs. "Gauge height" (also referred to as "stream stage", "stage of the [body of water]", or simply "stage") is the level of the water surface above an established zero datum at a given location. The zero level can be arbitrary, but it is usually close to the bottom of the stream or river or at the average level of standing bodies of water. Stage was traditionally measured visually using a staff gauge, which is a fixed ruler marked in 1/100 and 1/10 foot intervals, however electronic sensors that transmit real-time information to the Internet are now used for many of these kind of measurements. The flood stage measurements are given as a height above or below the zero level. Levels below zero are reported as a negative value.

text: Flood stage is the water level, as read by a

text: stream gauge

text: or

text: tide gauge

text: , for a body of water at a particular location, measured from the level at which a body of water threatens lives, property,

text: commerce

text: , or travel. The term "at flood stage" is commonly used to describe the point at which this occurs. "Gauge height" (also referred to as "stream stage", "stage of the [body of water]", or simply "stage") is the level of the water surface above an established

text: zero datum

text: at a given location. The zero level can be

text: arbitrary

text: , but it is usually close to the bottom of the stream or river or at the average level of standing bodies of water. Stage was traditionally measured visually using a staff gauge, which is a fixed

text: ruler

text: marked in 1/100 and 1/10

text: foot

text: intervals, however electronic sensors that transmit real-time information to the

text: Internet

text: are now used for many of these kind of measurements. The flood stage measurements are given as a height above or below the zero level. Levels below zero are reported as a negative value.

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answers: Flood stage

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answers: It is not possible to tell

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answers: flood stage

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answers: zero

answers: NDQ_006064

answers: Flood stage

answers: NDQ_006065

answers: negative value

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answers: west side of the continental divide

answers: NDQ_006067

answers: The zero level can be arbitrary

answers: NDQ_006068

answers: commerce

answers: NDQ_006069

answers: The central valley of california

text: Besides being crossed by the Tunjuelo and Bogotá rivers Bosa also has the Tunjuelito river and numerous creeks and streams which include the Quebradas Limas (Limas Stream), Trompeta stream, La Estrella stream and El Infierno, Quiba, Calderón, Bebedero and Aguas Calientes creeks.

text: Besides being crossed by the Tunjuelo and Bogotá rivers Bosa also has the Tunjuelito river and numerous creeks and streams which include the Quebradas Limas (Limas Stream), Trompeta stream, La Estrella stream and El Infierno, Quiba, Calderón, Bebedero and Aguas Calientes creeks.

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answers: creek

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answers: creeks

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answers: Pacific Ocean

answers: NDQ_006067

answers: It's impossible to say

answers: NDQ_006068

answers: creeks

answers: NDQ_006069

answers: Quebradas Limas

text: Rattlesnake Creek is an approximately 95 mile stream that is a tributary to the Arkansas River in central Kansas. The head of the stream is in northern Kiowa County and it flows northeast through Edwards and Stafford Counties before converging with the Arkansas River in Rice County. The stream flows through Quivira National Wildlife Refuge dividing the refuge in half. The stream was officially named Rattlesnake Creek in 1971 by the Department of Interior; before 1971 it was called either Rattlesnake Creek, Salt Creek, or West Fork Rattlesnake Creek.

text: Rattlesnake Creek is an approximately 95 mile stream that is a tributary to the

text: Arkansas River

text: in central

text: Kansas

text: . The head of the stream is in northern

text: Kiowa County

text: and it flows northeast through

text: Edwards

text: and

text: Stafford

text: Counties before converging with the Arkansas River in

text: Rice County

text: . The stream flows through

text: Quivira National Wildlife Refuge

text: dividing the refuge in half. The stream was officially named Rattlesnake Creek in 1971 by the

text: Department of Interior

text: ; before 1971 it was called either Rattlesnake Creek, Salt Creek, or West Fork Rattlesnake Creek.

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answers: Quivira National Wildlife Refuge

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answers: No

answers: NDQ_006062

answers: Arkansas River

answers: NDQ_006063

answers: Arkansas River

answers: NDQ_006064

answers: head

answers: NDQ_006065

answers: approximately 95 mile

answers: NDQ_006066

answers: west side of the continental divide

answers: NDQ_006067

answers: Salt Creek

answers: NDQ_006068

answers: rivers provided water, plus

answers: NDQ_006069

answers: Arkansas River

text: A perennial stream or perennial river is a stream or river (channel) that has continuous flow in parts of its stream bed all year round during years of normal rainfall.  "Perennial" streams are contrasted with "intermittent" streams which normally cease flowing for weeks or months each year, and with "ephemeral" channels that  flow only for hours or days following rainfall. During unusually dry years, a normally perennial stream may cease flowing, becoming intermittent for days, weeks, or months depending on severity of the drought. The boundaries between perennial, intermittent, and ephemeral channels are indefinite, and subject to a variety of identification methods adopted by local governments, academics, and others with a need to classify stream-flow permanence.

text: A perennial stream or perennial river is a

text: stream

text: or

text: river

text: (channel) that has continuous flow in parts of its

text: stream bed

text: all year round during years of normal rainfall.  "Perennial" streams are contrasted with "intermittent" streams which normally cease flowing for weeks or months each year, and with "ephemeral" channels that  flow only for hours or days following rainfall. During unusually dry years, a normally perennial stream may cease flowing, becoming intermittent for days, weeks, or months depending on severity of the drought. The boundaries between perennial, intermittent, and ephemeral channels are indefinite, and subject to a variety of identification methods adopted by local governments, academics, and others with a need to classify stream-flow permanence.

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answers: river

answers: NDQ_006061

answers: It is not possible to tell

answers: NDQ_006062

answers: a perennial river

answers: NDQ_006063

answers: normal rainfall

answers: NDQ_006064

answers: perennial river

answers: NDQ_006065

answers: depending on severity of the drought

answers: NDQ_006066

answers: continental divide

answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: rainfall

answers: NDQ_006069

answers: normal rainfall

text: Another section of the park is The Shallows, a winding stream leading off the River Medway, with various gravel beds for crossing the river. It was at one stage part of the River Medway, with meanders which were sometimes shallow and therefore difficult to navigate with large boats. Since the river was used by canal craft, a navigable diversion was constructed around this section. The Shallows then became a quiet backwater stream which is gradually developing into marshland.

text: Another section of the park is The Shallows, a winding stream leading off the River Medway, with various gravel beds for crossing the river. It was at one stage part of the River Medway, with

text: meander

text: s which were sometimes shallow and therefore difficult to navigate with large boats. Since the river was used by canal craft, a navigable diversion was constructed around this section. The Shallows then became a quiet backwater stream which is gradually developing into marshland.

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answers: 4

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answers: 0

answers: NDQ_006060

answers: River Medway

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: a quiet backwater stream

answers: NDQ_006063

answers: gravel beds

answers: NDQ_006064

answers: backwater

answers: NDQ_006065

answers: gradually developing

answers: NDQ_006066

answers: River Medway

answers: NDQ_006067

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text: A floodplain or flood plain is an area of land adjacent to a stream or river that stretches from the banks of its channel to the base of the enclosing valley walls and experiences flooding during periods of high discharge. It includes the floodway, which consists of the stream channel and adjacent areas that actively carry flood flows downstream, and the flood fringe, which are areas inundated by the flood, but which do not experience a strong current.In other words, a floodplain is an area near a river or a stream which floods when the water level reaches flood stage.

text: A floodplain or flood plain is an area of land adjacent to a

text: stream

text: or

text: river

text: that stretches from the banks of its channel to the base of the enclosing valley walls and experiences

text: flood

text: ing during periods of high discharge. It includes the floodway, which consists of the stream

text: channel

text: and adjacent areas that actively carry flood flows downstream, and the flood fringe, which are areas inundated by the flood, but which do not experience a strong

text: current

text: .In other words, a floodplain is an area near a river or a stream which floods when the water level reaches

text: flood stage

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answers: It includes the floodway

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text: Near Bhola, just before flowing into the Bay of Bengal, the river divides into two main streams in the Ganges delta and separates an island from both sides of the mainland. The western stream is called Ilsha and the eastern one is called Bamni.

text: Near

text: Bhola

text: , just before flowing into the Bay of Bengal, the river divides into two main streams in the Ganges delta and separates an island from both sides of the mainland. The western stream is called Ilsha and the eastern one is called Bamni.

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answers: Bamni

text: Arnave was built on the banks of a stream by the same name. The source of this stream is at an approximate altitude of , at the foot of Mount Fourcat . It is fed by two other streams, the Ruisseau de la Sécaille and, further downstream, the Ruisseau de la Montagne. The former descends by way of Cazenave-Serres-et-Allens and its source is at  the base of le Pic du Han (). The source of the latter is further to the north and on the other side of the Cazenave mountain, at the Lauzate peak. The Arnave stream is also fed by other smaller streams and springs. The Arnave stream itself empties into the Ariege River four kilometres downstream from the town of Arnave, at the site of Bompas, Ariège.

text: Arnave was built on the banks of a stream by the same name. The source of this stream is at an approximate altitude of , at the foot of Mount Fourcat . It is fed by two other streams, the Ruisseau de la Sécaille and, further downstream, the Ruisseau de la Montagne. The former descends by way of

text: Cazenave-Serres-et-Allens

text: and its source is at  the base of le Pic du Han (). The source of the latter is further to the north and on the other side of the Cazenave mountain, at the Lauzate peak. The Arnave stream is also fed by other smaller streams and springs. The Arnave stream itself empties into the

text: Ariege River

text: four kilometres downstream from the town of Arnave, at the site of

text: Bompas, Ariège

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text: Ambedkarnagar district is located on the North-Eastern part of Uttar Pradesh. It lies between 26o 09‟ N to 26o 40‟ N latitudes and 82o 12‟ E to 83o 05‟ E longitudes. It is bounded on the north by Basti and Sant Kabir Nagar districts, on the north-east by Gorakhpur district, on the south by Sultanpur district, on the west by Faizabad district and on the east by Azamgarh district. The total area of the district is 2520 km². The total length of the district from east to west is approximately 75 km and the breadth from north to south is about 42 km. The district of Ambedkarnagar forms a part of the central Ganga basin. The soils of the Ambedkarnagar district are alluvium. The Saryu River is the main river and is located at the northern boundary of the district. The Tanda, Rajesultanpur, Ramnager and Baskhari blocks are located along this river and use its water for irrigation. Irrigation in the Baskhari block is also from Lake Devhat and the Rajesultanpur Lakes. Lake Darvan provides water in the Katehari block. The Akbarpur, Bhiti, Bhiyam, and Jalapur blocks depend upon smaller rivers and seasonal streams. The city of Akbarpur is situated on the bank of the River Tons (Tamasa), which divides the city into the two parts Akbarpur and Shahzadpur, with the latter being the main commercial centre of the city.

text: Ambedkarnagar district is located on the North-Eastern part of Uttar Pradesh. It lies between 26o 09‟ N to 26o 40‟ N latitudes and 82o 12‟ E to 83o 05‟ E longitudes. It is bounded on the north by Basti and Sant Kabir Nagar districts, on the north-east by Gorakhpur district, on the south by Sultanpur district, on the west by Faizabad district and on the east by Azamgarh district. The total area of the district is 2520 km². The total length of the district from east to west is approximately 75 km and the breadth from north to south is about 42 km. The district of Ambedkarnagar forms a part of the central Ganga basin. The soils of the Ambedkarnagar district are alluvium. The

text: Saryu River

text: is the main river and is located at the northern boundary of the district. The Tanda, Rajesultanpur, Ramnager and Baskhari blocks are located along this river and use its water for irrigation. Irrigation in the Baskhari block is also from Lake Devhat and the

text: Rajesultanpur

text: Lakes. Lake Darvan provides water in the Katehari block. The Akbarpur, Bhiti, Bhiyam, and Jalapur blocks depend upon smaller rivers and seasonal streams. The city of Akbarpur is situated on the bank of the River

text: Tons

text: Tamasa

text: ), which divides the city into the two parts Akbarpur and Shahzadpur, with the latter being the main commercial centre of the city.

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answers: The district of Ambedkarnagar forms a part of the central Ganga basin

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answers: irrigation

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answers: The district of Ambedkarnagar forms a part of the central Ganga basin

text: The base level of a river or stream is the lowest point to which it can flow, often referred to as the 'mouth of the river'. For large rivers, sea level is usually the base level, but a large river or lake is likewise the base level for tributary streams. All rivers and streams erode toward sea level, which is also known as the "ultimate base level." A rather rare exception can be seen in the Jordan River, for which the base level is the Dead Sea, 417 m below modern sea level. If a river is dammed, a new base level (the level of the reservoir) replaces the ultimate base level. As a result, the stream’s base level is raised. Consequently, this reduces the stream’s velocity, leads to deposition, and a reduction of the gradient upstream from the reservoir.

text: The base level of a

text: river

text: or

text: stream

text: is the lowest point to which it can flow, often referred to as the

text: 'mouth of the river'

text: . For large rivers,

text: sea level

text: is usually the base level, but a large river or

text: lake

text: is likewise the base level for tributary streams. All rivers and streams erode toward sea level, which is also known as the "ultimate base level." A rather rare exception can be seen in the

text: Jordan River

text: , for which the base level is the

text: Dead Sea

text: , 417 m below modern sea level. If a river is dammed, a new base level (the level of the reservoir) replaces the ultimate base level. As a result, the stream’s base level is raised. Consequently, this reduces the stream’s velocity, leads to deposition, and a reduction of the gradient upstream from the reservoir.

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answers: lowest point to which it can flow

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answers: For large rivers, sea level is usually the base level

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answers: This reduces the stream’s velocity

answers: NDQ_006068

answers: base level

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answers: The Jordan River

text: The community's name is based on its proximity to the Continental Divide. As a station on the Union Pacific Railroad, Divide served as a distribution and stock shipping point for ranchers in the Big Hole Valley.

text: The community's name is based on its proximity to the

text: Continental Divide

text: . As a station on the

text: Union Pacific Railroad

text: , Divide served as a distribution and stock shipping point for ranchers in the Big Hole Valley.

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answers: NDQ_006067

answers: The Continental Divide

answers: NDQ_006068

answers: the Continental Divide

answers: NDQ_006069

answers: a mild climate

text: Grassy Creek is a stream in the U.S. state of Missouri. It is a stream of the Salt River.

text: Grassy Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a stream of the

text: Salt River

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answers: NDQ_006069

answers: Salt River

text: The second largest right tributary of the Yenisei joins it near the town of Turukhansk. According to the character of the stream, constitution of the river's valley and its shores, it can be divided into two parts: the first one starts at the source of the river and continues down to the village Preobrazhenskoye and the second section of the river lies downstream of this village in a canyon-like relief.

text: The second largest right tributary of the

text: Yenisei

text: joins it near the town of

text: Turukhansk

text: . According to the character of the stream, constitution of the river's valley and its shores, it can be divided into two parts: the first one starts at the source of the river and continues down to the village

text: Preobrazhenskoye

text: and the second section of the river lies downstream of this village in a canyon-like relief.

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answers: According to the character

answers: NDQ_006066

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answers: NDQ_006067

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answers: NDQ_006068

answers: river's valley

answers: NDQ_006069

answers: Preobrazhenskoye

text: Joining the Shenandoah Valley to the Piedmont region of the state, it is the site of the mountain crossing of Interstate 64, U.S. Route 250, and the former Blue Ridge Railroad which later became part of the Chesapeake and Ohio Railway and is currently part of the CSX line.  With an elevation of about , it is one of the lowest gaps between Manassas Gap and the James River.  Rockfish Gap lies along a drainage divide between southeast-flowing streams that drain to the James River and northwest-flowing streams in the Shenandoah River system.

text: Joining the

text: Shenandoah Valley

text: to the Piedmont region of the state, it is the site of the mountain crossing of

text: Interstate 64

text: U.S. Route 250

text: , and the former

text: Blue Ridge Railroad

text: which later became part of the

text: Chesapeake and Ohio Railway

text: and is currently part of the CSX line.  With an elevation of about , it is one of the lowest gaps between

text: Manassas Gap

text: and the

text: James River

text: .  Rockfish Gap lies along a drainage divide between southeast-flowing streams that drain to the James River and northwest-flowing streams in the Shenandoah River system.

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answers: NDQ_006068

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answers: NDQ_006069

answers: Shenandoah Valley

text: To qualify as a stream it must be either recurring or perennial. Recurring (intermittent) streams have water in the channel for at least part of the year. A stream of the first order is a stream which does not have any other recurring or perennial stream feeding into it. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream. Streams of lower order joining a higher order stream do not change the order of the higher stream. Thus, if a first-order stream joins a second-order stream, it remains a second-order stream. It is not until a second-order stream combines with another second-order stream that it becomes a third-order stream.

text: To qualify as a stream it must be either recurring or perennial. Recurring (

text: intermittent

text: ) streams have water in the channel for at least part of the year. A stream of the

text: first order

text: is a stream which does not have any other recurring or perennial stream feeding into it. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream. Streams of lower order joining a higher order stream do not change the order of the higher stream. Thus, if a first-order stream joins a second-order stream, it remains a second-order stream. It is not until a second-order stream combines with another second-order stream that it becomes a third-order stream.

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answers: third-order stream

answers: NDQ_006061

answers: A stream of the first order

answers: NDQ_006062

answers: third-order stream

answers: NDQ_006063

answers: water

answers: NDQ_006064

answers: At least part of the year

answers: NDQ_006065

answers: part of the year

answers: NDQ_006066

answers: When two second-order streams come together, they form a third-order stream

answers: NDQ_006067

answers: Fresh water streams do not flow into the salty ocean

answers: NDQ_006068

answers: Recurring (intermittent) streams

answers: NDQ_006069

answers: Recurring (intermittent) streams

text: Begbrook is a suburb of Bristol. It is named after the eponymous stream, which is a tributary of the Frome river.

text: Begbrook is a suburb of

text: Bristol

text: . It is named after the eponymous stream, which is a

text: tributary

text: of the

text: Frome

text: river.

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answers: NDQ_006063

answers: Bristol

answers: NDQ_006064

answers: tributary

answers: NDQ_006065

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answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: The Frome river

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: Begbrook

text: Yellow barbs are found in streams in the upper catchment of river basins, usually with rocky stream beds.

text: Yellow barbs are found in streams in the upper catchment of river basins, usually with rocky stream beds.

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text: Guimarães is part of the drainage basin of Ave river which divides the municipality in half. The Ave river has as tributaries the Vizela river, Torto river, Febras river and inside the city, the Selho river, the Couros river and the Santa Lúzia stream.

text: Guimarães is part of the

text: drainage basin

text: of

text: Ave river

text: which divides the municipality in half. The Ave river has as tributaries the Vizela river, Torto river, Febras river and inside the city, the Selho river, the Couros river and the Santa Lúzia stream.

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text: The river channel typically contains a single stream of water, but some rivers flow as several interconnecting streams of water, producing a braided river. Extensive braided rivers are now found in only a few regions worldwide, such as the South Island of New Zealand. They also occur on peneplains and some of the larger river deltas. Anastamosing rivers are similar to braided rivers and are also quite rare. They have multiple sinuous channels carrying large volumes of sediment. There are rare cases of river bifurcation in which a river divides and the resultant flows ending in different seas. An example is the bifurcation of Nerodime River in Kosovo.

text: The river channel typically contains a single stream of water, but some rivers flow as several interconnecting streams of water, producing a

text: braided river

text: . Extensive braided rivers are now found in only a few regions worldwide, such as the

text: South Island

text: of

text: New Zealand

text: . They also occur on

text: peneplain

text: s and some of the larger river deltas.

text: Anastamosing rivers

text: are similar to braided rivers and are also quite rare. They have multiple sinuous channels carrying large volumes of sediment. There are rare cases of

text: river bifurcation

text: in which a river divides and the resultant flows ending in different seas. An example is the

text: bifurcation of Nerodime River

text: in

text: Kosovo

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text: Similarly, a knowledge model of a process is basically a specification of the sequence of process stages. This sequence is determined by the fact that a kind of stream is output of a kind of process stage, whereas that same type of stream in input in the next process stage. So the defined streams have roles as inputs to process stages, whereas the same streams are outputs of other process stages. For example:

text: Similarly, a knowledge model of a process is basically a specification of the sequence of process stages. This sequence is determined by the fact that a kind of stream is output of a kind of process stage, whereas that same type of stream in input in the next process stage. So the defined streams have roles as inputs to process stages, whereas the same streams are outputs of other process stages. For example:

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answers: No

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answers: knowledge model of a process

text: Szinva is a stream in northern Hungary, a tributary to the river Sajó. It originates in the Bükk Mountains. It is 30 kilometres long, 20 kilometres of which can be found the city of Miskolc, through which the stream flows from west to east. More than 70 bridges were built over the stream, and in parts of the city centre it flows underground.

text: Szinva is a

text: stream

text: in northern

text: Hungary

text: , a

text: tributary

text: to the river

text: Sajó

text: . It originates in the

text: Bükk

text: Mountains. It is 30 kilometres long, 20 kilometres of which can be found the city of

text: Miskolc

text: , through which the stream flows from west to east. More than 70 bridges were built over the stream, and in parts of the city centre it flows underground.

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answers: It originates in the Bükk Mountains

text: River bifurcation may be temporary or semi-permanent, depending on the strength of the material which separates the distributaries. For example, a mid-stream island of soil or silt in a delta is most likely temporary. A location where a river divides around a rock fin, e.g. a volcanically formed dike, or a mountain, may be more lasting. A bifurcation may also be man-made, for example when two streams are separated by a long bridge pier.

text: River bifurcation may be temporary or semi-permanent, depending on the strength of the material which separates the distributaries. For example, a mid-stream island of soil or silt in a delta is most likely temporary. A location where a river divides around a rock fin, e.g. a volcanically formed

text: dike

text: , or a mountain, may be more lasting. A bifurcation may also be man-made, for example when two streams are separated by a long

text: bridge

text: pier.

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answers: river bifurcation may also be man-made

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answers: A location where a river divides around a rock fin

text: Pembroke's geography can be divided in half.  The northern half is dominated by the rivers and streams of the area, flowing through thick forests which once provided the lumber for the North River's shipbuilding industry.  The southern half is dominated by several ponds and Silver Lake, where the towns of Pembroke, Kingston, Plympton and Halifax come together.  The town has its own municipal forest, which is divided into sections around town.

text: Pembroke's geography can be divided in half.  The northern half is dominated by the rivers and streams of the area, flowing through thick forests which once provided the lumber for the

text: North River

text: 's shipbuilding industry.  The southern half is dominated by several ponds and

entity_name: Silver Lake (Plymouth County, Massachusetts)

text: Silver Lake

text: , where the towns of Pembroke, Kingston, Plympton and Halifax come together.  The town has its own municipal forest, which is divided into sections around town.

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answers: rivers and streams

text: Most of the state’s surface freshwater is in the south and southwest, with rivers, small lakes and estuaries. These diminish in the north where rainfall rapidly filtrates into the subsoil.  The rivers in the south and southwest belong to various basins, with the largest being the Grijalva-Usumacinta to which the Candelaria, Chumpán and Mamantal Rivers belong.  The Usumacinta also flows in the state but it tends to change course frequently and occasionally divides into branches.  The east branch of this river is also called the Palizada River, which has the largest volume although it is narrow.  The San Pedro River is another branch is the Usumacinta, which passes by the community of Jonuta in Tabasco before emptying in the Gulf.  The Chumpán River is an isolated river formed by the union of various streams. It runs north-south and empties in the Laguna de Terminos. The Candelaria River forms in Petén, Guatemala and runs north-south and empties into the Laguna de Pargos.  The Mamantel River empties into the Laguna de Panlau. The Campotón River  is in the center of the state and empties into the Gulf.  The rest of the states streams flow only in the rainy season.

text: Most of the state’s surface freshwater is in the south and southwest, with rivers, small lakes and estuaries. These diminish in the north where rainfall rapidly filtrates into the subsoil.  The rivers in the south and southwest belong to various basins, with the largest being the

text: Grijalva

text: Usumacinta

text: to which the Candelaria, Chumpán and Mamantal Rivers belong.  The Usumacinta also flows in the state but it tends to change course frequently and occasionally divides into branches.  The east branch of this river is also called the Palizada River, which has the largest volume although it is narrow.  The San Pedro River is another branch is the Usumacinta, which passes by the community of Jonuta in Tabasco before emptying in the Gulf.  The Chumpán River is an isolated river formed by the union of various streams. It runs north-south and empties in the Laguna de Terminos. The Candelaria River forms in Petén, Guatemala and runs north-south and empties into the Laguna de Pargos.  The Mamantel River empties into the Laguna de Panlau. The Campotón River  is in the center of the state and empties into the Gulf.  The rest of the states streams flow only in the rainy season.

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answers: Chumpán River

answers: NDQ_006061

answers: It runs north-south

answers: NDQ_006062

answers: estuaries

answers: NDQ_006063

answers: subsoil

answers: NDQ_006064

answers: basin

answers: NDQ_006065

answers: changes course frequently and occasionally divides into branches

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Gulf

answers: NDQ_006068

answers: The Chumpán River

answers: NDQ_006069

answers: The rest of the states streams flow only in the rainy season

text: In the Lesser Stream passage of Goyden Pot the many fractures in the rock allows the stream to diverge and flow in different directions.  Sandstone boulders are washed in from the surface through the numerous inlets in this area. These inlets are also opened and closed through the action of flooding. The various streams quickly unite and flow amongst the large boulders that form the floor of yet another impressive large breakdown chamber, Goyden Main Chamber. The stream then flows out from under the boulders and over the cascades to flow along the huge Main Stream Passage, 25m high in places and typically 6m wide for more than 150m, to where it flows into sump 1, 20m long. The river flows out of sump 1 past October Passage, which steals a small amount of the river.  It then flows along another huge gallery into sump 2, 6m long. From there the river flows along the largest of the stream passages in Goyden to sump 3, 27m long. Here the river flows into Bridge Hall, where a small inlet on the left enters, probably the water from October Passage but as yet unconfirmed. At the far side of Bridge Hall is sump 4, just 2m long, and then a short section of passage to sump 5, about 57m long, and a lake airbell with choked inlet in the roof. Sump 6, 12m long, leads from the airbell to a short passage with a roof passage leading into the Aquamole series that can be entered via Frog Pot. At the end of the short passage sump 7 is a low obstructed sump that connects with the upstream sump 2 and sump 1 of New Goyden Pot.

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answers: Goyden Main Chamber

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answers: no

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answers: Goyden Main Chamber

answers: NDQ_006063

answers: Goyden

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answers: Goyden

answers: NDQ_006065

answers: flowing in different directions

answers: NDQ_006066

answers: Goyden

answers: NDQ_006067

answers: Goyden Main Chamber

answers: NDQ_006068

answers: sandstone boulders

answers: NDQ_006069

answers: Goyden Main Chamber

text: The Horn drains to the northeast into Redington Stream, then into the South Branch of the Dead River, the Kennebec River, and into the Gulf of Maine. The Horn drains to the west into Saddleback Lake, then into Redington Stream. The Horn drains to the south into Winship Stream, then into Conant Stream, Orbeton Stream, and the Sandy River, another tributary of the Kennebec. The Horn drains to the southeast into Hardy Stream, then into Orbeton Stream.

text: The Horn drains to the northeast into Redington Stream, then into the

text: South Branch

text: of the

text: Dead River

text: , the

text: Kennebec River

text: , and into the

text: Gulf of Maine

text: . The Horn drains to the west into Saddleback Lake, then into Redington Stream. The Horn drains to the south into Winship Stream, then into Conant Stream, Orbeton Stream, and the

text: Sandy River

text: , another

text: tributary

text: of the Kennebec. The Horn drains to the southeast into Hardy Stream, then into Orbeton Stream.

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answers: Saddleback Lake

answers: NDQ_006061

answers: no

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answers: NDQ_006063

answers: Saddleback Lake

answers: NDQ_006064

answers: tributary

answers: NDQ_006065

answers: tributary

answers: NDQ_006066

answers: Gulf of Maine

answers: NDQ_006067

answers: Gulf of Maine

answers: NDQ_006068

answers: the Kennebec River

answers: NDQ_006069

answers: the Kennebec River

text: Cobre River, Santa Elena Stream, De las Cargas Stream, Tiburcio Stream, Valenzuela River, Montañez River, Del Yeso Stream, El Seguro Stream, Los Ángeles Stream, Pichú Trolón Stream, Chico River and Potimalal River.

text: Cobre River

text: , Santa Elena

text: Stream

text: , De las Cargas Stream, Tiburcio Stream,

text: Valenzuela River

text: Montañez River

text: , Del Yeso Stream, El Seguro Stream, Los Ángeles Stream, Pichú Trolón Stream,

text: Chico River

text: and

text: Potimalal River

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answers: Valenzuela River

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answers: no

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answers: NDQ_006063

answers: river

answers: NDQ_006064

answers: Potimalal

answers: NDQ_006065

answers: erodes

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: Streams

answers: NDQ_006069

answers: Streams

text: The North Branch Blackwater River is a  river in Squa Pan Township (Township 10, Range 4, WELS), Aroostook County, Maine. From its source (), the stream runs west to its confluence with the South Branch to form the Blackwater River. Via the Blackwater River, St. Croix Stream, and the Aroostook River, the North Branch is part of the Saint John River watershed.

text: The North Branch Blackwater River is a  river in Squa Pan Township (Township 10, Range 4, WELS),

text: Aroostook County

text: Maine

text: . From its source (), the stream runs west to its

text: confluence

text: with the

text: South Branch

text: to form the

text: Blackwater River

text: . Via the Blackwater River,

text: St. Croix Stream

text: , and the

text: Aroostook River

text: , the North Branch is part of the

text: Saint John River

text: watershed.

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answers: Blackwater River

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Saint John River

answers: NDQ_006063

answers: Blackwater River

answers: NDQ_006064

answers: source

answers: NDQ_006065

answers: from its source

answers: NDQ_006066

answers: Atlantic Ocean

answers: NDQ_006067

answers: Saint John River

answers: NDQ_006068

answers: Blackwater River

answers: NDQ_006069

answers: Blackwater River

text: Tordillo River, De la Pampa Stream, Del Infiernillo Stream, Del Totoral Stream, Carilaufquen Stream, De la Yesera Stream, Chacai-có Stream, Chequenco Stream and Agua Botada Stream.

text: Tordillo River

text: , De la Pampa Stream, Del Infiernillo Stream, Del Totoral Stream, Carilaufquen Stream, De la Yesera Stream, Chacai-có Stream, Chequenco Stream and Agua Botada Stream.

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answers: Tordillo River

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Pacific Ocean

answers: NDQ_006063

answers: De la Yesera

answers: NDQ_006064

answers: River

answers: NDQ_006065

answers: erodes

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: Streams

answers: NDQ_006069

answers: Streams

text: Pumpkinvine Creek is a stream in the U.S. state of Georgia. It is a tributary of the Etowah River.

text: Pumpkinvine Creek is a stream in the

text: U.S. state

text: of

text: Georgia

text: . It is a tributary of the

text: Etowah River

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answers: tributary

answers: NDQ_006061

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answers: NDQ_006063

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answers: NDQ_006064

answers: tributary

answers: NDQ_006065

answers: tributary

answers: NDQ_006066

answers: Atlantic Ocean

answers: NDQ_006067

answers: The salty ocean

answers: NDQ_006068

answers: the Etowah River

answers: NDQ_006069

answers: Pumpkinvine Creek

text: The east side of Baker Mountain drains into Baker Mountain Brook, then into the West Branch of the Pleasant River, the Piscataquis River, the Penobscot River, and into Penobscot Bay. The southwest side of Baker Mountain drains into North Brook, then into Upper and Lower Wilson Ponds, Eagle Stream, Big Wilson Stream, Sebec Lake, and the Sebec River, another tributary of the Piscataquis River. The northwest side of Baker Mountain drains into South Brook, then into Moosehead Lake, the source of the Kennebec River, which drains into the Gulf of Maine.

text: The east side of Baker Mountain drains into Baker Mountain Brook, then into the

entity_name: West Branch Pleasant River (Piscataquis River)

text: West Branch

text: of the

text: Pleasant River

text: , the

text: Piscataquis River

text: , the

text: Penobscot River

text: , and into

text: Penobscot Bay

text: . The southwest side of Baker Mountain drains into North Brook, then into Upper and Lower Wilson Ponds, Eagle Stream, Big Wilson Stream,

text: Sebec Lake

text: , and the

text: Sebec River

text: , another

text: tributary

text: of the Piscataquis River. The northwest side of Baker Mountain drains into South Brook, then into

text: Moosehead Lake

text: , the source of the

text: Kennebec River

text: , which drains into the

text: Gulf of Maine

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answers: Moosehead Lake

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Gulf of Maine

answers: NDQ_006063

answers: Bay

answers: NDQ_006064

answers: Brook

answers: NDQ_006065

answers: drains

answers: NDQ_006066

answers: Gulf of Maine

answers: NDQ_006067

answers: Gulf of Maine

answers: NDQ_006068

answers: Moosehead Lake

answers: NDQ_006069

answers: The southwest side of Baker Mountain drains into Baker Mountain Brook

text: A losing stream, disappearing stream or influent stream, is a stream or river that loses water  as it flows downstream. The water infiltrates into the ground recharging the local groundwater, because the water table is below the bottom of the stream channel. This is the opposite of a more common gaining  stream (or effluent stream) which increases in water volume farther down stream as it gains water from the local aquifer.

text: A losing stream, disappearing stream or influent stream, is a

text: stream

text: or

text: river

text: that loses water  as it flows downstream. The water

text: infiltrates

text: into the ground recharging the local

text: groundwater

text: , because the

text: water table

text: is below the bottom of the stream channel. This is the opposite of a more common gaining  stream (or effluent stream) which increases in water volume farther down stream as it gains water from the local

text: aquifer

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answers: infiltrates into the ground

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answers: Losing stream

text: Cope Branch is a stream in the U.S. state of Missouri. It is a tributary of the Little Black River.

text: Cope Branch is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the Little Black River.

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answers: Cope Branch

text: Based on river stream regions, the Ngaju people are divided into:-

text: Based on river stream regions, the Ngaju people are divided into:-

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answers: river stream regions

text: Streams flowing south from the Calapooyas into the North Umpqua River include Steamboat, Canton, and Rock creeks, while Calapooya Creek flows west from the divide into the Umpqua main stem. Streams flowing north or east into the Middle Fork Willamette River include Tumblebug, Staley, Coal, and Packard creeks. Flowing northwest or west into the Coast Fork Willamette River or its major tributary, the Row River, are Brice, Layng, and Mosby creeks and Big River. The Umpqua flows west through the Oregon Coast Range to the Pacific Ocean at Reedsport, while the Willamette flows north to the Columbia River, which flows northwest to the Pacific Ocean at Astoria.

text: Streams flowing south from the Calapooyas into the North Umpqua River include Steamboat, Canton, and Rock creeks, while

text: Calapooya Creek

text: flows west from the divide into the Umpqua main stem. Streams flowing north or east into the Middle Fork Willamette River include Tumblebug, Staley, Coal, and Packard creeks. Flowing northwest or west into the Coast Fork Willamette River or its major tributary, the

text: Row River

text: , are Brice, Layng, and

text: Mosby

text: creeks and

text: Big River

text: . The Umpqua flows west through the

text: Oregon Coast Range

text: to the Pacific Ocean at

text: Reedsport

text: , while the Willamette flows north to the

text: Columbia River

text: , which flows northwest to the Pacific Ocean at

text: Astoria

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answers: NDQ_006064

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answers: NDQ_006067

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answers: Rivers

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answers: Calapooyas

text: The Lane River is an  stream located in central New Hampshire in the United States.  It is a tributary of the Warner River, part of the Contoocook River (and ultimately Merrimack River) watershed.

text: The Lane River is an

text: stream

text: located in central

text: New Hampshire

text: in the

text: United States

text: .  It is a

text: tributary

text: of the

text: Warner River

text: , part of the

text: Contoocook River

text: (and ultimately

text: Merrimack River

text: watershed

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answers: The Lane River

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answers: NDQ_006069

answers: The Lane River

text: The Mokelumne watershed divide borders the basins of the American River on the north, the Calaveras and Stanislaus rivers to the south, and the Carson River to the east. The American, Calaveras and Stanislaus rivers, like the Mokelumne, drain westwards into the Central Valley, while the Carson flows eastwards into the Great Basin. Drainage within the Mokelumne watershed generally occurs from east to west with all of the perennial streams originating in the Sierra Nevada.

text: The Mokelumne watershed divide borders the basins of the

text: American River

text: on the north, the

text: Calaveras

text: and

text: Stanislaus

text: rivers to the south, and the

text: Carson River

text: to the east. The American, Calaveras and Stanislaus rivers, like the Mokelumne, drain westwards into the Central Valley, while the Carson flows eastwards into the

text: Great Basin

text: . Drainage within the Mokelumne watershed generally occurs from east to west with all of the

text: perennial stream

text: s originating in the Sierra Nevada.

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answers: NDQ_006068

answers: Rivers

answers: NDQ_006069

answers: the Sierra Nevada

text: There is a small stream known as Canacadea Creek, that flows throughout the year from south to north. This stream flows to the Canisteo River which is a tributary to the Susquehanna River watershed. The topography is steep hill country as it is part of the Allegheny Plateau, being the northern part of the Appalachian Mountain chain.

text: There is a small stream known as Canacadea Creek, that flows throughout the year from south to north. This stream flows to the Canisteo River which is a tributary to the Susquehanna River watershed. The topography is steep hill country as it is part of the Allegheny Plateau, being the northern part of the Appalachian Mountain chain.

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answers: NDQ_006067

answers: Canacadea Creek

answers: NDQ_006068

answers: Canisteo River

answers: NDQ_006069

answers: Canacadea Creek

text: This stream heads in Alaska and has a length, after crossing into Canadian territory measured along the valley, of about , and following the windings of the stream, of about  in total. Its fall, measured roughly with the barometer, from the boundary to the Yukon, amounts to , and the average grade of the valley to a little over  to the mile. At the international boundary, it is a rapid winding stream averaging about  in width and interrupted at frequent intervals by steep bars covered with only a few inches of water. The upper portion of the river from the boundary to California creek can hardly be considered a navigable stream even for small boats. Below California creek, the volume of water increases and the descent becomes less difficult, but bars and rapids continue almost to the mouth and no part of the river is easy to ascend. The tributary streams are small, as a rule, but two large streams, one draining the country to the west and one other to the south, come in within four miles of each other, nearly opposite Indian River, and these branches nearly double the volume of the main river. Towards its mouth, Sixtymile has an average width of from . Below Sixtymile, the Yukon contains many islands.

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answers: NDQ_006063

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answers: NDQ_006064

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answers: NDQ_006065

answers: average grade

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Its fall, measured roughly with the barometer

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: a few inches of water

text: Moxie Mountain stands within the watershed of the Kennebec River, which drains into the Gulf of Maine.The northeast side of Moxie Mtn. drains into Big and Little Dimmick Ponds, then into Baker Pond, Moxie Pond, Moxie Stream, and into the Kennebec River. The north side of Moxie drains into Pleasant Pond, then into Pleasant Pond Stream, and into the Kennebec River. The west side of Moxie drains into Robinson Pond Outlet, then into Pleasant Pond Stream. The south side of Moxie drains into Heald Stream, then into Austin Stream and the Kennebec River.

text: Moxie Mountain stands within the

text: watershed

text: of the

text: Kennebec River

text: , which drains into the

text: Gulf of Maine

text: .The northeast side of Moxie Mtn. drains into Big and Little Dimmick Ponds, then into Baker Pond, Moxie Pond, Moxie Stream, and into the Kennebec River. The north side of Moxie drains into Pleasant Pond, then into Pleasant Pond Stream, and into the Kennebec River. The west side of Moxie drains into Robinson Pond Outlet, then into Pleasant Pond Stream. The south side of Moxie drains into Heald Stream, then into Austin Stream and the Kennebec River.

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text: Subterranean rivers can also be the  result of covering over a river and/or diverting its flow into culverts, usually as part of urban development. Reversing this process is known as daylighting a stream and is a visible form of river restoration.  One successful example is the Cheonggye Stream in the centre of Seoul.

text: Subterranean rivers can also be the  result of covering over a river and/or diverting its flow into

text: culvert

text: s, usually as part of

text: urban development

text: . Reversing this process is known as

text: daylighting a stream

text: and is a visible form of river restoration.  One successful example is the

text: Cheonggye Stream

text: in the centre of

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text: DEFLATE specifies a stream-encoding such that any compliant decoder is able to parse any valid stream;  the algorithm and program used for the compression stage are not mandated.

text: DEFLATE

text: specifies a stream-

text: encoding

text: such that any compliant decoder is able to parse any valid stream;  the algorithm and program used for the compression stage are not mandated.

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answers: DEFLATE specifies a stream-encoding

text: The extent of land basin drained by a stream is termed its drainage basin (also known in North America as the watershed and, in British English, as a catchment). A basin may also be composed of smaller basins.  For instance, the Continental Divide in North America divides the mainly easterly-draining Atlantic Ocean and Arctic Ocean basins  from the largely westerly-flowing Pacific Ocean basin. The Atlantic Ocean basin, however, may be further subdivided into the Atlantic Ocean and Gulf of Mexico drainages. (This delineation is termed the Eastern Continental Divide.) Similarly, the Gulf of Mexico basin may be divided into the Mississippi River basin and several smaller basins, such as the Tombigbee River basin. Continuing in this vein, a component of the Mississippi River basin is the Ohio River basin, which in turn includes the Kentucky River basin, and so forth.

text: The extent of land basin drained by a stream is termed its

text: drainage basin

text: (also known in North America as the watershed and, in British English, as a catchment). A basin may also be composed of smaller basins.  For instance, the

text: Continental Divide

text: in North America divides the mainly easterly-draining

text: Atlantic Ocean

text: and

text: Arctic Ocean

text: basins  from the largely westerly-flowing

text: Pacific Ocean

text: basin. The Atlantic Ocean basin, however, may be further subdivided into the Atlantic Ocean and

text: Gulf of Mexico

text: drainages. (This delineation is termed the

text: Eastern Continental Divide

text: .) Similarly, the Gulf of Mexico basin may be divided into the

text: Mississippi River

text: basin and several smaller basins, such as the

text: Tombigbee River

text: basin. Continuing in this vein, a component of the Mississippi River basin is the

text: Ohio River

text: basin, which in turn includes the

text: Kentucky River

text: basin, and so forth.

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answers: NDQ_006069

answers: A basin may also be composed of smaller basins

text: The Becaguimec Stream is a minor tributary of the Saint John River in the Canadian Province of New Brunswick. It rises in the hilly,woods along the county line dividing Carleton County, Canada from York County, Canada in the western region of the province. Its watershed is adjacent to the South Branch of the Southwest Miramichi River, the Nashwaak River, the Keswick River and the Nackawic Stream.

text: The Becaguimec Stream is a minor

text: tributary

text: of the

text: Saint John River

text: in the Canadian Province of

text: New Brunswick

text: . It rises in the hilly,woods along the county line dividing

text: Carleton County, Canada

text: from

text: York County, Canada

text: in the western region of the province. Its watershed is adjacent to the South Branch of the Southwest

text: Miramichi River

text: , the

text: Nashwaak River

text: , the

text: Keswick River

text: and the

text: Nackawic Stream

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answers: NDQ_006069

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answers: NDQ_006060

answers: Saint John River

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Saint John River

answers: NDQ_006063

answers: Saint John River

answers: NDQ_006064

answers: hilly

answers: NDQ_006065

answers: minor

answers: NDQ_006066

answers: Atlantic Ocean

answers: NDQ_006067

answers: Saint John River

answers: NDQ_006068

answers: Saint John River

answers: NDQ_006069

answers: Saint John River

text: The largescale stoneroller is found natively in many of North American streams, rivers, lakes, and creeks. It is native to the Upper Mississippi River and Lake Michigan drainages of Wisconsin, eastern Minnesota, eastern Iowa, and northern Illinois; Ozarkian streams of central and southern Missouri, and northern Arkansas; Mobile Bay drainage, Georgia, Alabama, and eastern Mississippi; parts of Green, Cumberland, and Tennessee River drainages of Kentucky, Tennessee, Georgia, and Alabama   It has also been introduced into other areas in North America like the Illinois River in Oklahoma. It is thought that the reason for their introduction into the Oklahoma is due to the fact that it is a popular baitfish, and has effects on this area in ways that have not been noticed by scientist and researchers. The largescale stoneroller ranges from Alabama to Oklahoma.

text: The largescale stoneroller is found natively in many of North American streams, rivers, lakes, and creeks. It is native to the Upper Mississippi River and Lake Michigan drainages of Wisconsin, eastern Minnesota, eastern Iowa, and northern Illinois; Ozarkian streams of central and southern Missouri, and northern Arkansas; Mobile Bay drainage, Georgia, Alabama, and eastern Mississippi; parts of Green, Cumberland, and Tennessee River drainages of Kentucky, Tennessee, Georgia, and Alabama   It has also been introduced into other areas in North America like the Illinois River in Oklahoma. It is thought that the reason for their introduction into the Oklahoma is due to the fact that it is a popular baitfish, and has effects on this area in ways that have not been noticed by scientist and researchers. The largescale stoneroller ranges from Alabama to Oklahoma.

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answers: 4

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answers: Mobile Bay drainage

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Mobile Bay drainage

answers: NDQ_006063

answers: it is a popular baitfish

answers: NDQ_006064

answers: Ozarkian

answers: NDQ_006065

answers: effects on this area

answers: NDQ_006066

answers: The largescale stoneroller ranges from Alabama to Oklahoma

answers: NDQ_006067

answers: The largescale stoneroller

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The largescale stoneroller ranges from Alabama to Oklahoma

text: Apart from a very short stretch of coastline on the Gulf of Aqaba, Jordan is a landlocked country. It largely consists of an elevated plateau  high, divided into ridges by valleys and gorges. The eastern part of the country is desert and merges into the Syrian Desert and the northern part of the Arabian Desert. There are some oases here and some seasonal streams. The western part of the country is more mountainous with a natural vegetation of Mediterranean evergreen forest. The western border is the Jordan Rift Valley, where the Jordan River and the Dead Sea lie hundreds of feet below sea level and form the boundary between Jordan, to the east, and Israel and the Palestinian territories to the west.

text: Apart from a very short stretch of coastline on the

text: Gulf of Aqaba

text: , Jordan is a landlocked country. It largely consists of an elevated plateau  high, divided into ridges by valleys and gorges. The eastern part of the country is desert and merges into the

text: Syrian Desert

text: and the northern part of the

text: Arabian Desert

text: . There are some oases here and some seasonal streams. The western part of the country is more mountainous with a natural vegetation of Mediterranean evergreen forest. The western border is the

text: Jordan Rift Valley

text: , where the

text: Jordan River

text: and the

text: Dead Sea

text: lie hundreds of feet below sea level and form the boundary between Jordan, to the east, and

text: Israel

text: and the

text: Palestinian territories

text: to the west.

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answers: NDQ_006069

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answers: NDQ_006060

answers: Jordan Rift Valley

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Gulf of Aqaba

answers: NDQ_006063

answers: sea level

answers: NDQ_006064

answers: oases

answers: NDQ_006065

answers: seasonal

answers: NDQ_006066

answers: Gulf of Aqaba

answers: NDQ_006067

answers: Dead Sea

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Mediterranean evergreen forest

text: The river's name comes from Thracian Strymón, derived from IE *sru "stream", akin to English stream, Old Irish sruaimm "river", Polish strumień "stream", Lithuanian straumuoe "fast stream", Greek reuma "stream", Albanian rrymë "water flow", shri "rain".

text: The river's name comes from Thracian Strymón, derived from IE *sru "stream", akin to English stream, Old Irish sruaimm "river", Polish strumień "stream", Lithuanian straumuoe "fast stream", Greek reuma "stream", Albanian rrymë "water flow", shri "rain".

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text: A stream is a flowing body of water with a current, confined within a bed and stream banks. In the United States, a stream is classified as a watercourse less than  wide. Streams are important as conduits in the water cycle, instruments in groundwater recharge, and they serve as corridors for fish and wildlife migration. The biological habitat in the immediate vicinity of a stream is called a riparian zone. Given the status of the ongoing Holocene extinction, streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity. The study of streams and waterways in general involves many branches of inter-disciplinary natural science and engineering, including hydrology, fluvial geomorphology, aquatic ecology, fish biology, riparian ecology, and others.

text: A stream is a flowing body of water with a

text: current

text: , confined within a

text: bed

text: and

text: stream bank

text: s. In the United States, a stream is classified as a watercourse less than  wide. Streams are important as conduits in the

text: water cycle

text: , instruments in

text: groundwater recharge

text: , and they serve as corridors for fish and

text: wildlife

text: migration. The biological

text: habitat

text: in the immediate vicinity of a stream is called a

text: riparian zone

text: . Given the status of the ongoing

text: Holocene extinction

text: , streams play an important

text: corridor

text: role in connecting

text: fragmented habitats

text: and thus in conserving

text: biodiversity

text: . The study of streams and waterways in general involves many branches of inter-disciplinary natural science and engineering, including

text: hydrology

text: fluvial geomorphology

text: aquatic ecology

text: fish biology

text: riparian ecology

text: , and others.

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text: The municipality is divided between the basins of the Panuco and Moctezuma Rivers. The area is filled with small rivers, streams and arroyos, which almost always run north-south. The largest of the rivers are the Huascazaloya, Iztla, Hueypan and San Jeronimo. These rivers and streams feed 87 natural and dammed bodies of water, which vary in size from a few meters wide a couple of kilometers. The best known dam in the areas is the San Antonio Regla dam. Water from this dam is used primarily for agricultural irrigation. The major fresh water spring is called Ojo de Agua, which is surrounded by large willow and other trees.

text: The municipality is divided between the basins of the

text: Panuco

text: and

text: Moctezuma

text: Rivers. The area is filled with small rivers, streams and arroyos, which almost always run north-south. The largest of the rivers are the Huascazaloya, Iztla, Hueypan and San Jeronimo. These rivers and streams feed 87 natural and dammed bodies of water, which vary in size from a few meters wide a couple of kilometers. The best known dam in the areas is the San Antonio Regla dam. Water from this dam is used primarily for agricultural irrigation. The major fresh water spring is called Ojo de Agua, which is surrounded by large willow and other trees.

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text: Manimahesh Kailash or Mountain Kailash is in the watershed of the Budhil valley, which forms part the mid-Himalayan range of hills near Kugti pass and at Harsar. The perpetually snow-covered glacial peak, at the head of its own range, is the source of the sacred lake of Manimahesh situated beneath it. Manimahesh Ganga River originates in a cascade from the lake and joins the Budhil River on its left bank. This hill range is a contiguous spur that conjoins the main range near the Bara Banghal pass of the Pir Panjal range. After the Budhal River rises from the slopes of the Kukti (Kugati) pass and Bada Bangal pass, the watershed formed by the Budhil and Ravi rivers takes the form of an inverted triangle with its base at Khadamukh. Budhil itself is formed by several streams which rise from different faces of the Manimahesh Kailas peak. The streams which rise from the peak are: the 'Bhujla' (derived from Bhuja meaning the arm) from the left flank of the peak, which meets Bhudil (also spelt Budhal) below Kukti village; the Dhancho nala, rising from the snowy ranges of the southern flank of the peak, flows in northward direction; Androl stream carrying holy waters of the Manimahesh Lake flowing to the north of the peak and through the Barachundi Meadow, the Siv Karotar stream rises from the foot of the peak and joins Androl; and the Gauri stream from the Gauri Kund joins Androl. All these streams constitute the Dhancho nala that confluences with Budhil at Hadsar. In view of so many streams originating from the Manimhesah Peak and the Manimhaesh Lake, and all of which are also linked to legends and the annual yatra pilgrimage, the Budhal or Budhil River is also highly venerated by the Gaddi elders and is nicknamed as 'Bhujl'. Pir Pinjal lies in the lesser Himalayan Zone, which forms the central part of the state of Himachal Pradesh. The peak lies along the water shed between the Chenab River on the one side and Ravi and Beas on the other side.

text: Manimahesh Kailash or Mountain Kailash is in the watershed of the Budhil valley, which forms part the mid-Himalayan range of hills near Kugti pass and at Harsar. The perpetually snow-covered glacial peak, at the head of its own range, is the source of the sacred lake of Manimahesh situated beneath it. Manimahesh Ganga River originates in a cascade from the lake and joins the Budhil River on its left bank. This hill range is a contiguous spur that conjoins the main range near the Bara Banghal pass of the

text: Pir Panjal

text: Chenab River

text: on the one side and

text: Ravi

text: and

text: Beas

text: on the other side.

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answers: NDQ_006066

answers: Budhil itself is formed

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answers: Manimahesh Ganga River

answers: NDQ_006068

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answers: NDQ_006069

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text: The ISO base media file format supports streaming of media data over a network as well as local playback. A file that supports streaming includes information about the data units to stream (how to serve the elementary stream data in the file over streaming protocols). This information is placed in additional tracks of the file called "hint" tracks. Separate "hint" tracks for different protocols may be included within the same file. The media will play over all such protocols without making any additional copies or versions of the media data. Existing media can be easily made streamable for other specific protocols by the addition of appropriate hint tracks. The media data itself need not be reformatted in any way. The streams sent by the servers under the direction of the hint tracks, need contain no trace of file-specific information. When the presentation is played back locally (not streamed), the hint tracks may be ignored. Hint tracks may be created by an authoring tool, or may be added to an existing file (presentation) by a hinting tool. In media authored for progressive download  the moov box, which contains the index of frames should precede the movie data mdat box.

text: The ISO base media file format supports

text: streaming

text: of media data over a network as well as local playback. A file that supports streaming includes information about the data units to stream (how to serve the

text: elementary stream

text: data in the file over streaming protocols). This information is placed in additional tracks of the file called "hint" tracks. Separate "hint" tracks for different protocols may be included within the same file. The media will play over all such protocols without making any additional copies or versions of the media data. Existing media can be easily made streamable for other specific protocols by the addition of appropriate hint tracks. The media data itself need not be reformatted in any way. The streams sent by the servers under the direction of the hint tracks, need contain no trace of file-specific information. When the presentation is played back locally (not streamed), the hint tracks may be ignored. Hint tracks may be created by an authoring tool, or may be added to an existing file (presentation) by a hinting tool. In media authored for progressive download  the moov box, which contains the index of frames should precede the movie data mdat box.

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answers: The ISO base media file format supports streaming

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answers: The ISO base media file format supports streaming of media data over a network as well as local playback

answers: NDQ_006067

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answers: NDQ_006068

answers: It can be easily made streamable for other specific protocols by the addition of appropriate hint tracks

answers: NDQ_006069

answers: When the presentation is played back locally (not streamed), the hint tracks may be ignored

text: In hydrology, a rating curve is a graph of discharge versus stage for a given point on a stream, usually at gauging stations, where the stream discharge is measured across the stream channel with a flow meter. Numerous measurements of stream discharge are made over a range of stream stages. The rating curve is usually plotted as discharge on x-axis versus stage (surface elevation) on y-axis.

text: In

text: hydrology

text: , a rating curve is a graph of

text: discharge

text: versus

text: stage

text: for a given point on a stream, usually at gauging stations, where the stream discharge is measured across the stream channel with a

text: flow meter

text: . Numerous measurements of stream discharge are made over a range of stream stages. The rating curve is usually plotted as discharge on x-axis versus stage (surface elevation) on y-axis.

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answers: gauging stations

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answers: No

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answers: It does not say.

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answers: rating curve

text: SR 26 begins as a four-lane divided highway at a diamond interchange with US 460 and SR 24 (Richmond Highway) just north of the town of Appomattox.  The roadway continues south of the expressway bypass of the town as US 460 Business (Confederate Boulevard), which leads to the Appomattox Historic District.  SR 26 reduces to two lanes and heads north as Oakville Road through northwestern Appomattox County.  The state highway passes through the hamlet of Oakville.  Near the northern end of SR 26, the highway descends into the narrow valley of Bent Creek.  The state highway crosses the stream just south of the stream's mouth at the James River.  A short distance to the north, SR 26 reaches its terminus at US 60 (James Anderson Highway) in the hamlet of Bent Creek just south of the U.S. Highway's crossing of the James River.

text: SR 26 begins as a four-lane divided highway at a

text: diamond interchange

text: with US 460 and SR 24 (Richmond Highway) just north of the town of Appomattox.  The roadway continues south of the expressway bypass of the town as US 460 Business (Confederate Boulevard), which leads to the

text: Appomattox Historic District

text: .  SR 26 reduces to two lanes and heads north as Oakville Road through northwestern Appomattox County.  The state highway passes through the hamlet of

text: Oakville

text: .  Near the northern end of SR 26, the highway descends into the narrow valley of

text: Bent Creek

text: .  The state highway crosses the stream just south of the stream's mouth at the James River.  A short distance to the north, SR 26 reaches its terminus at US 60 (James Anderson Highway) in the hamlet of Bent Creek just south of the U.S. Highway's crossing of the James River.

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answers: Bent Creek

text: Northkill Creek is a stream primarily located in Berks County, Pennsylvania.  It feeds into Tulpehocken Creek and covers part of the Schuylkill River and Delaware River watersheds.  Northkill Creek and its tributaries are high quality trout streams.

text: Northkill Creek is a stream primarily located in

text: Berks County, Pennsylvania

text: .  It feeds into

text: Tulpehocken Creek

text: and covers part of the

text: Schuylkill River

text: and

text: Delaware River

text: watersheds.  Northkill Creek and its tributaries are high quality trout streams.

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answers: NDQ_006067

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answers: NDQ_006068

answers: river watersheds

answers: NDQ_006069

answers: Northkill Creek

text: Flat Creek is a stream in the U.S. state of Missouri. It is a tributary of the Little Black River.

text: Flat Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the Little Black River.

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text: Another kind of exception occurs when a stream falling onto the Divide splits and flows in both directions, or a lake straddling the divide overflows in both directions. Examples of these are, respectively, North Two Ocean Creek and Isa Lake, both located on the Continental Divide in Wyoming. The Panama Canal has this same feature, being man-made.  Both the Chagres and Gatun rivers flow into Gatun Lake, which empties to both oceans.

text: Another kind of exception occurs when a stream falling onto the Divide splits and flows in both directions, or a lake straddling the divide overflows in both directions. Examples of these are, respectively,

text: North Two Ocean Creek

text: and

text: Isa Lake

text: , both located on the Continental Divide in Wyoming. The

text: Panama Canal

text: has this same feature, being man-made.  Both the

text: Chagres

text: and Gatun rivers flow into

text: Gatun Lake

text: , which empties to both oceans.

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answers: The Panama Canal has this same feature, being man-made

text: The city sits along the Eastern Continental Divide. Streams to the west of the city center travel to the Chattahoochee River and ultimately the Gulf of Mexico, while streams to the east flow to the Yellow River, a tributary of the Ocmulgee River, which flows to the Atlantic Ocean north of Brunswick. This divide, or ridge, played a significant role in the early settlement of the area. Originally, the Creek and Cherokee people occupied this land, and the ridgeline was used as a major transportation route. Two American forts were established in the early 19th century due to the War of 1812: Fort Daniel (at Hog Mountain) and Peachtree Fort (in Atlanta). These two forts were connected by this old Indian trail which became known as the original Peachtree Road. By around 1840, this trail had evolved into a stagecoach route connecting South Carolina and Alabama through Georgia. The surrounding area became populated, and the small communities of Pinckneyville and Flint Hill prospered.

text: The city sits along the

text: Eastern Continental Divide

text: . Streams to the west of the city center travel to the

text: Chattahoochee River

text: and ultimately the

text: Gulf of Mexico

text: , while streams to the east flow to the

text: Yellow River

text: , a tributary of the

text: Ocmulgee River

text: , which flows to the

text: Atlantic Ocean

text: north of

text: Brunswick

text: . This divide, or ridge, played a significant role in the early settlement of the area. Originally, the

text: Creek

text: and

text: Cherokee

text: people occupied this land, and the ridgeline was used as a major transportation route. Two American forts were established in the early 19th century due to the

text: War of 1812

text: : Fort Daniel (at Hog Mountain) and Peachtree Fort (in Atlanta). These two forts were connected by this old Indian trail which became known as the original Peachtree Road. By around 1840, this trail had evolved into a stagecoach route connecting

text: South Carolina

text: and

text: Alabama

text: through Georgia. The surrounding area became populated, and the small communities of Pinckneyville and Flint Hill prospered.

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answers: The surrounding area became populated

text: River Churni is a stream in the Nadia district of the Indian state of West Bengal. It is a distributary of the Mathabhanga River, itself a distributary of the Padma River at Munshiganj in the Kushtia District ofBangladesh. The Mathabanga divides into two rivers, the Ichamati and the Churni near Majhdia in Nadia district.

text: River Churni is a stream in the

text: Nadia district

text: of the

text: Indian state

text: of

text: West Bengal

text: . It is a

text: distributary

text: of the

text: Mathabhanga River

text: , itself a distributary of the

text: Padma River

text: at Munshiganj in the

text: Kushtia District

text: ofBangladesh. The Mathabanga divides into two rivers, the

text: Ichamati

text: and the Churni near

text: Majhdia

text: in Nadia district.

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answers: No

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answers: River Churni

answers: NDQ_006063

answers: Indian

answers: NDQ_006064

answers: Nadia district

answers: NDQ_006065

answers: erodes

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answers: Pacific Ocean

answers: NDQ_006067

answers: The Mathabanga River

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: River Churni

text: Deer Creek is a stream in the U.S. state of Missouri. It is a tributary of the South Grand River.

text: Deer Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the South Grand River.

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answers: Deer Creek is a stream

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answers: Deer Creek

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answers: Deer Creek

text: This is a list of rivers of Antarctica. Although they are variously named river, creek or stream, those listed are technically all meltwater streams.

text: This is a list of rivers of

text: Antarctica

text: . Although they are variously named

text: river

text: , creek or

text: stream

text: , those listed are technically all meltwater streams.

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answers: rivers of Antarctica

answers: NDQ_006069

answers: rivers of Antarctica

text: The first part (the main stream) is a 10-round Feistel network, using four 8×8-bit S-boxes much like the ones from CIPHERUNICORN-E. The last two rounds of the main stream are influenced by the output of the second part (the temporary key generation function). This second, 6-round Feistel network uses modular multiplication, as well as two of the S-boxes.

text: The first part (the main stream) is a 10-round Feistel network, using four 8×8-bit

text: S-boxes

text: much like the ones from CIPHERUNICORN-E. The last two rounds of the main stream are influenced by the output of the second part (the temporary key generation function). This second, 6-round Feistel network uses

text: modular multiplication

text: , as well as two of the S-boxes.

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answers: influenced

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answers: NDQ_006067

answers: CIPHERUNICORN

answers: NDQ_006068

answers: Feistel network

answers: NDQ_006069

answers: Feistel network

text: A tributary or affluent is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean.

text: A tributary or affluent is a

text: stream

text: or

text: river

text: that flows into a larger stream or

text: main stem

text: (or parent) river or a

text: lake

text: . A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding

text: drainage basin

text: of its surface water and

text: groundwater

text: , leading the water out into an ocean.

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answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: drainage basin

answers: NDQ_006063

answers: groundwater

answers: NDQ_006064

answers: drainage basin

answers: NDQ_006065

answers: drain the surrounding drainage basin

answers: NDQ_006066

answers: ocean

answers: NDQ_006067

answers: Sea or ocean

answers: NDQ_006068

answers: surface water and groundwater

answers: NDQ_006069

answers: A tributary

text: A drainage divide, water divide, divide, ridgeline, watershed, water parting, or (in Canada) height of land, is the line that separates neighbouring drainage basins.  In hilly country, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. In flat country—especially where the ground is marshy—the divide may be harder to discern.

text: A drainage divide, water divide, divide, ridgeline, watershed, water parting, or (in

text: Canada

text: ) height of land, is the line that separates neighbouring

text: drainage basin

text: s.  In

text: hill

text: y country, the divide lies along

text: topographical

text: ridge

text: s, and may be in the form of a single range of hills or

text: mountain

text: s, known as a dividing range. In flat country—especially where the ground is

text: marsh

text: y—the divide may be harder to discern.

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answers: drainage divide

answers: NDQ_006061

answers: In hilly country

answers: NDQ_006062

answers: drainage divide

answers: NDQ_006063

answers: ground

answers: NDQ_006064

answers: drainage basin

answers: NDQ_006065

answers: hard to discern

answers: NDQ_006066

answers: the divide lies along topographical ridges

answers: NDQ_006067

answers: marshy

answers: NDQ_006068

answers: drainage

answers: NDQ_006069

answers: hilly country

text: North of the Lunda Divide the Kwango and many other streams flow north from the tableland to join the Kasai River (one of the largest affluents of the Congo), which in its upper course forms for fully  the boundary between Angola and the Congo. South of the divide some rivers flow into the Zambezi River system and thence to the Indian Ocean, others to the Okavango River (as the Cubango River is called along the border with Namibia and in Botswana) and thence to Lake Ngami and the Okavango Swamp in Botswana. The tributaries of the Cubango River and several of the southern rivers flowing to the Atlantic are seasonal, completely dry much of the year.

text: North of the Lunda Divide the

text: Kwango

text: and many other streams flow north from the tableland to join the

text: Kasai River

text: (one of the largest affluents of the Congo), which in its upper course forms for fully  the boundary between Angola and the Congo. South of the divide some rivers flow into the Zambezi River system and thence to the Indian Ocean, others to the Okavango River (as the Cubango River is called along the border with Namibia and in Botswana) and thence to

text: Lake Ngami

text: and the Okavango Swamp in Botswana. The tributaries of the Cubango River and several of the southern rivers flowing to the Atlantic are seasonal, completely dry much of the year.

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answers: Lunda Divide

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Lunda Divide

answers: NDQ_006063

answers: the tableland

answers: NDQ_006064

answers: Lunda Divide

answers: NDQ_006065

answers: seasonal

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Atlantic

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: the Okavango River

text: Multiple stages in series can be applied to achieve higher purity permeate streams. Due to the modular nature of membrane processes, multiple modules can be arranged in parallel to treat greater volumes.

text: Multiple stages in series can be applied to achieve higher purity permeate streams. Due to the modular nature of membrane processes, multiple modules can be arranged in parallel to treat greater volumes.

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answers: permeate streams

answers: NDQ_006063

answers: permeate

answers: NDQ_006064

answers: streams

answers: NDQ_006065

answers: greater volumes

answers: NDQ_006066

answers: The continental divide

answers: NDQ_006067

answers: permeate streams

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: modular nature of membrane processes

text: The Divide crosses into the United States in northwestern Montana, at the boundary between Waterton Lakes National Park and Glacier National Park. In Canada, it forms the western boundary of Waterton Lakes National Park, and in the US bisects Glacier National Park.  Further south, the Divide forms the backbone of the Rocky Mountain Front (Front Range) in the Bob Marshall Wilderness, heads south towards Helena and Butte, then west past the namesake community of Divide, Montana through the Anaconda-Pintler Wilderness to the Bitterroot Range, where it forms the eastern third of the state boundary between Idaho and Montana.  The Divide crosses into Wyoming within Yellowstone National Park and continues southeast into Colorado where it reaches its highest point in North America at the summit of  Grays Peak at   .  It crosses US Hwy 160 in southern Colorado at Wolf Creek Pass, where a line symbolizes the division.  The Divide then proceeds south into western New Mexico, passing along the western boundary of the endorheic Plains of San Agustin.  Although the Divide represents the height of land between watersheds, it does not always follow the highest ranges/peaks within each state or province.

text: The Divide crosses into the

text: United States

text: in northwestern

text: Montana

text: , at the boundary between

text: Waterton Lakes National Park

text: and

text: Glacier National Park

text: . In Canada, it forms the western boundary of Waterton Lakes National Park, and in the US bisects Glacier National Park.  Further south, the Divide forms the backbone of the

text: Rocky Mountain Front

text: (Front Range) in the

text: Bob Marshall Wilderness

text: , heads south towards

text: Helena

text: and

text: Butte

text: , then west past the namesake community of

text: Divide, Montana

text: through the Anaconda-Pintler Wilderness to the

text: Bitterroot Range

text: , where it forms the eastern third of the state boundary between

text: Idaho

text: and Montana.  The Divide crosses into

text: Wyoming

text: within

text: Yellowstone National Park

text: and continues southeast into

text: Colorado

text: where it reaches its highest point in North America at the summit of

text: Grays Peak

text: at   .  It crosses US Hwy 160 in southern Colorado at

text: Wolf Creek Pass

text: , where a line symbolizes the division.  The Divide then proceeds south into western

text: New Mexico

text: , passing along the western boundary of the endorheic Plains of San Agustin.  Although the Divide represents the height of land between watersheds, it does not always follow the highest ranges/peaks within each state or province.

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text: Beyond the lake, the Torne River flows unhindered by any concentrations of human inhabitants until the village of Kurravaara, around  northeast of Kiruna.The river splits in two parts that only join at Kurravaara, the part between the river is Alajávri nature reserve (Alajávri naturreservat).Between the lake and Kurravaara, the streams Čearrojogaš and Rávdojohka join on the right side, and shortly befare Kurravaara, the  long Rautas Riverflows into the Torne.On the left side, the streams Gukkajohka, Reaskkajohka and Dápmokjohka join.In the area between the two streams, the Beallejohka joins the right arm from the left.

text: Beyond the lake, the Torne River flows unhindered by any concentrations of human inhabitants until the village of

text: Kurravaara

text: , around  northeast of

text: Kiruna

text: .The river splits in two parts that only join at Kurravaara, the part between the river is

text: Alajávri nature reserve

text: (Alajávri naturreservat).Between the lake and Kurravaara, the streams

text: Čearrojogaš

text: and

text: Rávdojohka

text: join on the right side, and shortly befare Kurravaara, the  long

text: Rautas River

text: flows into the Torne.On the left side, the streams

text: Gukkajohka

text: Reaskkajohka

text: and

text: Dápmokjohka

text: join.In the area between the two streams, the

text: Beallejohka

text: joins the right arm from the left.

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text: The sources of several rivers are located in the Smokies, including the Little Pigeon River, the Oconaluftee River, and Little River.  Streams in the Smokies are part of the Tennessee River watershed and are thus entirely west of the Eastern Continental Divide.  The largest stream wholly within the park is Abrams Creek, which rises in Cades Cove and empties into the Chilhowee Lake impoundment of the Little Tennessee River near Chilhowee Dam.

text: The sources of several rivers are located in the Smokies, including the

text: Little Pigeon River

text: , the

text: Oconaluftee River

text: , and

text: Little River

text: .  Streams in the Smokies are part of the

text: Tennessee River

text: watershed and are thus entirely west of the

text: Eastern Continental Divide

text: .  The largest stream wholly within the park is

text: Abrams Creek

text: , which rises in Cades Cove and empties into the Chilhowee Lake impoundment of the Little Tennessee River near

text: Chilhowee Dam

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text: Stratford is on the banks of the Patea River, at the junction of the Patea River and Paetahi Stream, approximately 15 km east of the headwaters. Due to the narrow width of the catchment, the southern boundary of the town is on the Patea/Waingongoro divide, while 4 km to the north Midhirst is on the Patea/Manganui divide.

text: Stratford is on the banks of the

text: Patea River

text: , at the junction of the Patea River and

text: Paetahi Stream

text: , approximately 15 km east of the headwaters. Due to the narrow width of the catchment, the southern boundary of the town is on the Patea/Waingongoro

text: divide

text: , while 4 km to the north

text: Midhirst

text: is on the Patea/Manganui divide.

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answers: NDQ_006060

answers: Paetahi Stream

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Patea River

answers: NDQ_006063

answers: Patea

answers: NDQ_006064

answers: headwaters

answers: NDQ_006065

answers: narrow width

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Patea River

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Patea River

text: This is a list of streams and rivers in Eritrea, arranged geographically by drainage basin.  Generally, rivers in Eritrea are divided into three groups: those that drain into Sudan, towards the Red Sea and towards the Afar Depression.  There is an alphabetic list at the end of this article.

text: This is a list of

text: streams

text: and

text: rivers

text: in

text: Eritrea

text: , arranged geographically by drainage basin.  Generally, rivers in Eritrea are divided into three groups: those that drain into

text: Sudan

text: , towards the

text: Red Sea

text: and towards the

text: Afar Depression

text: .  There is an alphabetic list at the end of this article.

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answers: NDQ_006064

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answers: NDQ_006066

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answers: NDQ_006067

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answers: NDQ_006068

answers: drainage basin

answers: NDQ_006069

answers: rivers in Eritrea

text: Water is an essential part to the ecosystem of forests including the plants and animal species survival, stream, rivers and lakes habitats and also human activities. The act of deforestation can affect the quality of water, quantity of water as well as the aquatic ecosystems located in the forests. When deforestation takes place by the forest sector, the water quality can be affected by sedimentation, pollution and changes in water levels. When roads are put in to cross streams and rivers, 94% of the roads crossings have low to moderate potential to deliver sediment to a stream, When the deforestation takes place near a stream, riparian techniques are used to conserve the tree density around the stream to protect and provide many benefits to the water quality, quantity and stability of the aquatic ecosystem. With 87% of the riparian area within the deforested area being in properly functioning conditions, the forest sector has high conservation efforts to protect the water within forest. The passage of fish species to upstream and downstream habitats can be an essential part of survival and can be affected by deforestation practices, especially the building of roads by forest sector. With only 42% of the road stream crossings having a low effect on the passage of fish species, the remainder of crossings have a high to moderate risk of limiting fish passage. With an increase in stream crossings by roads from 421,830 in 2000 to 488,674 in 2005, a strategic plan is in process to address the fish passage concern.

text: Water is an essential part to the ecosystem of forests including the plants and animal species survival, stream, rivers and lakes habitats and also human activities. The act of deforestation can affect the quality of water, quantity of water as well as the aquatic ecosystems located in the forests. When deforestation takes place by the forest sector, the water quality can be affected by

text: sedimentation

text: , pollution and changes in water levels. When roads are put in to cross streams and rivers, 94% of the roads crossings have low to moderate potential to deliver sediment to a stream, When the deforestation takes place near a stream,

text: riparian

text: techniques are used to conserve the tree density around the stream to protect and provide many benefits to the water quality, quantity and stability of the aquatic ecosystem. With 87% of the riparian area within the deforested area being in properly functioning conditions, the forest sector has high conservation efforts to protect the water within forest. The passage of fish species to upstream and downstream habitats can be an essential part of survival and can be affected by deforestation practices, especially the building of roads by forest sector. With only 42% of the road stream crossings having a low effect on the passage of fish species, the remainder of crossings have a high to moderate risk of limiting fish passage. With an increase in stream crossings by roads from 421,830 in 2000 to 488,674 in 2005, a strategic plan is in process to address the fish passage concern.

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answers: low to moderate

answers: NDQ_006066

answers: west side of the continental divide

answers: NDQ_006067

answers: fish

answers: NDQ_006068

answers: rivers and lakes

answers: NDQ_006069

answers: deforestation practices, especially the building of roads by forest sector

text: A post office called Divide has been in operation since 1889. The community was named for a drainage divide near the original town site.

text: A post office called Divide has been in operation since 1889. The community was named for a

text: drainage divide

text: near the original town site.

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answers: NDQ_006063

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answers: NDQ_006064

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answers: NDQ_006065

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answers: NDQ_006066

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answers: NDQ_006067

answers: no

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answers: drainage divide

answers: NDQ_006069

answers: drainage divide

text: The Sint-Jansbeek is a stream in Arnhem, which streams down from the hills of Zijpendaal through the Sonsbeek park and the inner city of Arnhem to the river Rhine. The Sint-Jansbeek has always been an open stream, but the part in the inner city is covered since the city moats were filled in the 19th century. The stream from the source in Zijpendaal through the park Sonsbeek is still open.

text: The Sint-Jansbeek is a

text: stream

text: in

text: Arnhem

text: , which streams down from the hills of

text: Zijpendaal

text: through the

text: Sonsbeek

text: park and the inner city of Arnhem to the river

text: Rhine

text: . The Sint-Jansbeek has always been an open stream, but the part in the inner city is covered since the city

text: moat

text: s were filled in the 19th century. The stream from the source in Zijpendaal through the park Sonsbeek is still open.

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answers: The Sint-Jansbeek

text: Since for every odd prime p, p divides a if and only if p is congruent to 1 mod 4, and since p divides the denominator of (p - 1)th Bernoulli number for every odd prime p, so for any odd prime p, p cannot divide a. Besides, if and only if an odd prime p divides a (and 2p does not divide n), then p also divides a (if 2p divides n, then the sentence should be changed to "p also divides a". In fact, if 2p divides n and p(p - 1) does not divide n, then p divides a.) for every integer k (a condition is n + k(p - 1) must be > 1). For example, since 19 divides a and 2 × 19 = 38 does not divide 11, so 19 divides a for all k. Thus, the definition of irregular pair (p, n), n should be at most p - 2.

text: Since for every odd prime p, p divides a if and only if p is congruent to 1 mod 4, and since p divides the denominator of (p - 1)th Bernoulli number for every odd prime p, so for any odd prime p, p cannot divide a. Besides, if and only if an odd prime p divides a (and 2p does not divide n), then p also divides a (if 2p divides n, then the sentence should be changed to "p also divides a". In fact, if 2p divides n and p(p - 1) does not divide n, then p divides a.) for every integer k (a condition is n + k(p - 1) must be > 1). For example, since 19 divides a and 2 × 19 = 38 does not divide 11, so 19 divides a for all k. Thus, the definition of irregular pair (p, n), n should be at most p - 2.

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answers: (p, n)

answers: NDQ_006061

answers: If 2p divides n and p(p - 1) does not divide n, then p divides a

answers: NDQ_006062

answers: pacific ocean

answers: NDQ_006063

answers: 1 mod 4

answers: NDQ_006064

answers: a location where a stream forms

answers: NDQ_006065

answers: if and only if an odd prime p divides a

answers: NDQ_006066

answers: For every odd prime p, p divides the denominator of (p - 1)th Bernoulli number for every odd prime p, so for any odd prime p, p cannot divide a.

answers: NDQ_006067

answers: No organisms can live where a fresh water stream flows into the salty ocean.

answers: NDQ_006068

answers: inland cities were often built on rivers because they provided water

answers: NDQ_006069

answers: For every odd prime p, p divides a if and only if p is congruent to 1 mod 4, and since p divides the denominator of (p - 1)th Bernoulli number for every odd prime p, so for any odd prime p, p cannot divide a.

text: The Kabbalistic form of Jewish mysticism itself divides into three general streams: the Theosophical/Speculative Kabbalah (seeking to understand and describe the divine realm), the Meditative/Ecstatic Kabbalah (seeking to achieve a mystical union with God), and the Practical/Magical Kabbalah (seeking to theurgically alter the divine realms and the World). These three different, but inter-relating, methods or aims of mystical involvement are also found throughout the other pre-Kabbalistic and post-Kabbalistic stages in Jewish mystical development, as three general typologies. As in Kabbalah, the same text can contain aspects of all three approaches, though the three streams often distill into three separate literatures under the influence of particular exponents or eras.

text: The Kabbalistic form of Jewish mysticism itself divides into three general streams: the

text: Theosophical/Speculative Kabbalah

text: (seeking to understand and describe the divine realm), the

text: Meditative/Ecstatic Kabbalah

text: (seeking to achieve a mystical union with God), and the

text: Practical/Magical Kabbalah

text: (seeking to

text: theurgically

text: alter the divine realms and the World). These three different, but inter-relating, methods or aims of mystical involvement are also found throughout the other pre-Kabbalistic and post-Kabbalistic stages in Jewish mystical development, as three general typologies. As in Kabbalah, the same text can contain aspects of all three approaches, though the three streams often distill into three separate literatures under the influence of particular exponents or eras.

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answers: the same text can contain aspects of all three approaches

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answers: no

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answers: Theosophical

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answers: streams

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answers: often distill

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Theosophical/Speculative Kabbalah

text: parallel streams, each of which is converted to a binary stream using an appropriate symbol detector. These streams are then re-combined into a serial stream,

text: parallel streams, each of which is converted to a binary stream using an appropriate symbol

text: detector

text: . These streams are then re-combined into a serial stream,

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answers: no

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answers: NDQ_006063

answers: binary

answers: NDQ_006064

answers: parallel streams

answers: NDQ_006065

answers: a stream

answers: NDQ_006066

answers: serial stream

answers: NDQ_006067

answers: parallel streams

answers: NDQ_006068

answers: parallel streams

answers: NDQ_006069

answers: binary stream

text: There are over 500 lakes in the forest, and  of streams and rivers. The Clarks Fork of the Yellowstone River is federally designated as a Wild and Scenic River for  through the forest, with cliffs towering up to  as the river winds through a gorge. The forest is on the eastern slopes of the Continental Divide, and the rivers flow into the Atlantic Ocean basin.

text: There are over 500 lakes in the forest, and  of streams and rivers. The Clarks Fork of the Yellowstone River is federally designated as a

text: Wild and Scenic River

text: for  through the forest, with cliffs towering up to  as the river winds through a gorge. The forest is on the eastern slopes of the Continental Divide, and the rivers flow into the

text: Atlantic Ocean basin

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answers: streams and rivers

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answers: the Atlantic Ocean basin

text: The river's has five major tributaries, the Dalang Stream (), Minzhi Stream (), Zhangkengjing Stream (), Niuhu Stream (), and Baihua Stream ().

text: The river's has five major tributaries, the Dalang Stream (), Minzhi Stream (), Zhangkengjing Stream (), Niuhu Stream (), and Baihua Stream ().

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answers: Dalang Stream

text: The drainage of the state is wholly into the Mississippi River, directly or indirectly, and to a large extent into either that river or the Missouri River  within the borders of the state. The latter stream, crossing the state and cutting the eastern and western borders at or near St Louis and Kansas City respectively, has a length within Missouri of . The areas drained into the Mississippi outside the state through the St. Francis, White and other minor streams are relatively small. The larger streams of the Ozark dome are of decided interest to the physiographer. Those of the White system have opentrough valleys bordered by hills in their upper courses and canyons in their lower courses.

text: The drainage of the state is wholly into the

text: Mississippi River

text: , directly or indirectly, and to a large extent into either that river or the

text: Missouri River

text: within the borders of the state. The latter stream, crossing the state and cutting the eastern and western borders at or near St Louis and Kansas City respectively, has a length within Missouri of . The areas drained into the Mississippi outside the state through the

text: St. Francis

text: White

text: and other minor streams are relatively small. The larger streams of the

text: Ozark

text: dome are of decided interest to the physiographer. Those of the White system have opentrough valleys bordered by hills in their upper courses and canyons in their lower courses.

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answers: NDQ_006064

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answers: NDQ_006065

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answers: NDQ_006067

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answers: NDQ_006068

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answers: NDQ_006069

answers: drainage of the state

text: Bokes Creek is a stream in the U.S. state of Ohio. It is a tributary of the Scioto River.

text: Bokes Creek is a stream in the

text: U.S. state

text: of

text: Ohio

text: . It is a

text: tributary

text: of the

text: Scioto River

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answers: NDQ_006063

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answers: NDQ_006067

answers: Bokes Creek

answers: NDQ_006068

answers: Bokes Creek

answers: NDQ_006069

answers: Scioto River

text: Rapid Run is a stream located entirely within Hamilton County, Ohio. The  long stream is a tributary of the Ohio River.

text: Rapid Run is a

text: stream

text: located entirely within

text: Hamilton County, Ohio

text: . The  long stream is a tributary of the

text: Ohio River

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answers: NDQ_006068

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text: The Garte is a 23 km long stream that rises to the east of Weißenborn at an elevation of 303 m amsl. Towns that it runs through or by include Beienrode, Kerstlingerode, Rittmarshausen (where it is joined by the Bernsroder Bach), Wöllmarshausen, Benniehausen (where the Bischhäuser Bach joins it),  Klein Lengden (where the Bramke and Eichbach join it), and Diemarden.  The stream joins the Leine River south of Göttingen. With a drop of 151 m, the stream averages a bed slope of 6.6‰.  The watershed is 87 km².  It is classified as a third-order (i.e., lowest) stream according to the German system of body-of-water ranking.

text: The Garte is a 23 km long stream that rises to the east of Weißenborn at an elevation of 303 m amsl. Towns that it runs through or by include

text: Beienrode

text: Kerstlingerode

text: Rittmarshausen

text: (where it is joined by the Bernsroder Bach), Wöllmarshausen,

text: Benniehausen

text: (where the Bischhäuser Bach joins it),

text: Klein Lengden

text: (where the Bramke and Eichbach join it), and

text: Diemarden

text: .  The stream joins the Leine River south of

text: Göttingen

text: . With a drop of 151 m, the stream averages a bed slope of 6.6‰.  The watershed is 87 km².  It is classified as a third-order (i.e., lowest) stream according to the German system of body-of-water ranking.

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answers: NDQ_006063

answers: 303 m amsl

answers: NDQ_006064

answers: elevation

answers: NDQ_006065

answers: 6.6

answers: NDQ_006066

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answers: NDQ_006067

answers: The Garte

answers: NDQ_006068

answers: Towns that it runs through

answers: NDQ_006069

answers: The Garte

text: Divide is a census-designated place and a U.S. Post Office in Teller County, Colorado, United States.  The population as of the 2010 Census was 127.Divide sits on the north slope of Pikes Peak on U.S. Highway 24.  Ute Pass is immediately west of town.  The Divide Post Office has the ZIP Code 80814.

text: Divide is a

text: census-designated place

text: and a

text: U.S. Post Office

text: in

text: Teller County

text: Colorado

text: United States

text: .  The population as of the

text: 2010 Census

text: was 127.Divide sits on the north slope of

text: Pikes Peak

text: on

text: U.S. Highway 24

text: Ute Pass

text: is immediately west of town.  The Divide Post Office has the

text: ZIP Code

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answers: Divide

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Divide is a census-designated place

answers: NDQ_006063

answers: North slope

answers: NDQ_006064

answers: Pass

answers: NDQ_006065

answers: slope

answers: NDQ_006066

answers: Ute Pass is immediately west of town.

answers: NDQ_006067

answers: Ute Pass

answers: NDQ_006068

answers: Pikes Peak

answers: NDQ_006069

answers: Pikes Peak

text: Ingiriya starts  from the sea side of the country to  to the inner side of the country.Basically, the area is full of mountains and the east border contains more mountain characteristics. The highest land in the area is Madakada Giranchi Mountain, which is  high. The Eduragala Mountain is also over  in height. The eastern part contains some higher mountains over  here and there and also in western part there are similar mountains. Overall 60% of the area is  flat plains.The Kalu river flows along the southern border of Ingiriya and many streams flow into the Kalu River. From the eastern part it flows Nambapana stream and the largest stream of the area, Mawak Oya starts from North and flows along west side and connects to the Kalu River in the South.

text: Ingiriya starts  from the sea side of the country to  to the inner side of the country.Basically, the area is full of mountains and the east border contains more mountain characteristics. The highest land in the area is Madakada Giranchi Mountain, which is  high. The Eduragala Mountain is also over  in height. The eastern part contains some higher mountains over  here and there and also in western part there are similar mountains. Overall 60% of the area is  flat plains.The Kalu river flows along the southern border of Ingiriya and many streams flow into the Kalu River. From the eastern part it flows Nambapana stream and the largest stream of the area, Mawak Oya starts from North and flows along west side and connects to the Kalu River in the South.

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answers: the Kalu River

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Ingiriya

answers: NDQ_006063

answers: 60%

answers: NDQ_006064

answers: Nambapana

answers: NDQ_006065

answers: a stream

answers: NDQ_006066

answers: the pacific ocean

answers: NDQ_006067

answers: The Kalu River

answers: NDQ_006068

answers: The Kalu River

answers: NDQ_006069

answers: The highest land in the area is Madakada Giranchi Mountain

text: The first stage is the token generation, or lexical analysis, by which the input character stream is split into meaningful symbols defined by a grammar of regular expressions. For example, a calculator program would look at an input such as "12*(3+4)^2" and split it into the tokens 12, *, (, 3, +, 4, ), ^, 2, each of which is a meaningful symbol in the context of an arithmetic expression. The lexer would contain rules to tell it that the characters *, +, ^, ( and ) mark the start of a new token, so meaningless tokens like "12*" or "(3" will not be generated.

text: The first stage is the token generation, or

text: lexical analysis

text: , by which the input character stream is split into meaningful symbols defined by a grammar of

text: regular expression

text: s. For example, a calculator program would look at an input such as "12*(3+4)^2" and split it into the tokens 12, *, (, 3, +, 4, ), ^, 2, each of which is a meaningful symbol in the context of an arithmetic expression. The lexer would contain rules to tell it that the characters *, +, ^, ( and ) mark the start of a new token, so meaningless tokens like "12*" or "(3" will not be generated.

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text: The area consists of modest rolling hills broken by small streams, all of them fed mainly by run-off from storm drainage, although the community contains at least one natural spring still producing aquifer-fed water. All streams to the east side of Glenmont are part of the Anacostia River watershed; they flow into the Northwest Branch of the Anacostia, which empties into the Potomac. Streams to the west of Glenmont generally reach the Potomac River by way of Rock Creek, with Georgia Avenue serving as a rough dividing line between the two drainage areas.

text: The area consists of modest rolling hills broken by small streams, all of them fed mainly by run-off from storm drainage, although the community contains at least one natural spring still producing aquifer-fed water. All streams to the east side of Glenmont are part of the

text: Anacostia River

text: watershed; they flow into the Northwest Branch of the Anacostia, which empties into the Potomac. Streams to the west of Glenmont generally reach the

text: Potomac River

text: by way of Rock Creek, with Georgia Avenue serving as a rough dividing line between the two drainage areas.

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text: Modern multimedia codecs, like G.718 and Adaptive Multi-Rate (AMR) for audio and H.264 and MPEG-4 for video, have resilience features already built into the syntax and structure of the stream. This allows the codec to (a) detect errors in the stream and (b) potentially correct, or at least conceal, the error during playback. These codecs are ideal partners for UDP-Lite, since they are designed to work with a damaged data stream, and it is better for these codecs to receive perhaps 200 bytes where a few bits are damaged rather than have to conceal the loss of an entire packet that was discarded due to a bad checksum. The application layer understands the significance of the data, where the transport only sees UDP packets. This means that error protection can be added if necessary at a higher layer, for example with a forward error correction scheme. The application is the best place to decide which parts of the stream are most sensitive to error and protect them accordingly, rather than have a single "brute force" checksum that covers everything equally. An example of this can be seen in research by Hammer et al. where UDP-Lite is coupled with the AMR codec to give improved speech quality in lossy network conditions.

text: Modern multimedia codecs, like

text: and

text: Adaptive Multi-Rate

text: (AMR) for audio and

text: and

text: for video, have resilience features already built into the syntax and structure of the stream. This allows the codec to (a) detect errors in the stream and (b) potentially correct, or at least conceal, the error during playback. These codecs are ideal partners for UDP-Lite, since they are designed to work with a damaged data stream, and it is better for these codecs to receive perhaps 200 bytes where a few bits are damaged rather than have to conceal the loss of an entire packet that was discarded due to a bad checksum. The application layer understands the significance of the data, where the transport only sees UDP packets. This means that error protection can be added if necessary at a higher layer, for example with a

text: forward error correction

text: scheme. The application is the best place to decide which parts of the stream are most sensitive to error and protect them accordingly, rather than have a single "brute force" checksum that covers everything equally. An example of this can be seen in research by Hammer et al. where UDP-Lite is coupled with the AMR codec to give improved speech quality in lossy network conditions.

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text: The Hasbani River  ( / ALA-LC: al-Ḥāṣbānī; ) or Snir Stream ( / Nahal Snir), is the major tributary of the Jordan River. The Hasbani River derives most of its discharge from two springs in Lebanon,<ref>FAO (Water Resources section) <blockquote>Overall, there are about 40 major streams in Lebanon and, based on the hydrographic system, the country can be divided into five regions: …[including] the Hasbani river basin in the south-east.

text: The Hasbani River  ( /

text: ALA-LC

text: : al-Ḥāṣbānī; ) or Snir Stream ( / Nahal Snir), is the major

text: tributary

text: of the

text: Jordan River

text: . The Hasbani River derives most of its discharge from two

text: springs

text: in

text: Lebanon

text: ,<ref>

text: FAO

text: (Water Resources section) <blockquote>Overall, there are about 40 major streams in Lebanon and, based on the hydrographic system, the country can be divided into five regions: …[including] the Hasbani river basin in the south-east.

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answers: Hasbani River basin

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answers: derives most of its discharge

answers: NDQ_006066

answers: The Hasbani River

answers: NDQ_006067

answers: Jordan River

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The Hasbani River

text: The Pleasant River Grange is located in a rural area near the center of Vinalhaven island.  The island is nearly divided by the Pleasant River, a north-flowing stream the exits into Vinal Cove; the grange hall is located on the east side of the river near its mouth, on the north side of Round Island Road, east of its junction with North Haven Road.  It is a two-story wood frame structure, with a gabled roof, clapboard siding, and a granite foundation.  The facade facing southeast toward the road is symmetrical, with two sash windows on each floor, and one in the gable.  The main entrance is on the longer southwest facade, near the southern corner and under a shed-roof porch.  The interior has a hallway extending across the front, with a dining room and kitchen in the rear of the first floor, and open auditorium on the second floor.  The walls and ceilings are finished in tongue-and-groove maple.

text: The Pleasant River Grange is located in a rural area near the center of Vinalhaven island.  The island is nearly divided by the Pleasant River, a north-flowing stream the exits into Vinal Cove; the grange hall is located on the east side of the river near its mouth, on the north side of Round Island Road, east of its junction with North Haven Road.  It is a two-story wood frame structure, with a gabled roof, clapboard siding, and a granite foundation.  The facade facing southeast toward the road is symmetrical, with two sash windows on each floor, and one in the gable.  The main entrance is on the longer southwest facade, near the southern corner and under a shed-roof porch.  The interior has a hallway extending across the front, with a dining room and kitchen in the rear of the first floor, and open auditorium on the second floor.  The walls and ceilings are finished in tongue-and-groove maple.

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answers: north-flowing

answers: NDQ_006066

answers: Atlantic Ocean

answers: NDQ_006067

answers: Vinal Cove

answers: NDQ_006068

answers: river

answers: NDQ_006069

answers: Vinalhaven

text: The Chariton River is a  tributary to the Missouri River in southeast Iowa and northeast Missouri. The river forms in southeastern Clarke County, Iowa.  It is dammed at  Rathbun Reservoir in Appanoose County, Iowa and then flows  before entering Missouri where it forms the boundary between Putnam and Schuyler counties. It enters the Missouri River in Chariton County near Keytesville.  are in Missouri and  are in Iowa. The river has been called Missouri's "Grand Divide" because streams west of the Chariton flow into the Missouri and streams east of it flow into the Mississippi River.

text: The Chariton River is a  tributary to the

text: Missouri River

text: in southeast Iowa and northeast Missouri. The river forms in southeastern

text: Clarke County, Iowa

text: .  It is dammed at

text: Rathbun Reservoir

text: in

text: Appanoose County, Iowa

text: and then flows  before entering Missouri where it forms the boundary between

text: Putnam

text: and

text: Schuyler

text: counties. It enters the Missouri River in

text: Chariton County

text: near

text: Keytesville

text: .  are in Missouri and  are in Iowa. The river has been called Missouri's "Grand Divide" because streams west of the Chariton flow into the Missouri and streams east of it flow into the

text: Mississippi River

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answers: Grand Divide

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Grand Divide

answers: NDQ_006063

answers: Missouri River

answers: NDQ_006064

answers: Grand Divide

answers: NDQ_006065

answers: tributary

answers: NDQ_006066

answers: Mississippi River

answers: NDQ_006067

answers: Mississippi River

answers: NDQ_006068

answers: Missouri River

answers: NDQ_006069

answers: Missouri River

text: Near Blowing Rock, North Carolina, the divide meets the Eastern Continental Divide in the Blue Ridge Mountains. This point forms a triple point between the streams draining west to the Tennessee, north to the New River, and east to the coastal rivers of North Carolina.

text: Near

text: Blowing Rock, North Carolina

text: , the divide meets the

text: Eastern Continental Divide

text: in the

text: Blue Ridge Mountains

text: . This point forms a triple point between the streams draining west to the Tennessee, north to the New River, and east to the coastal rivers of

text: North Carolina

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answers: divide meets the Eastern Continental Divide

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answers: a triple point

answers: NDQ_006063

answers: Blue Ridge Mountains

answers: NDQ_006064

answers: Triple point

answers: NDQ_006065

answers: draining

answers: NDQ_006066

answers: the Atlantic Ocean

answers: NDQ_006067

answers: coastal rivers

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Blue Ridge Mountains

text: Drainage density is the total length of all the streams and rivers in a drainage basin divided by the total area of the drainage basin. It is a measure of how well or how poorly a watershed is drained by stream channels. It is equal to the reciprocal of the constant of channel maintenance and equal to the reciprocal of two times the length of overland flow.

text: Drainage density is the total length of all the

text: streams

text: and

text: river

text: s in a

text: drainage basin

text: divided by the total area of the drainage basin. It is a measure of how well or how poorly a watershed is drained by stream channels. It is equal to the reciprocal of the constant of channel maintenance and equal to the reciprocal of two times the length of overland flow.

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answers: the constant of channel maintenance

answers: NDQ_006064

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answers: how well or how poorly

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answers: NDQ_006067

answers: Drainage density

answers: NDQ_006068

answers: drainage

answers: NDQ_006069

answers: a watershed is drained by stream channels

text: Kibby Mountain stands within the watershed of the Kennebec River, which drains into the Gulf of Maine. The north side of Kibby Mountain drains into the East Branch of the Moose River, then into the South Branch of the Moose, the Moose River, and the Kennebec River. The west side of Kibby Mountain drains into Caribou Flow, then into the South Branch of the Moose River. The southwest end of Kibby Mountain drains into the Middle Branch of Kibby Stream, then into Spencer Stream and the Dead River, another tributary of the Kennebec. The southeast side of Kibby Mountain drains into the West Branch of Spencer Stream.

text: Kibby Mountain stands within the

text: watershed

text: of the

text: Kennebec River

text: , which drains into the

text: Gulf of Maine

text: . The north side of Kibby Mountain drains into the

text: East Branch

text: of the Moose River, then into the

text: South Branch

text: of the Moose, the

text: Moose River

text: , and the Kennebec River. The west side of Kibby Mountain drains into Caribou Flow, then into the South Branch of the Moose River. The southwest end of Kibby Mountain drains into the Middle Branch of Kibby Stream, then into Spencer Stream and the

text: Dead River

text: , another

text: tributary

text: of the Kennebec. The southeast side of Kibby Mountain drains into the West Branch of Spencer Stream.

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answers: Kibby Stream

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Gulf of Maine

answers: NDQ_006063

answers: Gulf of Maine

answers: NDQ_006064

answers: Kibby Mountain

answers: NDQ_006065

answers: watershed

answers: NDQ_006066

answers: Gulf of Maine

answers: NDQ_006067

answers: Gulf of Maine

answers: NDQ_006068

answers: the Kennebec River

answers: NDQ_006069

answers: the Kennebec River

text: Three streams are available in this program – one for singers (2 or 3 years), one for operatic repetiteurs (2 years) and one for operatic stage directors (2 years).

text: Three streams are available in this program – one for singers (2 or 3 years), one for operatic repetiteurs (2 years) and one for operatic stage directors (2 years).

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answers: NDQ_006063

answers: singers

answers: NDQ_006064

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answers: NDQ_006065

answers: 2 years

answers: NDQ_006066

answers: operatic stage directors

answers: NDQ_006067

answers: salty

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: operatic stage directors

text: Over time, the main river flows through the landscape, widening a valley and creating a floodplain.  Sediment accumulates and creates a natural levee. Tributaries that want to enter the main channel are not allowed because of this levee.  Instead, the water then enters the back swamps, or form a yazoo stream. Because yazoo streams are separated from the main river by natural levees, they flow and meander (streams and rivers rarely flow in straight lines) parallel to the main stream channel or river on the floodplain for a considerable distance. These series of smooth bends or curves flows with a slight gradient, usually south, and is normally blocked from entering by a natural levee along the larger stream. A yazoo stream will join the major river where it will eventually break through the natural levees and flow into the larger waterway at its belated confluence.

text: Over time, the main river flows through the landscape, widening a valley and creating a

text: floodplain

text: Sediment

text: accumulates and creates a natural

text: levee

text: Tributaries

text: that want to enter the main channel are not allowed because of this levee.  Instead, the water then enters the back swamps, or form a yazoo stream. Because yazoo streams are separated from the main river by natural levees, they flow and meander (streams and rivers rarely flow in straight lines) parallel to the main stream channel or river on the

text: floodplain

text: for a considerable distance. These series of smooth bends or curves flows with a slight gradient, usually south, and is normally blocked from entering by a natural levee along the larger stream. A yazoo stream will join the major river where it will eventually break through the natural levees and flow into the larger waterway at its belated confluence.

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answers: NDQ_006060

answers: its belated confluence

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: a floodplain

answers: NDQ_006063

answers: floodplain

answers: NDQ_006064

answers: back swamps

answers: NDQ_006065

answers: slight gradient

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: yazoo streams

answers: NDQ_006068

answers: a floodplain

answers: NDQ_006069

answers: natural levees

text: The major drainage divide runs from the southwest part of the Akwapim-Togo Ranges northwest through the Kwahu Plateau and then irregularly westward to the Ivory Coast border. Almost all the rivers and streams north of this divide form part of the Volta system. Extending about 1,600 kilometers in length and draining an area of about 388,000 square kilometers, of which about 158,000 km lie within Ghana, the Volta and its tributaries, such as the Afram River and the Oti River, drain more than twothirds of the country. To the south of the divide are several smaller, independent rivers. The most important of these are the Pra River, the Tano River, the Ankobra River, the Birim River, and the Densu River. With the exception of smaller streams that dry up in the dry seasons or rivers that empty into inland lakes, all the major rivers in the country flow into the Gulf of Guinea directly or as tributaries to other major rivers. The Ankobra and Tano are navigable for considerable distances in their lower reaches.

text: The major drainage divide runs from the southwest part of the Akwapim-Togo Ranges northwest through the Kwahu Plateau and then irregularly westward to the Ivory Coast border. Almost all the rivers and streams north of this divide form part of the Volta system. Extending about 1,600 kilometers in length and draining an area of about 388,000 square kilometers, of which about 158,000 km lie within Ghana, the Volta and its tributaries, such as the

text: Afram River

text: and the Oti River, drain more than twothirds of the country. To the south of the divide are several smaller, independent rivers. The most important of these are the Pra River, the Tano River, the Ankobra River, the

text: Birim River

text: , and the

text: Densu River

text: . With the exception of smaller streams that dry up in the dry seasons or rivers that empty into inland lakes, all the major rivers in the country flow into the Gulf of Guinea directly or as tributaries to other major rivers. The Ankobra and Tano are navigable for considerable distances in their lower reaches.

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answers: major drainage divide

answers: NDQ_006061

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answers: Gulf of Guinea

answers: NDQ_006063

answers: Kwahu

answers: NDQ_006064

answers: Plateau

answers: NDQ_006065

answers: dry up in the dry seasons

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: The Ankobra and Tano are navigable for considerable distances in their lower reaches

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Volta system

text: The river experienced a record flood on May 14, 1970 with a  greater than 50 year recurrence interval. At the flood crest the stream gage on the Deep River station at the town of Deep River measured a record stage of  and a stream flow of

text: The river experienced a record flood on May 14, 1970 with a  greater than 50 year

text: recurrence interval

text: . At the

text: flood crest

text: the

text: stream gage

text: on the Deep River station at the town of Deep River measured a record stage of  and a stream flow of

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answers: flood crest

answers: NDQ_006061

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answers: Deep River

answers: NDQ_006063

answers: Deep River

answers: NDQ_006064

answers: Flood crest

answers: NDQ_006065

answers: recorded

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Deep River

answers: NDQ_006068

answers: a record stage

answers: NDQ_006069

text: The Akçay River which divides the town into two parts is the resource of life and natural beauty. It is fed by two different rivers: Kocaman stream stems from the eastern side of Kızlar Plateau, it passes through Devecik and Yoğunoluk towns and falls down over Kocaman and Özpınar ending in İkizce. This stream conjoins in Adalar territory and by passing thorough town it is poured into the Black Sea with the name of Akçay River.

text: The

text: Akçay River

text: which divides the town into two parts is the resource of life and natural beauty. It is fed by two different rivers: Kocaman stream stems from the eastern side of

text: Kızlar Plateau

text: , it passes through Devecik and Yoğunoluk towns and falls down over Kocaman and Özpınar ending in İkizce. This stream conjoins in Adalar territory and by passing thorough town it is poured into the Black Sea with the name of Akçay River.

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answers: NDQ_006064

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answers: NDQ_006065

answers: falls down

answers: NDQ_006066

answers: Kocaman stream

answers: NDQ_006067

answers: Kocaman stream

answers: NDQ_006068

answers: natural beauty

answers: NDQ_006069

answers: Kocaman stream

text: The city is in the northwestern part of Jeollabuk-do. East are the rugged mountains of Mt. Cheonho and Mt. Mireuk (Mireuksan (Jeollabuk-do)) at the edge of the Noryeong Mountains, and northwest the range of Mt. Hamra lead to a series of hills and a great stream that has formed the fertile Okgu plain to the west. Iksan borders Nonsan-gun and Buyeo-gun, Chuncheongnam-do, and is divided by the Keum-gang[river] in the north. It faces the Kimje Plains, divided by Mankyeong-gang, to the south.

text: The city is in the northwestern part of Jeollabuk-do. East are the rugged mountains of Mt. Cheonho and Mt. Mireuk (

text: Mireuksan (Jeollabuk-do)

text: ) at the edge of the Noryeong Mountains, and northwest the range of Mt. Hamra lead to a series of hills and a great stream that has formed the fertile Okgu plain to the west. Iksan borders Nonsan-gun and Buyeo-gun, Chuncheongnam-do, and is divided by the Keum-gang[river] in the north. It faces the Kimje Plains, divided by Mankyeong-gang, to the south.

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answers: Noryeong Mountains

text: The Red River (formerly known as the Ponsandean stream) has been “streamed” for tin up to its source at Tregilliowe (SW540329).

text: The Red River (formerly known as the Ponsandean stream) has been “streamed” for tin up to its source at Tregilliowe (SW540329).

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answers: The Red River

text: The first stage is that of Sotāpanna (Pali; Sanskrit: ), literally meaning "one who enters () the stream (sotas)," with the stream being the supermundane Noble Eightfold Path regarded as the highest Dharma. The stream-enterer is also said to have "opened the eye of the Dharma" (dhammacakkhu, Sanskrit: ).

text: The first stage is that of

text: Sotāpanna

text: Pali

text: Sanskrit

text: : ), literally meaning "one who enters () the stream (sotas)," with the stream being the supermundane

text: Noble Eightfold Path

text: regarded as the highest Dharma. The stream-enterer is also said to have "opened the eye of the Dharma" (dhammacakkhu, Sanskrit: ).

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answers: The first stage is that of Sot panna

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answers: Sot panna

text: Yazoo streams here drain the back swamps of the Wakarusa River Valley.

text: Yazoo streams here drain the back swamps of the Wakarusa River Valley.

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answers: Yazoo streams

text: Some 1,4 km of the stream is passing through culverts and long stretches of it have been straitened out to form part of the local stormwater system.  Notwithstanding, other sections are furnished with promenades and ponds and therefore considered as of local recreational interest.  The municipalities sharing the catchment area, together with the county administrative board, are collaborating to improve water quality and the areas surrounding the stream.

text: Some 1,4 km of the stream is passing through culverts and long stretches of it have been straitened out to form part of the local stormwater system.  Notwithstanding, other sections are furnished with promenades and ponds and therefore considered as of local recreational interest.  The municipalities sharing the catchment area, together with the county administrative board, are collaborating to improve water quality and the areas surrounding the stream.

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text: An underfit stream can result when glaciation modifies the landscape by creating glacial troughs. The rivers that occupy such valleys after the ice has retreated are not in proportion with the size of the valley. Given the scale of most glacial troughs almost all of them contain misfit streams. Misfit streams can also be caused by reductions in the discharge of the stream. Channel size responds rapidly to variations in discharge, but valley size responds over much longer timescales. Many causes of reduced discharges are possible. If misfit streams are widespread in an area, climate change, particularly a reduction in precipitation, is likely to be the cause. If a single river appears to be a misfit stream, it may be as a result of anthropogenic interference through groundwater extraction or dam construction upstream. Natural causes include stream capture or other changes in drainage patterns. For instance, New Zealand's largest river (the Waikato) used to flow through the Hauraki Plains to the North Island's east coast, but changed its course to exit on the west coast due to a large volcanic eruption, leaving its former course through the 1-km wide Hinuera Gap occupied by only a small stream.

text: An underfit stream can result when

text: glaciation

text: modifies the landscape by creating

text: glacial troughs

text: . The rivers that occupy such valleys after the ice has retreated are not in proportion with the size of the

text: valley

text: . Given the scale of most

text: glacial troughs

text: almost all of them contain misfit streams. Misfit streams can also be caused by reductions in the

text: discharge

text: of the stream. Channel size responds rapidly to variations in

text: discharge

text: , but valley size responds over much longer timescales. Many causes of reduced

text: discharges

text: are possible. If misfit streams are widespread in an area,

text: climate change

text: , particularly a reduction in

text: precipitation

text: , is likely to be the cause. If a single river appears to be a misfit stream, it may be as a result of anthropogenic interference through

text: groundwater

text: extraction or

text: dam

text: construction upstream. Natural causes include

text: stream capture

text: or other changes in drainage patterns. For instance, New Zealand's largest river (the

text: Waikato

text: ) used to flow through the

text: Hauraki Plains

text: to the

text: North Island

text: 's east coast, but changed its course to exit on the west coast due to

text: a large volcanic eruption

text: , leaving its former course through the 1-km wide Hinuera Gap occupied by only a small stream.

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text: In the Oxford area the river splits into several streams across the floodplain (Seacourt Stream, Castle Mill Stream, Bulstake Stream and others), creating several islands (Fiddler's Island, Osney and others). Desborough Island, Ham Island at Old Windsor and Penton Hook Island were artificially created by lock cuts and navigation channels. Chiswick Eyot is a familiar landmark on the Boat Race course, while Glover's Island forms the centrepiece of the spectacular view from Richmond Hill.

text: In the Oxford area the river splits into several streams across the

text: floodplain

text: Seacourt Stream

text: Castle Mill Stream

text: Bulstake Stream

text: and others), creating several islands (

text: Fiddler's Island

text: Osney

text: and others).

text: Desborough Island

text: Ham Island

text: at Old Windsor and

text: Penton Hook Island

text: were artificially created by lock cuts and navigation channels.

text: Chiswick Eyot

text: is a familiar landmark on the Boat Race course, while

text: Glover's Island

text: forms the centrepiece of the spectacular view from

text: Richmond Hill

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answers: NDQ_006069

answers: Desborough Island, Ham Island at Old Windsor

text: Catchments from the reserve feeds numerous villages and towns from Kiwira to Katumba to Tukuyu and Kandete, and all settlements in between. All streams from the north, west and southwest flow into the Kiwira River. These streams include the Marogala, Sinini, Kipoke, Kilasi and Mulagala. In the southeast is the source of the Mbaka River, with the Suma River feeding into it. In the east the Mrambo and the Mwatisi flow out of the reserve. All of the above rivers flow into Lake Nyasa. The region's rivers are generally clear and fresh, and the area is outside the mosquito zone. Freshwater fish abound in the rivers. Other rivers flow from various sources in a catchment divide at the area called Igoma in Mbeya rural district. Also, Igoma is a dividing watershed for the two river systems, those flowing southward to lake Nyasa and those flowing northward towards the Usangu plains. The rivers flowing norhtwards are Ipatagwa, Mlowo Mwambalizi and other minor ones and are among tributaries of the great Ruaha River which flows into Indian Ocean.

text: Catchments from the reserve feeds numerous villages and towns from

text: Kiwira

text: to

text: Katumba

text: to

text: Tukuyu

text: and

text: Kandete

text: , and all settlements in between. All streams from the north, west and southwest flow into the

text: Kiwira River

text: . These streams include the

text: Marogala

text: Sinini

text: Kipoke

text: Kilasi

text: and

text: Mulagala

text: . In the southeast is the source of the

text: Mbaka River

text: , with the

text: Suma River

text: feeding into it. In the east the

text: Mrambo

text: and the

text: Mwatisi

text: flow out of the reserve. All of the above rivers flow into

text: Lake Nyasa

text: . The region's rivers are generally clear and fresh, and the area is outside the

text: mosquito

text: zone. Freshwater fish abound in the rivers. Other rivers flow from various sources in a catchment divide at the area called Igoma in Mbeya rural district. Also, Igoma is a dividing watershed for the two river systems, those flowing southward to lake Nyasa and those flowing northward towards the Usangu plains. The rivers flowing norhtwards are Ipatagwa, Mlowo Mwambalizi and other minor ones and are among tributaries of the great Ruaha River which flows into Indian Ocean.

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answers: NDQ_006063

answers: Kiwira River

answers: NDQ_006064

answers: Catchments

answers: NDQ_006065

answers: generally clear and fresh

answers: NDQ_006066

answers: Lake Nyasa

answers: NDQ_006067

answers: mosquito zone

answers: NDQ_006068

answers: Freshwater fish

answers: NDQ_006069

answers: Lake Nyasa

text: A 1971 study of the Chariton River in northern Missouri, United States, found that the channelized section of the river contained only 13 species of fish, whereas the natural segment of the stream was home to 21 species of fish. The biomass of fish able to be caught in the dredged segments of the river was 80 percent less than in the natural parts of the same stream. This loss of fish diversity and abundance is thought to occur because of reduction in habitat, elimination of riffles and pools, greater fluctuation of stream levels and water temperature, and shifting substrates. The rate of recovery for a stream once it has been dredged is extremely slow, with many streams showing no significant recovery 30 to 40 years after the date of channelization.

text: A 1971 study of the

text: Chariton River

text: in northern

text: Missouri

text: , United States, found that the channelized section of the river contained only 13 species of fish, whereas the natural segment of the stream was home to 21 species of fish. The biomass of fish able to be caught in the dredged segments of the river was 80 percent less than in the natural parts of the same stream. This loss of fish diversity and abundance is thought to occur because of reduction in habitat, elimination of riffles and pools, greater fluctuation of stream levels and water temperature, and shifting substrates. The rate of recovery for a stream once it has been dredged is extremely slow, with many streams showing no significant recovery 30 to 40 years after the date of channelization.

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answers: The rate of recovery for a stream once it has been dredged is extremely slow

text: Fluvial terraces are remnants of the former floodplain of a stream or river. They are formed by the downcutting of a river or stream channel into and the abandonment and lateral erosion of its former floodplain. The downcutting, abandonment, and lateral erosion of a former floodplain can be the result of either changes in sea level, local or regional tectonic uplift; changes in local or regional climate; changes the amount of sediment being carried by the river or stream; change in discharge of the river; or a complex mixture of these and other factors. The most common sources of the variations in rivers and streams that create fluvial terraces are vegetative, geomorphic, and hydrologic responses to climate. More recently, the direct modification of rivers and streams and their watersheds by cultural processes have result in the development of terraces along many rivers and streams.

text: Fluvial terraces are remnants of the former

text: floodplain

text: of a stream or river. They are formed by the downcutting of a river or stream channel into and the abandonment and lateral erosion of its former floodplain. The downcutting, abandonment, and lateral erosion of a former floodplain can be the result of either changes in sea level, local or regional tectonic uplift; changes in local or regional climate; changes the amount of sediment being carried by the river or stream; change in discharge of the river; or a complex mixture of these and other factors. The most common sources of the variations in rivers and streams that create fluvial terraces are vegetative, geomorphic, and hydrologic responses to climate. More recently, the direct modification of rivers and streams and their watersheds by cultural processes have result in the development of terraces along many rivers and streams.

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answers: no

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answers: It can be the result of either changes in local or regional climate

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answers: changes in local or regional climate

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answers: downcutting of a river or stream channel

text: "No longer dependent on the larger towns for its success, the road was completed through the wilds of Preston, considerably south of Kingwood, in 1832, and was opened westward to Clarksburg and Parkersburg by 1838. Its construction cost $400,000. It crossed the mountains by easy grades and the larger streams (in some sections all the streams) by good bridges. It was macadamized from Tygart Valley River to Parkersburg in 1848. About 1852, it was further improved by construction of new bridges across several streams at important crossings. In 1840, facilities for travel and news were increased on the western end of the road by the establishment of a daily line of stages, and a regular mail service, which made connection with the Ohio steamers at Parkersburg. By 1845, there was a line of fast tri-weekly stages at Romney to the Ohio at Parkersburg. It connected at Romney with stages from Winchester, from Moorefield, and from Green Spring at which connections were made with Baltimore by trains of the Baltimore and Ohio Railway. The fare from Green Spring to Parkersburg (210 miles) was $10.00."

text: "No longer dependent on the larger towns for its success, the road was completed through the wilds of Preston, considerably south of Kingwood, in 1832, and was opened westward to Clarksburg and Parkersburg by 1838. Its construction cost $400,000. It crossed the mountains by easy grades and the larger streams (in some sections all the streams) by good bridges. It was macadamized from

text: Tygart Valley River

text: to Parkersburg in 1848. About 1852, it was further improved by construction of new bridges across several streams at important crossings. In 1840, facilities for travel and news were increased on the western end of the road by the establishment of a daily line of stages, and a regular mail service, which made connection with the Ohio steamers at Parkersburg. By 1845, there was a line of fast tri-weekly stages at Romney to the Ohio at Parkersburg. It connected at Romney with stages from Winchester, from Moorefield, and from

text: Green Spring

text: at which connections were made with

text: Baltimore

text: by trains of the

text: Baltimore and Ohio

text: Railway. The fare from Green Spring to Parkersburg (210 miles) was $10.00."

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answers: important crossings

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answers: no

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answers: Parkersburg

answers: NDQ_006063

answers: construction cost $400,000.

answers: NDQ_006064

answers: wilds

answers: NDQ_006065

answers: larger streams

answers: NDQ_006066

answers: the pacific ocean

answers: NDQ_006067

answers: Tygart Valley River

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: It crossed the mountains by easy grades

text: Access to key resources, mainly water, is a primary source of the Civil War in Sudan. Ecologically, Sudan is divided into a northern and southern region. The North is densely populated with Arab Muslims. Although the Nile flows through the northern part of Sudan, it is largely beyond the drainage basins of the feeder streams and rivers that consolidate themselves into the White and Blue Niles further to the south. The South is lightly populated, but much more fertile. It receives adequate rainfall and benefits from many feeder streams and springs scattered throughout the area. Persistent drought and desertification, population expansion, and the need to increase food output have forced many northern Arabs to look south for lands and resources. The introduction by the North of mechanized farming equipment continues to threaten southern subsistence farming. Organized as the Sudan People’s Liberation Army (SPLA), southerners have fought back against northern intrusion for the better part of three decades.

text: Access to key resources, mainly water, is a primary source of the Civil War in Sudan. Ecologically, Sudan is divided into a northern and southern region. The North is densely populated with Arab Muslims. Although the Nile flows through the northern part of Sudan, it is largely beyond the drainage basins of the feeder streams and rivers that consolidate themselves into the White and Blue Niles further to the south. The South is lightly populated, but much more fertile. It receives adequate rainfall and benefits from many feeder streams and springs scattered throughout the area. Persistent drought and desertification, population expansion, and the need to increase food output have forced many northern Arabs to look south for lands and resources. The introduction by the North of mechanized farming equipment continues to threaten southern subsistence farming. Organized as the

text: Sudan People’s Liberation Army

text: (SPLA), southerners have fought back against northern intrusion for the better part of three decades.

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text: In musical terminology, Divisi ("div.") is an instruction to divide a single section of instruments into multiple subsections of instruments. This usually applies to the violins of the string section in an orchestra, although violas, cellos, and double basses can also be divided. Typically, 4-part French Horn sections include divided sections if Horns 1/2 and/or 3/4 are not playing the same music ("a2"). Other brass instruments can also be divided but it is not as frequent as with the Horn section. Woodwinds - especially Flutes and Clarinets - also utilize "divisi" to divide music between parts and even between players of the same part.

text: In musical terminology, Divisi ("div.") is an instruction to divide a single section of instruments into multiple subsections of instruments. This usually applies to the

text: violin

text: s of the

text: string section

text: in an

text: orchestra

text: , although

text: viola

text: s,

text: cello

text: s, and

text: double bass

text: es can also be divided. Typically, 4-part

text: French Horn

text: sections include divided sections if Horns 1/2 and/or 3/4 are not playing the same music ("a2"). Other

text: brass instruments

text: can also be divided but it is not as frequent as with the Horn section.

text: Woodwinds

text: - especially

text: Flutes

text: and

text: Clarinets

text: - also utilize "divisi" to divide music between parts and even between players of the same part.

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text: Downcutting, also called erosional downcutting, downward erosion or vertical erosion is a geological process by hydraulic action that deepens the channel of a stream or valley by removing material from the stream's bed or the valley's floor. The speed of downcutting depends on the stream's base level, the lowest point to which the stream can erode. Sea level is the ultimate base level, but many streams have a higher "temporary" base level because they empty into another body of water that is above sea level or encounter bedrock that resists erosion. A concurrent process called lateral erosion refers to the widening of a stream channel or valley. When a stream is high above its base level, downcutting will take place faster than lateral erosion; but as the level of the stream approaches its base level, the rate of lateral erosion increases. This is why streams in  mountainous areas tend to be narrow and swift, forming V-shaped valleys, while streams in lowland areas tend to be wide and slow-moving, with valleys that are correspondingly wide and flat-bottomed. The term gradient refers to the elevation of a stream relative to its base level. The steeper the gradient, the faster the stream flows. Sometimes geological uplift will increase the gradient of a stream even while the stream downcuts toward its base level, a process called "rejuvenation." This happened in the case of the Colorado River in the western United States, resulting in the process that created the Grand Canyon.

text: Downcutting, also called erosional downcutting, downward erosion or vertical erosion is a

text: geological

text: process by

text: hydraulic action

text: that deepens the

text: channel

text: of a

text: stream

text: or

text: valley

text: by removing material from the stream's bed or the valley's floor. The speed of downcutting depends on the stream's

text: base level

text: , the lowest point to which the stream can

text: erode

text: Sea level

text: is the ultimate base level, but many streams have a higher "temporary" base level because they empty into another body of water that is above sea level or encounter

text: bedrock

text: that resists erosion. A concurrent process called

text: lateral erosion

text: refers to the widening of a stream channel or valley. When a stream is high above its base level, downcutting will take place faster than lateral erosion; but as the level of the stream approaches its base level, the rate of lateral erosion increases. This is why streams in

text: mountain

text: ous areas tend to be narrow and swift, forming

text: V-shaped valley

text: s, while streams in

text: lowland

text: areas tend to be wide and slow-moving, with valleys that are correspondingly wide and flat-bottomed. The term

text: gradient

text: refers to the elevation of a stream relative to its base level. The steeper the gradient, the faster the stream flows. Sometimes geological

text: uplift

text: will increase the gradient of a stream even while the stream downcuts toward its base level, a process called "

text: rejuvenation

text: ." This happened in the case of the

text: Colorado River

text: in the western

text: United States

text: , resulting in the process that created the

text: Grand Canyon

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text: The village core of the district is located north of, and near to, the River Dodder, and parts of the broader area within South Dublin are close to the borders of Dublin City, Kildare, Dún Laoghaire–Rathdown and County Wicklow. Several streams flow in the area, notably the Jobstown or Tallaght Stream (a tributary of the Dodder River), and the Fettercairn Stream (a tributary of the River Camac), while the Tymon River, the main component of the River Poddle (Liffey tributary), rises in Cookstown, near Fettercairn.

text: The village core of the district is located north of, and near to, the

text: River Dodder

text: , and parts of the broader area within South Dublin are close to the borders of

text: Dublin City

text: Kildare

text: Dún Laoghaire–Rathdown

text: and

text: County Wicklow

text: . Several streams flow in the area, notably the Jobstown or Tallaght Stream (a tributary of the

text: Dodder River

text: ), and the Fettercairn Stream (a tributary of the

text: River Camac

text: ), while the Tymon River, the main component of the

text: River Poddle

text: Liffey

text: tributary), rises in Cookstown, near Fettercairn.

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text: Therefore, hydronomy can be a tool to reconstruct past cultural interactions, population movements, religious conversions or older languages. For example, history professor Kenneth H. Jackson identified a river-name pattern against which to fit the story of the Anglo-Saxon invasion of Britain and the pockets of survival of native British culture. His river map of Britain divided the island into three principal areas of English settlement: the river valleys draining eastward in which surviving British names are limited to the largest rivers and Saxon settlement was early and dense, the highland spine and a third region whose British hydronyms apply even to the smaller streams.

text: Therefore, hydronomy can be a tool to reconstruct past cultural interactions, population movements, religious conversions or older languages. For example, history professor

text: Kenneth H. Jackson

text: identified a river-name pattern against which to fit the story of the

text: Anglo-Saxon

text: invasion of Britain and the pockets of survival of native British culture. His river map of Britain divided the island into three principal areas of English settlement: the river valleys draining eastward in which surviving British names are limited to the largest rivers and Saxon settlement was early and dense, the highland spine and a third region whose British hydronyms apply even to the smaller streams.

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text: A small stream passes by the village and is popularly known as part of the Kuri River.

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text: The Stage is the seventh studio album by American heavy metal band Avenged Sevenfold. It is a concept album about artificial intelligence and self-destruction of society. It was released on October 28, 2016 after a live stream event on the band's Facebook page. The Stage is the first Avenged Sevenfold album to feature Brooks Wackerman on drums, after departure of Arin Ilejay in July 2015, and the band's first album to be released through Capitol Records. It is also the band's longest studio album at 73 minutes and 35 seconds, thus beating City of Evil by almost a minute. The album also features their longest song to date, "Exist", with a run-time of 15 minutes and 41 seconds.

text: The Stage is the seventh

text: studio album

text: by American

text: heavy metal

text: band

text: Avenged Sevenfold

text: . It is a concept album about artificial intelligence and self-destruction of society. It was released on October 28, 2016 after a live stream event on the band's

text: Facebook

text: page. The Stage is the first Avenged Sevenfold album to feature

text: Brooks Wackerman

text: on drums, after departure of Arin Ilejay in July 2015, and the band's first album to be released through

text: Capitol Records

text: . It is also the band's longest studio album at 73 minutes and 35 seconds, thus beating

text: City of Evil

text: by almost a minute. The album also features their longest song to date, "Exist", with a run-time of 15 minutes and 41 seconds.

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answers: The Stage is also the band's first album to be released through Capitol Records

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text: The meander ratio or sinuosity index is a means of quantifying how much a river or stream meanders (how much its course deviates from the shortest possible path). It is calculated as the length of the stream divided by the length of the valley. A perfectly straight river would have a meander ratio of 1 (it would be the same length as its valley), while the higher this ratio is above 1, the more the river meanders.

text: The meander ratio or

text: sinuosity index

text: is a means of quantifying how much a

text: river

text: or

text: stream

text: meanders (how much its course deviates from the shortest possible path). It is calculated as the

text: length

text: of the stream divided by the length of the

text: valley

text: . A perfectly straight river would have a meander ratio of 1 (it would be the same length as its valley), while the higher this

text: ratio

text: is above 1, the more the river meanders.

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answers: It would be the same length as its valley

answers: NDQ_006068

answers: river or stream meanders

answers: NDQ_006069

answers: The meander ratio or sinuosity index

text: Some source also stated that it was derived from a fruit called "mata kucing" (Euphoria malaiense), a fruit that grows widely in Malaysia and Indonesia. There was also a hill in the city that was named after the fruit, which is called Bukit Mata Kuching. While as been written by a British woman to her son in the 19th century, it was stated that the name was derived from a stream of the same name, called "Sungai Kuching" or Cat River in English. On page 64 of Bamfylde and Baring-Gould's 1909 'A History of Sarawak under its Two White Rajahs', it says: "Kuching, the capital of Sarawak, is so called from a small stream that runs through the town into the main river...." The stream was situated at the foot of Bukit Mata Kuching and in front of the Tua Pek Kong Temple. In the 1950s, the river became very shallow because of silt deposits in the river. The river was later filled to make way for roads.

text: Some source also stated that it was derived from a fruit called "mata kucing" (Euphoria malaiense), a fruit that grows widely in Malaysia and Indonesia. There was also a hill in the city that was named after the fruit, which is called Bukit Mata Kuching. While as been written by a British woman to her son in the 19th century, it was stated that the name was derived from a stream of the same name, called "Sungai Kuching" or Cat River in English. On page 64 of Bamfylde and Baring-Gould's 1909 'A History of Sarawak under its Two White Rajahs', it says: "Kuching, the capital of Sarawak, is so called from a small stream that runs through the town into the main river...." The stream was situated at the foot of Bukit Mata Kuching and in front of the Tua Pek Kong Temple. In the 1950s, the river became very shallow because of silt deposits in the river. The river was later filled to make way for roads.

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answers: a fruit

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answers: very shallow because of silt deposits

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answers: Cat River

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answers: The river was later filled to make way for roads

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The river was later filled to make way for roads

text: Within the Slavonia highlands, the Papuk Mountain stretches from west to east and is the most spacious and most interesting mountain. From the main mountain-ridge well intended are two spurs and a tract watered by a drainage basin in the direction north south. As a remarkable point, emphasis lies on peaks Točak (887 m), Papuk (953 m), Ivačka glava (913 m), Češljakovački vis (820 m), and Kapovac (792 m), which are spread out continuously, and act as a drainage divide between the numerous tributary streams flowing to the river Drava to the north, and the river Sava to the south.

text: Within the Slavonia highlands, the Papuk Mountain stretches from west to east and is the most spacious and most interesting

text: mountain

text: . From the main mountain-ridge well intended are two spurs and a tract watered by a

text: drainage basin

text: in the direction north south. As a remarkable point, emphasis lies on peaks Točak (887 m), Papuk (953 m), Ivačka glava (913 m), Češljakovački vis (820 m), and Kapovac (792 m), which are spread out continuously, and act as a drainage divide between the numerous tributary

text: streams

text: flowing to the river

text: Drava

text: to the north, and the river

text: Sava

text: to the south.

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answers: Papuk Mountain

text: Bessen River is a stream in the U.S. state of Missouri.

text: Bessen River is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

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answers: rivers often provided water, plus

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answers: Bessen River

text: Sources of natural water:- Ibore river, Agua lake, Ohiel Stream Afuda, Oza Stream Idumoza, Ujabhole Stream Eko-Iriobhude, Oraje & Omobo rivers at Ewu.

text: Sources of natural water:- Ibore river, Agua lake, Ohiel Stream Afuda, Oza Stream Idumoza, Ujabhole Stream Eko-Iriobhude, Oraje & Omobo rivers at Ewu.

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text: Some part of these chemicals leaves the field. Nitrogen in forms such as nitrate (NO3) is highly soluble, and along with some pesticides infiltrates downwards toward the water table, where it can migrate to water wells, rivers and streams. A 2008 National Research Council study found that regionally the highest stream concentrations occur where the rates of application were highest, and that these rates were highest in the Corn Belt. These flows mainly stem from corn, which as of 2010 was the major source of total nitrogen loading to the Mississippi River.

text: Some part of these chemicals leaves the field. Nitrogen in forms such as

text: nitrate

text: (NO3) is highly soluble, and along with some pesticides infiltrates downwards toward the

text: water table

text: , where it can migrate to water wells, rivers and streams. A 2008 National Research Council study found that regionally the highest stream concentrations occur where the rates of application were highest, and that these rates were highest in the

text: Corn Belt

text: . These flows mainly stem from corn, which as of 2010 was the major source of total nitrogen loading to the

text: Mississippi River

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text: Along with this increasing complexity of neural representation may come a level of specialization of processing into two distinct pathways: the dorsal stream and the ventral stream (the Two Streams hypothesis, first proposed by Ungerleider and Mishkin in 1982). The dorsal stream, commonly referred to as the "where" stream, is involved in spatial attention (covert and overt), and communicates with regions that control eye movements and hand movements.  More recently, this area has been called the "how" stream to emphasize its role in guiding behaviors to spatial locations. The ventral stream, commonly referred as the "what" stream, is involved in the recognition, identification and categorization of visual stimuli.

text: Along with this increasing complexity of neural representation may come a level of specialization of processing into two distinct pathways: the dorsal stream and the ventral stream (the

text: Two Streams hypothesis

text: , first proposed by Ungerleider and Mishkin in 1982). The dorsal stream, commonly referred to as the "where" stream, is involved in spatial attention (covert and overt), and communicates with regions that control eye movements and hand movements.  More recently, this area has been called the "how" stream to emphasize its role in guiding behaviors to spatial locations. The ventral stream, commonly referred as the "what" stream, is involved in the recognition, identification and categorization of visual stimuli.

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text: In this example, the < stage reads the input disk file and passes the records to the next stage in the pipeline. The locate stage separates the input stream into two output streams. The primary output of locate (records containing Hello) passes the records to the insert stage. The insert stage modifies the input records as specified in its arguments and passes them to its output. The output is connected to faninany that combines records from all input streams to form a single output stream. The output is written to the new disk file.

text: In this example, the < stage reads the input disk file and passes the records to the next stage in the pipeline. The locate stage separates the input stream into two output streams. The primary output of locate (records containing Hello) passes the records to the insert stage. The insert stage modifies the input records as specified in its arguments and passes them to its output. The output is connected to faninany that combines records from all input streams to form a single output stream. The output is written to the new disk file.

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answers: locate stage separates the input stream

text: Long Branch is a stream in the U.S. state of Missouri. It is a tributary of the Salt River.

text: Long Branch is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the

text: Salt River

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text: North Dry Sac River is a stream in the U.S. state of Missouri.

text: North Dry Sac River is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

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answers: North Dry Sac River

text: The confluence of three small rivers (Triveni Sangam); namely Hirnakshi, Bhimakshi and Kosambi; is located here. After the confluence, the river is known as Harnav which merges with Sabarmati river down stream. It divides the town in north and south parts. Harnav river was formerly known as Hiranyaksh or Harnai river.

text: The confluence of three small rivers (Triveni Sangam); namely Hirnakshi, Bhimakshi and Kosambi; is located here. After the confluence, the river is known as Harnav which merges with

text: Sabarmati

text: river down stream. It divides the town in north and south parts. Harnav river was formerly known as Hiranyaksh or Harnai river.

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text: The canal followed the course of Mill Creek from the center of Worcester, MA to the southern part of that community. It then followed the Blackstone River downstream to Ashton, RI. At Ashton, it paralleled the river's west bank, maintaining elevation until it entered Cranberry and Scotts Ponds on the divide of the watershed with the Moshassuck River. It then locked down into the Moshassuck Valley and followed that stream into Providence, RI.

text: The canal followed the course of Mill Creek from the center of Worcester, MA to the southern part of that community. It then followed the Blackstone River downstream to Ashton, RI. At Ashton, it paralleled the river's west bank, maintaining elevation until it entered Cranberry and Scotts Ponds on the divide of the watershed with the Moshassuck River. It then locked down into the Moshassuck Valley and followed that stream into Providence, RI.

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answers: Moshassuck Valley

text: Geographically, Kebumen is located at 7 ° 27 '- 7 ° 50' south latitude and 109 ° 22 '- 109 ° 50' east longitude. The southern part of Kebumen is lowland, while in the northern part of the mountains and hills that are part of a series of South Serayu Mountains. Meanwhile, in the western region Gombong, there Karst South Gombong a limestone mountain range that stretches to the south coast of north-south trending. This area has more than a hundred caves berstalaktit and stalagmites. The largest river in Kebumen is Luk Ulo river, river Jatinegara, Karanganyar rivers, streams Clove, Kedungbener rivers, streams Kemit, Gombong rivers, streams Ijo, Kejawang rivers, and streams Gebang.

text: Geographically, Kebumen is located at 7 ° 27 '- 7 ° 50' south latitude and 109 ° 22 '- 109 ° 50' east longitude. The southern part of Kebumen is lowland, while in the northern part of the mountains and hills that are part of a series of South Serayu Mountains. Meanwhile, in the western region Gombong, there Karst South Gombong a limestone mountain range that stretches to the south coast of north-south trending. This area has more than a hundred caves berstalaktit and stalagmites. The largest river in Kebumen is Luk Ulo river, river Jatinegara, Karanganyar rivers, streams Clove, Kedungbener rivers, streams Kemit, Gombong rivers, streams Ijo, Kejawang rivers, and streams Gebang.

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answers: Gombong rivers, streams Ijo, Kejawang rivers, and streams Gebang

text: The name Edayar came from two words in Malayalam.  "Eda" in Malayalam means in-between and "Aar" means a small river.  A small stream which is part of a tributary to Periyar River is passing through this village. This water stream was the life line of this small village.  The water from this stream was used for agriculture and all other domestic uses by the villagers.

text: The name Edayar came from two words in

text: Malayalam

text: .  "Eda" in Malayalam means in-between and "Aar" means a small river.  A small stream which is part of a tributary to

text: Periyar River

text: is passing through this village. This water stream was the life line of this small village.  The water from this stream was used for agriculture and all other domestic uses by the villagers.

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text: Bulstake Stream, also spelt Bullstake Stream, is a backwater of the River Thames at Oxford, England.

text: Bulstake Stream, also spelt Bullstake Stream, is a backwater of the

text: River Thames

text: at

text: Oxford

text: , England.

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text: Kanchan Daniel and the Beards, all either in their early Twenties with the exception of guitarist Kush Upadhyay [aged 17] and keyboardist Mukesh Lobo [aged 29], have a great time playing the blues, and bring in other influences including R&B, soul, funk and psychedelic rock to form a free flowing stream of sound. With the album due in March this year, the band hopes to play bigger stages across the country and introduce the blues to younger audiences

text: Kanchan Daniel and the Beards, all either in their early Twenties with the exception of

text: guitarist

text: Kush Upadhyay [aged 17] and

text: keyboardist

text: Mukesh Lobo [aged 29], have a great time playing the blues, and bring in other influences including R&B, soul, funk and psychedelic rock to form a free flowing stream of sound. With the album due in March this year, the band hopes to play bigger stages across the country and introduce the blues to younger audiences

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answers: Kanchan Daniel and the Beards

text: A post office was established at Divide in 1879, and remained in operation until 1905. The community most likely was so named on account of its location near a drainage divide.

text: A post office was established at Divide in 1879, and remained in operation until 1905. The community most likely was so named on account of its location near a

text: drainage divide

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answers: drainage divide

text: Rapids are hydrological features between a run (a smoothly flowing part of a stream) and a cascade. Rapids are characterised by the river becoming shallower with some rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white colour, forming what is called "whitewater". Rapids occur where the bed material is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause water aeration of the stream or river resulting in better water quality.

text: Rapids are

text: hydrological

text: features between a run (a smoothly flowing part of a

text: stream

text: ) and a

text: cascade

text: . Rapids are characterised by the river becoming shallower with some

text: rock

text: s exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white colour, forming what is called "

text: whitewater

text: ". Rapids occur where the

text: bed material

text: is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause

text: water aeration

text: of the stream or river resulting in better water quality.

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answers: It does not

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answers: NDQ_006065

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answers: NDQ_006069

answers: Rapids are characterised by the river becoming shallower with some rocks exposed above the flow surface

text: Melet River, Bolaman River, Elekçi River, Turnasuyu Stream, Akçaova Stream and Civil Stream are the main rivers of the province. The topography of the province is not conducive to lake formation and only two major lakes, Gaga Lake and Ulugöl, are present in Ordu.

text: Melet River

text: Bolaman River

text: Elekçi River

text: Turnasuyu Stream

text: Akçaova Stream

text: and

text: Civil Stream

text: are the main rivers of the province. The topography of the province is not conducive to lake formation and only two major lakes,

text: Gaga Lake

text: and

text: Ulugöl

text: , are present in Ordu.

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answers: NDQ_006061

answers: no

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answers: NDQ_006064

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answers: not conducive

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answers: Gaga Lake

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answers: rivers

answers: NDQ_006069

answers: Gaga Lake and Ulugöl

text: A stream channel is the physical confine of a stream (river) consisting of a bed and stream banks.Stream channels exist in a variety of geometries. Stream channel development is controlled by both water and sediment movement. There is a difference between low gradient streams (less than a couple of percent in gradient or slightly sloped) and high gradient streams (steeply sloped). A wide variety of stream channel types can be distinguished (e.g. Braided rivers, Wandering rivers, Single Thread Sinuous rivers etc.). During floods, water flow may exceed the capacity of the channel and flood waters will spill out of the channel and across the valley bottom, floodplain or drainage area.

text: A stream channel is the physical confine of a

text: stream

text: river

text: ) consisting of a

text: bed

text: and

text: stream bank

text: s.Stream channels exist in a variety of geometries. Stream channel development is controlled by both

text: water

text: and

text: sediment

text: movement. There is a difference between low

text: gradient

text: streams (less than a couple of percent in gradient or slightly sloped) and high gradient streams (steeply sloped). A wide variety of stream

text: channel types

text: can be distinguished (e.g.

text: Braided river

text: s, Wandering rivers, Single Thread

text: Sinuous

text: rivers etc.). During

text: flood

text: s, water flow may exceed the capacity of the channel and flood waters will spill out of the channel and across the

text: valley

text: bottom,

text: floodplain

text: or

text: drainage area

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answers: NDQ_006061

answers: It does not

answers: NDQ_006062

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answers: NDQ_006063

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answers: NDQ_006064

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answers: NDQ_006065

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answers: NDQ_006066

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answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: Stream channels

answers: NDQ_006069

answers: low gradient streams

text: Twin Creek is a stream in the U.S. state of Ohio. The  long stream is a tributary of Great Miami River.

text: Twin Creek is a stream in the

text: U.S. state

text: of

text: Ohio

text: . The  long stream is a tributary of

text: Great Miami River

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text: The geographical terrain is 83.7% mountainous and 11.2% cultivable. It is very rugged, except in some of the urban areas and villages that can be found in the valleys and hills. The main water system ranges from the upper stream of the 23.7 km long Namhan River, which flows through the county. Pyeongchang River, one of the streams flowing from Odaesan, joins several streams at Jungnyeong, Danyang, and Geumgok, originating from Sobaeksan. Danyang Stream, which has its source in Hakseongsan, Gyeongsangbuk-do, joins the Namhan River at Habang-ri, Danseong-myeon, together with Jungnyeong Stream flowing from Jungnyeong and Dosolsan to Hyeoncholli, Danyang-eup, Maepo Stream from Geumsusan to Dodam, and Geumgok Stream from Biro Peak to Gosu-ri, Danyang-eup.

text: The geographical terrain is 83.7% mountainous and 11.2% cultivable. It is very rugged, except in some of the urban areas and villages that can be found in the valleys and hills. The main water system ranges from the upper stream of the 23.7 km long

text: Namhan River

text: , which flows through the county.

text: Pyeongchang River

text: , one of the streams flowing from

text: Odaesan

text: , joins several streams at Jungnyeong, Danyang, and Geumgok, originating from

text: Sobaeksan

text: . Danyang Stream, which has its source in

text: Hakseongsan

text: Gyeongsangbuk-do

text: , joins the Namhan River at Habang-ri, Danseong-myeon, together with Jungnyeong Stream flowing from Jungnyeong and

text: Dosolsan

text: to Hyeoncholli, Danyang-eup, Maepo Stream from

text: Geumsusan

text: to Dodam, and Geumgok Stream from Biro Peak to Gosu-ri, Danyang-eup.

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answers: 11.2%

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answers: west side of the continental divide

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answers: the upper stream of the 23.7 km long Namhan River

answers: NDQ_006069

answers: 11.2% cultivable

text: A cultural divide is "a boundary in society that separates communities whose social economic structures, opportunities for success, conventions, styles,  are so different that they have substantially different psychologies". A cultural divide is the virtual barrier caused by cultural differences, that hinder interactions, and harmonious exchange between people of different cultures. For example, avoiding eye contact with a superior shows deference and respect in East Asian cultures, but can be interpreted as suspicious behavior in Western cultures. Studies on cultural divide usually focus on identifying and bridging the cultural divide at different levels of society.

text: A cultural divide is "a boundary in society that separates communities whose social economic structures, opportunities for success, conventions, styles,  are so different that they have substantially different psychologies". A cultural divide is the virtual barrier caused by cultural differences, that hinder interactions, and harmonious exchange between people of different cultures. For example, avoiding eye contact with a superior shows deference and respect in East Asian cultures, but can be interpreted as suspicious behavior in Western cultures. Studies on cultural divide usually focus on identifying and bridging the cultural divide at different levels of society.

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answers: cultural divide at different levels of society

text: The fifth subdivision includes all the streams flowing into Lakes George and Champlain. They are mostly mountain torrents, frequently interrupted by cascades. The principal streams are the Chazy, Saranac, and Ausable rivers, and Wood Creek. Deep strata of Tertiary clay extend along the shores of Lake Champlain and Wood Creek. The water of most of the streams in this region is colored by the iron over which it flows.

text: The fifth subdivision includes all the streams flowing into Lakes George and Champlain. They are mostly mountain torrents, frequently interrupted by cascades. The principal streams are the

text: Chazy

text: Saranac

text: , and

text: Ausable

text: rivers, and Wood Creek. Deep strata of

text: Tertiary

text: clay extend along the shores of Lake Champlain and Wood Creek. The water of most of the streams in this region is colored by the iron over which it flows.

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answers: frequently interrupted by cascades

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answers: Tertiary clay

text: Many plants and animals are at their eastern or westernmost points of natural distribution. The reserve is situated at one of the lowest points of the Great Divide. The streams forming from the east reach the Hunter River, and those from the west eventually flow to the Darling River.

text: Many plants and animals are at their eastern or westernmost points of natural distribution. The reserve is situated at one of the lowest points of the Great Divide. The streams forming from the east reach the

text: Hunter River

text: , and those from the west eventually flow to the

text: Darling River

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answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: natural distribution

text: The county straddles the Tennessee Valley Divide, with waters east of the divide flowing into the Tennessee River, and waters west of the divide flowing into the Mississippi River.  Primary streams include the Beech River and the Forked Deer River.

text: The county straddles the Tennessee Valley Divide, with waters east of the divide flowing into the

text: Tennessee River

text: , and waters west of the divide flowing into the

text: Mississippi River

text: .  Primary streams include the

text: Beech River

text: and the

text: Forked Deer River

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answers: Tennessee River

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answers: NDQ_006063

answers: Tennessee Valley Divide

answers: NDQ_006064

answers: Tennessee Valley

answers: NDQ_006065

answers: flowing

answers: NDQ_006066

answers: Mississippi River

answers: NDQ_006067

answers: Mississippi River

answers: NDQ_006068

answers: Tennessee River

answers: NDQ_006069

answers: Tennessee Valley Divide

text: The Wood River originates in Fortress Lake in Hamber Provincial Park. Its headwater streams drain the western slope of the Continental Divide. The Wood River flows generally southwest to join the Canoe and Columbia rivers in Kinbasket Lake.

text: The Wood River originates in Fortress Lake in

text: Hamber Provincial Park

text: . Its headwater streams drain the western slope of the

text: Continental Divide

text: . The Wood River flows generally southwest to join the Canoe and Columbia rivers in Kinbasket Lake.

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answers: Kinbasket Lake

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Fortress Lake

answers: NDQ_006063

answers: Continental Divide

answers: NDQ_006064

answers: Fortress Lake

answers: NDQ_006065

answers: drain

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Canoe

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Canoe and Columbia rivers

text: This list of rivers and streams in Ostwestfalen-Lippe contains a selection of the rivers, streams and lakes which lie wholly or partly in Ostwestfalen-Lippe (OWL). The rivers are organised based on the Weser, Lippe and Ems river systems. In addition they are sometimes further divided into sub-regions. The list does not contain all named rivers in OWL, but at least all those with a total catchment area of 10 square kilometres. The list of lakes is also not a full list of all named lakes, especially as the distinction with ponds is not always clear.

text: This list of rivers and streams in Ostwestfalen-Lippe contains a selection of the rivers, streams and lakes which lie wholly or partly in

text: Ostwestfalen-Lippe

text: (OWL). The rivers are organised based on the Weser, Lippe and Ems river systems. In addition they are sometimes further divided into sub-regions. The list does not contain all named rivers in OWL, but at least all those with a total catchment area of 10 square kilometres. The list of lakes is also not a full list of all named lakes, especially as the distinction with ponds is not always clear.

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answers: NDQ_006060

answers: ponds

answers: NDQ_006061

answers: It does not

answers: NDQ_006062

answers: Lake Tahoe

answers: NDQ_006063

answers: 10 square kilometres

answers: NDQ_006064

answers: catchment

answers: NDQ_006065

answers: catchment area of 10 square kilometres

answers: NDQ_006066

answers: Ostwestfalen-Lippe

answers: NDQ_006067

answers: Weser

answers: NDQ_006068

answers: rivers and streams

answers: NDQ_006069

answers: the distinction with ponds is not always clear

text: The Dodder's main tributaries after Glenasmole, in and prior to which many streams join, are the Jobstown (or Tallaght) Stream, the Owendoher River and its tributary the Whitechurch Stream, the Little Dargle River (with Castle Stream and other tributaries), the Slang or Dundrum River, the Swan River (or Water), and the small Muckross Stream.

text: The Dodder's main tributaries after Glenasmole, in and prior to which many streams join, are the Jobstown (or Tallaght) Stream, the Owendoher River and its tributary the Whitechurch Stream, the Little Dargle River (with Castle Stream and other tributaries),

text: the Slang or Dundrum River

text: , the Swan River (or Water), and the small Muckross Stream.

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answers: Dodder's main tributaries

text: Elk Fork is a stream in the U.S. state of Missouri. It is a tributary of South Grand River.

text: Elk Fork is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of South Grand River.

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answers: Elk Fork is a stream

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answers: Elk Fork

text: Stream-oriented files consist of a single sequence of bytes on which programs can map application data however they want. Stream files are the primary file model supported by Unix and Unix-like operating systems and by Windows. DDM defines a single stream file model and a single stream access method.

text: Stream-oriented files consist of a single sequence of bytes on which programs can map application data however they want. Stream files are the primary file model supported by

text: Unix

text: and

text: Unix-like

text: operating systems and by

text: Windows

text: . DDM defines a single stream file model and a single stream access method.

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answers: Stream files

text: In the 19th Century the district was still defined by the Währinger Stream, which rises in Pötzleinsdorfer Schlosspark. Originally this stream was in a deep valley along the route of the streets Pötzleinsdorfer Straße, Gersthofer Straße, Gentzgasse and Währinger Straße, and flowed into the River Als in the 9th District. By the end of the 19th Century it had been completely transformed into a drain. The last open-flowing part of the stream system is a stretch of the Dürwaring Stream, near Schafbergbad south of the Ladenburghöhe.

text: In the 19th Century the district was still defined by the Währinger Stream, which rises in Pötzleinsdorfer Schlosspark. Originally this stream was in a deep valley along the route of the streets Pötzleinsdorfer Straße, Gersthofer Straße, Gentzgasse and Währinger Straße, and flowed into the River Als in the

text: 9th District

text: . By the end of the 19th Century it had been completely transformed into a drain. The last open-flowing part of the stream system is a stretch of the Dürwaring Stream, near Schafbergbad south of the Ladenburghöhe.

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answers: By the end of the 19th Century it had been completely transformed into a drain

text: The Dzungarian basin does not have a single catchment center. The northernmost section of Dzungaria is part of the basin of the Irtysh River, which ultimately drains into the Arctic Ocean. The rest of the region is split into a number of endorheic basins. In particular, south of the Irtysh, the Ulungur River ends up in the (presently) endorheic Lake Ulungur. The Southwestern part of the Dzungarian basin drains into the Aibi Lake. In the west-central part of the region, streams flow into (or toward) a group of endorheic lakes that include Lake Manas and Lake Ailik. During the region's geological past, a much larger lake (the "Old Manas Lake") was located in the area of today's Manas Lake; it was fed not only by the streams that presently flow toward it, but also by the Irtysh and Ulungur, which too were flowing toward the Old Manas Lake at the time.

text: The Dzungarian basin does not have a single

text: catchment

text: center. The northernmost section of Dzungaria is part of the basin of the

text: Irtysh River

text: , which ultimately drains into the

text: Arctic Ocean

text: . The rest of the region is split into a number of

text: endorheic basins

text: . In particular, south of the Irtysh, the

text: Ulungur River

text: ends up in the (presently)

text: endorheic

text: Lake Ulungur

text: . The Southwestern part of the Dzungarian basin drains into the

text: Aibi Lake

text: . In the west-central part of the region, streams flow into (or toward) a group of endorheic lakes that include

text: Lake Manas

text: and

text: Lake Ailik

text: . During the region's geological past, a much larger lake (the "Old Manas Lake") was located in the area of today's Manas Lake; it was fed not only by the streams that presently flow toward it, but also by the Irtysh and Ulungur, which too were flowing toward the Old Manas Lake at the time.

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answers: Lake Manas and Lake Ailik

text: A divided family is a family that is divided between two or more countries due to conflict between such countries. Members of a divided family often do not have chance to live together.

text: A divided family is a family that is divided between two or more countries due to conflict between such countries. Members of a divided family often do not have chance to live together.

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text: The Blackwater River is a  river in Aroostook County, Maine. From the confluence of its North Branch and South Branch () in Squa Pan Township (Township 10, Range 4, WELS), the river runs west to St. Croix Stream in Masardis. Via St. Croix Stream and the Aroostook River, the Blackwater River is part of the Saint John River watershed.

text: The Blackwater River is a  river in

text: Aroostook County

text: Maine

text: . From the

text: confluence

text: of its

text: North Branch

text: and

text: South Branch

text: () in Squa Pan Township (Township 10, Range 4, WELS), the river runs west to

text: St. Croix Stream

text: in

text: Masardis

text: . Via St. Croix Stream and the

text: Aroostook River

text: , the Blackwater River is part of the

text: Saint John River

text: watershed.

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answers: Blackwater River

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text: Packetized Elementary Stream (PES) is a

text: specification

text: in the

text: Part 1 (Systems) (ISO/IEC 13818-1) and ITU-T H.222.0 that defines carrying of

text: elementary stream

text: s (usually the output of an audio or video encoder) in packets within

text: MPEG program streams

text: and

text: MPEG transport streams

text: . The elementary stream is

text: packetized

text: by encapsulating sequential data bytes from the elementary stream inside PES packet headers.

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text: On December 19, he struck north again, retracing his path. He crossed Monida Pass, then turned east after crossing the Beaverhead Mountains, passing through a broad prairie between the Pioneer Mountains and the Ruby Range. He followed the Beaverhead River to the Jefferson River again, then explored the Gallatin Valley before turning west to the Big Hole River again. Turning north, he followed a stream until he reached a series of low ridges which divided the Big Hole tributary from the Hellgate Fork of the Bitterroot River.  Crossing these, he arrived at the headwaters of the Deer Lodge River (now known as the Clark Fork River) on December 31. He followed the Deer Lodge River to the Hellgate Fork, and retraced his path back to Fort Owen, which he reached on January 10. They had traveled through heavy snows and strong winds that drove the wind chill tens of degrees below zero, crossed rivers and streams covered in thin ice (through which their horses frequently plunged), and often went hungry. They had crossed the Continental Divide four times in the dead of winter, had identified two wagon routes from Fort Hall to Fort Owen, and seen Beaverhead Rock (which, in 1805, had told the Lemhi Shoshone teenage girl guide Sacagawea that she and the Lewis & Clark Expedition were near her homeland). In 45 days, he had traveled more than .

text: On December 19, he struck north again, retracing his path. He crossed

text: Monida Pass

text: , then turned east after crossing the Beaverhead Mountains, passing through a broad prairie between the

text: Pioneer Mountains

text: and the

text: Ruby Range

text: . He followed the

text: Beaverhead River

text: to the Jefferson River again, then explored the Gallatin Valley before turning west to the Big Hole River again. Turning north, he followed a stream until he reached a series of low ridges which divided the Big Hole tributary from the Hellgate Fork of the Bitterroot River.  Crossing these, he arrived at the headwaters of the Deer Lodge River (now known as the

text: Clark Fork River

text: ) on December 31. He followed the Deer Lodge River to the Hellgate Fork, and retraced his path back to Fort Owen, which he reached on January 10. They had traveled through heavy snows and strong winds that drove the

text: wind chill

text: tens of degrees below zero, crossed rivers and streams covered in thin ice (through which their horses frequently plunged), and often went hungry. They had crossed the Continental Divide four times in the dead of winter, had identified two wagon routes from Fort Hall to Fort Owen, and seen

text: Beaverhead Rock

text: (which, in 1805, had told the

text: Lemhi Shoshone

text: teenage girl guide

text: Sacagawea

text: that she and the Lewis & Clark Expedition were near her homeland). In 45 days, he had traveled more than .

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text: The rivers of the state include a number of small plateau streams flowing southward to the São Francisco River, and several large streams in the eastern part flowing eastward to the Atlantic. The former are the Moxotó, Ema, Pajeú, Terra Nova, Brigida, Boa Vista and Pontai, and are dry channels the greater part of the year.

text: The rivers of the state include a number of small plateau streams flowing southward to the

text: São Francisco River

text: , and several large streams in the eastern part flowing eastward to the Atlantic. The former are the

text: Moxotó

text: Ema

text: Pajeú

text: Terra Nova

text: , Brigida, Boa Vista and Pontai, and are dry channels the greater part of the year.

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text: To keep the stream from running dry, water is piped into it.  The stream is further fed by additional groundwater and influx from sources such as the Taufkirchen duckpond.  The flint layer that had kept the groundwater close to the surface, allowing the stream to form, drops deeper just north of Unterhaching, which also causes the water table to drop.  That would have caused the river to go underground in the gravel of the Munich floodplain, but due to the formation of a silt bed caused by the stream itself, it only goes underground just north of Ostpark at the borders of the districts of Perlach, Ramersdorf and Berg am Laim.

text: To keep the stream from running dry, water is piped into it.  The stream is further fed by additional groundwater and influx from sources such as the Taufkirchen duckpond.  The

text: flint

text: layer that had kept the groundwater close to the surface, allowing the stream to form, drops deeper just north of Unterhaching, which also causes the water table to drop.  That would have caused the river to go underground in the gravel of the Munich floodplain, but due to the formation of a silt bed caused by the stream itself, it only goes underground just north of

text: Ostpark

text: at the borders of the districts of Perlach,

text: Ramersdorf

text: and

text: Berg am Laim

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answers: The stream is further fed by additional groundwater and influx from sources such as the Taufkirchen duckpond

text: The main rivers are the Royon stream, the stream of La Goutte and the stream of Bareille which will combine to form further down the stream of Les Salles.

text: The main rivers are the Royon stream, the stream of La Goutte and the stream of Bareille which will combine to form further down the stream of Les Salles.

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text: In terms of students served, Divide ISD is the smallest district in Texas; the 2015 "graduation/promotion ceremony" featured a mere 11 students and the district had as few as eight students at the beginning of the 2014-2015 school year.  Divide ISD serves much of western Kerr County. Divide ISD is one of the few remaining "one room schoolhouses" in the United States.

text: In terms of students served, Divide ISD is the smallest district in Texas; the 2015 "graduation/promotion ceremony" featured a mere 11 students and the district had as few as eight students at the beginning of the 2014-2015 school year.  Divide ISD serves much of western Kerr County. Divide ISD is one of the few remaining "

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text: Moreau River is a stream in the U.S. state of Missouri.

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text: Spring Creek is a stream in the U.S. state of Ohio. The  stream is a tributary of the Great Miami River.

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text: The main river in this area is the Cuencamé stream. All of the rivers in this area reach the Cuencamé stream. There are many small streams that, in the rainy season, are filled with water. There is another stream near to San Pedro Ocuila named the “Arrieras”.In recent years many of these streams have decreased substantially. The Cuencamé stream runs into the Nazas River at the point named Rancho de Fernández. In the 50's two dams were built to keep the mountain water in the area. These dams have helped the agricultural needs in this north area.

text: The main river in this area is the Cuencamé stream. All of the rivers in this area reach the Cuencamé stream. There are many small streams that, in the rainy season, are filled with water. There is another stream near to San Pedro Ocuila named the “Arrieras”.In recent years many of these streams have decreased substantially. The Cuencamé stream runs into the

text: Nazas River

text: at the point named Rancho de Fernández. In the 50's two dams were built to keep the mountain water in the area. These dams have helped the agricultural needs in this north area.

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text: Kimmage () is a small residential suburb located on the south side of Dublin, Ireland. Surrounded by Crumlin, Greenhills, Harold's Cross, Rathfarnham, Templeogue and Terenure, the name Kimmage comes from the Irish Gaelic cam uisce, which means winding water. In this case it is the water of the River Poddle, a Liffey tributary, which provided the major water supply to medieval Dublin. Rising at Tymon Lake near the Green Hills, it flows through Kimmage, and north to the city after dividing at Mount Argus. One stream flows through via Crumlin and Dolphins Barn to join the River Liffey after Mullinahack, a millrace near Usher's Island. The other stream flows via The Coombe underground around Dublin Castle and into the Liffey further east near Merchants Quay.  Kimmage is divided between postal districts Dublin 12 and Dublin 6W.

text: Kimmage () is a small residential suburb located on the south side of

text: Dublin

text: , Ireland. Surrounded by

text: Crumlin

text: Greenhills

text: Harold's Cross

text: Rathfarnham

text: Templeogue

text: and

text: Terenure

text: , the name Kimmage comes from the Irish Gaelic cam uisce, which means winding water. In this case it is the water of the River Poddle, a Liffey tributary, which provided the major water supply to medieval Dublin. Rising at Tymon Lake near the Green Hills, it flows through Kimmage, and north to the city after dividing at

text: Mount Argus

text: . One stream flows through via Crumlin and Dolphins Barn to join the

text: River Liffey

text: after Mullinahack, a millrace near

text: Usher's Island

text: . The other stream flows via The Coombe underground around Dublin Castle and into the Liffey further east near Merchants Quay.  Kimmage is divided between postal districts

text: Dublin 12

text: and

text: Dublin 6W

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answers: Kimmage is divided between postal districts Dublin 12 and Dublin 6W

text: A misfit stream is  a river that is either too large or too small to have eroded the valley or cave passage in which it flows. This term is also used for a stream or river with meanders that obviously are not proportional in size to the meanders of the valley or meander scars cut into its valley walls. If the misfit stream is too large for either its valley or meanders, it is known as an overfit stream. If the misfit stream is too small for either its valley or meanders, it is known as an underfit stream.

text: A misfit stream is  a river that is either too large or too small to have eroded the valley or cave passage in which it flows. This term is also used for a stream or river with meanders that obviously are not proportional in size to the meanders of the valley or meander scars cut into its valley walls. If the misfit stream is too large for either its valley or meanders, it is known as an overfit stream. If the misfit stream is too small for either its valley or meanders, it is known as an underfit stream.

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answers: valley

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answers: too large or too small

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answers: meanders

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answers: misfit stream

text: The River Stour bifurcates through Canterbury, the western stream powered two watermills and the eastern stream powered eight.

text: The River Stour bifurcates through

text: Canterbury

text: , the western stream powered two watermills and the eastern stream powered eight.

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answers: The River Stour

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answers: bifurcate

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answers: The River Stour

text: The Gulf Coastal Plain's southern boundary is the Gulf of Mexico in the U.S. and the Sierra Madre de Chiapas in Mexico.  On the north, it extends to the Ouachita Highlands of the Interior Low Plateaus and the southern Appalachian Mountains. Its northernmost extent is along the Mississippi embayment (Mississippi Alluvial Valley) as far north as the southern tip of Illinois. To the east the Gulf coastal plain meets the South Atlantic Coastal Plain in  southern Georgia along the basin divide between the rivers flowing into the Gulf and those flowing to the Atlantic and south along the Apalachicola River through the Florida panhandle. The flat to rolling topography is broken by many streams, river riparian areas, and marsh wetlands.The Gulf Coastal Plain also extends into southern Mexico.

text: The Gulf Coastal Plain's southern boundary is the Gulf of Mexico in the U.S. and the

text: Sierra Madre de Chiapas

text: in Mexico.  On the north, it extends to the

text: Ouachita Highlands

text: of the Interior Low Plateaus and the southern

text: Appalachian Mountains

text: . Its northernmost extent is along the

text: Mississippi embayment

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text: . To the east the Gulf coastal plain meets the

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text: in  southern Georgia along the basin divide between the rivers flowing into the Gulf and those flowing to the Atlantic and south along the

text: Apalachicola River

text: through the Florida panhandle. The flat to rolling topography is broken by many streams, river

text: riparian

text: areas, and marsh wetlands.The Gulf Coastal Plain also extends into southern Mexico.

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answers: The Gulf Coastal Plain also extends into southern Mexico

text: Wyaconda River is a stream in the U.S. state of Missouri.

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text: On February 6, 2006, A City by the Light Divided was announced for release. "Counting 5-4-3-2-1" was made available for streaming on February 28. From mid March to the beginning of April, the band went on the first leg of the Shirts for a Cure tour, with support from Minus the Bear, The Number Twelve Looks Like You, and We're All Broken. On March 29, "At This Velocity" was made available for streaming via Alternative Press. For most of April, the band went on the 2006 edition of the Taste of Chaos tour. However, on April 13, Rickly became ill, resulting in the band dropping off the tour. On April 18, A City by the Light Divided was made available for streaming via the band's Myspace profile, and "Counting 1-2-3-4-5" was released to radio.

text: On February 6, 2006, A City by the Light Divided was announced for release. "Counting 5-4-3-2-1" was made available for streaming on February 28. From mid March to the beginning of April, the band went on the first leg of the Shirts for a Cure tour, with support from

text: Minus the Bear

text: The Number Twelve Looks Like You

text: , and We're All Broken. On March 29, "At This Velocity" was made available for streaming via

text: Alternative Press

text: . For most of April, the band went on the

text: 2006 edition

text: of the

text: Taste of Chaos

text: tour. However, on April 13, Rickly became ill, resulting in the band dropping off the tour. On April 18, A City by the Light Divided was made available for streaming via the band's

text: Myspace

text: profile, and "Counting 1-2-3-4-5" was released to radio.

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text: Banister Branch is a stream in the U.S. state of Missouri. It is a tributary of the Flat River.

text: Banister Branch is a

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text: . It is a tributary of the Flat River.

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answers: Pacific Ocean

answers: NDQ_006067

answers: Bacteria

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: Banister Branch

text: Manta is located in a depression formed by the river basin of the Aguacia River that divides the territory into two parts. The territory is bounded by a mountain course that begins and ends in the north where the Machetá River and the Aguacia River form the Sunuba River, tributary of the water reservoir of La Esmeralda ("The Emerald"), in Chivor. At the top of the mountain, is the Laguna del Cerro ("Lake of the Hill"), which has been established as a nature reserve area of the municipality. There are several creeks and streams along the mountain river flowing into the 'Aguacia river'. Some of these streams as it descends through the mountains and waterfalls form the creek of El Golpe ("The Strike").

text: Manta is located in a depression formed by the river basin of the Aguacia River that divides the territory into two parts. The territory is bounded by a mountain course that begins and ends in the north where the Machetá River and the Aguacia River form the Sunuba River, tributary of the water reservoir of La Esmeralda ("The Emerald"), in

text: Chivor

text: . At the top of the mountain, is the Laguna del Cerro ("Lake of the Hill"), which has been established as a nature reserve area of the municipality. There are several creeks and streams along the mountain river flowing into the 'Aguacia river'. Some of these streams as it descends through the mountains and waterfalls form the creek of El Golpe ("The Strike").

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answers: NDQ_006061

answers: No

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answers: NDQ_006068

answers: Rivers

answers: NDQ_006069

answers: Aguacia River

text: The stream that drains the lake is a tributary of the Juncalillo River, which flows into the Juncal River.

text: The stream that drains the lake is a tributary of the Juncalillo River, which flows into the

text: Juncal River

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answers: Juncalillo River

text: Nearly all of the precipitation that falls on Albania drains into the rivers and reaches the coast without even leaving the country. In the north, only one small stream escapes Albania. In the south, an even smaller rivulet drains into Greece. Because the topographical divide is east of the Albanian border with its neighbors, a considerable amount of water from other countries drains through Albania. An extensive portion of the basin of the White Drin river (Drini i Bardhë), basin is in the Rrafshi i Dukagjinit area, across Albania's northeastern border. The three eastern lakes that Albania shares with its neighboring countries, as well as the streams that flow into them, drain into the Black Drin river (Drini i Zi). The watershed divide in the south also dips nearly  into Greece at one point. Several tributaries of the Vjosa River rise in that area.

text: Nearly all of the precipitation that falls on Albania drains into the

text: river

text: s and reaches the coast without even leaving the country. In the north, only one small stream escapes Albania. In the south, an even smaller rivulet drains into Greece. Because the topographical divide is east of the Albanian border with its neighbors, a considerable amount of water from other countries drains through Albania. An extensive portion of the basin of the

text: White Drin

text: river (Drini i Bardhë), basin is in the Rrafshi i Dukagjinit area, across Albania's northeastern border. The three eastern lakes that Albania shares with its neighboring countries, as well as the streams that flow into them, drain into the

text: Black Drin

text: river (Drini i Zi). The watershed divide in the south also dips nearly  into Greece at one point. Several tributaries of the

text: Vjosa River

text: rise in that area.

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answers: NDQ_006067

answers: In the north, only one small stream escapes Albania

answers: NDQ_006068

answers: a considerable amount of water from other countries

answers: NDQ_006069

answers: In the north, only one small stream escapes Albania

text: The direction of Oregon stream flow is influenced by four major drainage divides: the Oregon Coast Range on the west, the Cascade Range further inland, the Klamath–Siskiyou Mountains in the southwest, and the Blue Mountains in the northeast. One set of streams, including the Nehalem River, flows directly into the Pacific Ocean or into larger streams flowing directly to the Pacific; other streams, such as the Deschutes River, flow into the Columbia River or its tributaries. A third set, including the Klamath River and its tributaries, originates in Oregon, but its waters eventually flow into northern California before reaching the ocean. Other streams like the Donner und Blitzen River flow into closed basins, such as Malheur Lake, that have no outlet to the sea.

text: The direction of Oregon stream flow is influenced by four major drainage divides: the

text: Oregon Coast Range

text: on the west, the

text: Cascade Range

text: further inland, the

text: Klamath

text: Siskiyou

text: Mountains in the southwest, and the

text: Blue Mountains

text: in the northeast. One set of streams, including the

text: Nehalem River

text: , flows directly into the Pacific Ocean or into larger streams flowing directly to the Pacific; other streams, such as the

text: Deschutes River

text: , flow into the Columbia River or its tributaries. A third set, including the

text: Klamath River

text: and its tributaries, originates in Oregon, but its waters eventually flow into northern California before reaching the ocean. Other streams like the

text: Donner und Blitzen River

text: flow into

text: closed basin

text: s, such as

text: Malheur Lake

text: , that have no outlet to the sea.

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answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Malheur Lake

answers: NDQ_006063

answers: Pacific Ocean

answers: NDQ_006064

answers: drainage divide

answers: NDQ_006065

answers: direction of Oregon stream flow

answers: NDQ_006066

answers: The direction of Oregon stream flow

answers: NDQ_006067

answers: closed basins

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: the Columbia River or its tributaries

text: The main branches of Mirusha River are: the river of Biniqëve, "Lugu i Perrockës", "Lugu i Malishevës", Stopanica, the river of Bubavec and the stream of Kijevo. Most streams, even those who have large catchment area, for each year in the dry season of the year they dry in the lower parts of the territory, such as: The stream of Kijevo, the brook of Drenoc and the river of Bubavec.

text: The main branches of Mirusha River are: the river of Biniqëve, "Lugu i Perrockës", "Lugu i Malishevës", Stopanica, the river of Bubavec and the stream of Kijevo. Most streams, even those who have large catchment area, for each year in the dry season of the year they dry in the lower parts of the territory, such as: The stream of Kijevo, the brook of Drenoc and the river of Bubavec.

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answers: brook of Drenoc

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Mirusha River

answers: NDQ_006063

answers: lower

answers: NDQ_006064

answers: catchment

answers: NDQ_006065

answers: large catchment area

answers: NDQ_006066

answers: Mirusha River

answers: NDQ_006067

answers: It does not say

answers: NDQ_006068

answers: river of Bubavec

answers: NDQ_006069

answers: Mirusha River

text: One system, developed by Strahler, known as the Strahler stream order, ranks streams based on a hierarchy of tributaries. Each segment of a stream or river within a river network is treated as a node in a tree, with the next segment downstream as its parent. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream, and so on.

text: One system, developed by

text: Strahler

text: , known as the

text: Strahler stream order

text: , ranks streams based on a hierarchy of tributaries. Each segment of a stream or river within a river network is treated as a node in a tree, with the next segment downstream as its parent. When two first-order streams come together, they form a second-order stream. When two second-order streams come together, they form a third-order stream, and so on.

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answers: first-order

answers: NDQ_006061

answers: no

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answers: Strahler stream order

answers: NDQ_006063

answers: tributaries

answers: NDQ_006064

answers: tributary

answers: NDQ_006065

answers: ranks streams

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: The Strahler stream order

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: The Strahler stream order

text: Stream capture, river capture, or stream piracy is a geomorphological phenomenon occurring when a stream or river drainage system or watershed is diverted from its own bed, and flows instead down the bed of a neighbouring stream.  This can happen for several reasons, including:

text: Stream capture, river capture, or stream piracy is a

text: geomorphological

text: phenomenon occurring when a stream or river

text: drainage system

text: or

text: watershed

text: is diverted from its own bed, and flows instead down the bed of a neighbouring stream.  This can happen for several reasons, including:

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answers: Stream capture

answers: NDQ_006061

answers: diverted

answers: NDQ_006062

answers: piracy

answers: NDQ_006063

answers: watershed

answers: NDQ_006064

answers: Stream capture

answers: NDQ_006065

answers: diverted

answers: NDQ_006066

answers: diverted water from its own bed

answers: NDQ_006067

answers: Stream capture

answers: NDQ_006068

answers: piracy

answers: NDQ_006069

answers: diverted water

text: The river is  long, making it the third longest in South Korea. The area of the Geum River Basin is . The upper part of the river flows slowly through part of the Noryeong Mountains and is marked by extensive stream meandering. On the other hand, river curves on middle and lower parts of the river are more gradual and there is comparatively less stream meandering.

text: The river is  long, making it the third longest in South Korea. The area of the Geum River Basin is . The upper part of the river flows slowly through part of the Noryeong Mountains and is marked by extensive stream meandering. On the other hand, river curves on middle and lower parts of the river are more gradual and there is comparatively less stream meandering.

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text: Stream load is a geologic term referring to the solid matter carried by a stream (Strahler and Strahler, 2006).  Erosion and bed shear stress continually remove mineral material from the bed and banks of the stream channel, adding this material to the regular flow of water.  The amount of solid load that a stream can carry, or stream capacity, is measured in metric tons per day, passing a given location.  Stream capacity is dependent upon the stream’s velocity, the amount of water flow, and the  gradation (because streams that occur on steeper slopes tend to have greater flow and velocity) (Strahler and Strahler, 2006).

text: Stream load is a geologic term referring to the solid matter carried by a

text: stream

text: (Strahler and Strahler, 2006).

text: Erosion

text: and bed

text: shear stress

text: continually remove mineral material from the

text: bed

text: and banks of the stream channel, adding this material to the regular flow of water.  The amount of solid load that a stream can carry, or stream capacity, is measured in metric tons per day, passing a given location.  Stream capacity is dependent upon the stream’s

text: velocity

text: , the amount of water flow, and the

text: gradation

text: (because streams that occur on steeper slopes tend to have greater flow and velocity) (Strahler and Strahler, 2006).

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text: Divided governments are seen by different groups as a benefit or as an undesirable product of said separations. Those in favor of divided government believe that the separations encourage more policing of those in power by the opposition, as well as limiting spending and the expansion of undesirable laws. Opponents, however, argue that divided governments become lethargic, leading to many gridlocks. In the late 1980s, Terry M. Moe, a professor of political science at Stanford University, examined the issue. He concluded that divided governments lead to compromise which can be seen as beneficial. But he also noticed that divided governments subvert performance and politicize the decisions of executive agencies.

text: Divided governments are seen by different groups as a benefit or as an undesirable product of said separations. Those in favor of divided government believe that the separations encourage more policing of those in power by the opposition, as well as limiting spending and the expansion of undesirable laws. Opponents, however, argue that divided governments become lethargic, leading to many

text: gridlock

text: s. In the late 1980s,

text: Terry M. Moe

text: , a professor of political science at

text: Stanford University

text: , examined the issue. He concluded that divided governments lead to compromise which can be seen as beneficial. But he also noticed that divided governments subvert performance and politicize the decisions of executive agencies.

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answers: a benefit or as an undesirable product

text: A continental divide is a drainage divide such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea. In the Laurentian Divide, water north of the height of land flows to the Arctic Ocean by rivers to Hudson Bay or directly to the Arctic.  Water south of the divide makes its way to the Atlantic Ocean by a variety of streams, including the Great Lakes and Saint Lawrence River to the east, and the Mississippi River to the Gulf of Mexico to the south. Many sources consider Hudson Bay to be part of the Atlantic Ocean, not the Arctic, which would make the Laurentian Divide a lesser divide between the seas of one ocean.

text: A continental divide is a drainage divide such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea. In the Laurentian Divide, water north of the height of land flows to the

text: Arctic Ocean

text: by rivers to

text: Hudson Bay

text: or directly to the Arctic.  Water south of the divide makes its way to the

text: Atlantic Ocean

text: by a variety of streams, including the

text: Great Lakes

text: and

text: Saint Lawrence River

text: to the east, and the

text: Mississippi River

text: to the

text: Gulf of Mexico

text: to the south. Many sources consider Hudson Bay to be part of the Atlantic Ocean, not the Arctic, which would make the Laurentian Divide a lesser divide between the seas of one ocean.

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answers: Water south of the divide makes its way to the Atlantic Ocean

text: The audio data stream in an audio CD is continuous, but has three parts. The main portion, which is further divided into playable audio tracks, is the program area. This section is preceded by a lead-in track and followed by a lead-out track. The lead-in and lead-out tracks encode only silent audio, but all three sections contain subcode data streams.

text: The audio data stream in an audio CD is continuous, but has three parts. The main portion, which is further divided into playable audio tracks, is the program area. This section is preceded by a lead-in track and followed by a lead-out track. The lead-in and lead-out tracks encode only silent audio, but all three sections contain

text: subcode

text: data streams.

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text: Extending from the south-east angle of the main group of buildings are the walls and foundations of a secondary group of buildings (17, 18). These have been identified as the hospitium or the abbot's house, but they occupy the position in which the infirmary is more usually found. The hall was a very spacious apartment, measuring 83 ft. in length by 48 ft. 9 inches in breadth, which was divided by two rows of columns. The fish-ponds lay between the monastery and the river to the south. The abbey mill was situated about 80 yards to the north-west. The millpool may be distinctly traced, together with the goit or mill stream.

text: Extending from the south-east angle of the main group of buildings are the walls and foundations of a secondary group of buildings (17, 18). These have been identified as the hospitium or the abbot's house, but they occupy the position in which the infirmary is more usually found. The hall was a very spacious apartment, measuring 83 ft. in length by 48 ft. 9 inches in breadth, which was divided by two rows of columns. The fish-ponds lay between the monastery and the river to the south. The abbey mill was situated about 80 yards to the north-west. The millpool may be distinctly traced, together with the

text: goit

text: or mill stream.

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answers: The hall was a very spacious apartment

text: A glacier turns into the Wakhan River and joins the Pamir River about  downstream.Bill Colegrave's expedition to Wakhan in 2007 found that both claimants 2 and 3 had the same source, the Chelab stream, which bifurcates on the watershed of the Little Pamir, half flowing into Lake Chamaktin and half into the parent stream of the Little Pamir/Sarhad River. Therefore, the Chelab stream may be properly considered the true source or parent stream of the Oxus.The Panj River forms the border of Afghanistan and Tajikistan. It flows west to Ishkashim where it turns north and then north-west through the Pamirs passing the Tajikistan–Afghanistan Friendship Bridge. It subsequently forms the border of Afghanistan and Uzbekistan for about , passing Termez and the Afghanistan–Uzbekistan Friendship Bridge. It delineates the border of Afghanistan and Turkmenistan for another  before it flows into Turkmenistan at Atamurat. As the Amudarya, it flows across Turkmenistan south to north, passing Türkmenabat, and forms the border of Turkmenistan and Uzbekistan from Halkabat. It is then split by the Tuyamuyun Hydro Complex into many waterways that used to form the river delta joining the Aral Sea, passing Urgench, Daşoguz, and other cities, but it does not reach what is left of the sea any more and is lost in the desert.

text: A glacier turns into the

text: Wakhan River

text: and joins the Pamir River about  downstream.Bill Colegrave's expedition to Wakhan in 2007 found that both claimants 2 and 3 had the same source, the Chelab stream, which bifurcates on the watershed of the Little Pamir, half flowing into Lake Chamaktin and half into the parent stream of the Little Pamir/Sarhad River. Therefore, the Chelab stream may be properly considered the true source or parent stream of the Oxus.The Panj River forms the border of

text: Afghanistan

text: and

text: Tajikistan

text: . It flows west to

text: Ishkashim

text: where it turns north and then north-west through the

text: Pamirs

text: passing the

text: Tajikistan–Afghanistan Friendship Bridge

text: . It subsequently forms the border of Afghanistan and Uzbekistan for about , passing

text: Termez

text: and the

text: Afghanistan–Uzbekistan Friendship Bridge

text: . It delineates the border of Afghanistan and Turkmenistan for another  before it flows into Turkmenistan at

text: Atamurat

text: . As the Amudarya, it flows across Turkmenistan south to north, passing

text: Türkmenabat

text: , and forms the border of Turkmenistan and Uzbekistan from

text: Halkabat

text: . It is then split by the

text: Tuyamuyun Hydro Complex

text: into many waterways that used to form the

text: river delta

text: joining the Aral Sea, passing

text: Urgench

text: Daşoguz

text: , and other cities, but it does not reach what is left of the sea any more and is lost in the desert.

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text: Treisman links the process of binding that occurs in the focused attention stage to physiology by noting that an object causes activity in both the '’what'’ and '’where'’ streams of the cortex (see Two-streams hypothesis). Activity in the '’what'’ stream would include information about color and form, while activity in the '’where'’ stream would include information about location and motion. According to Treisman, attention is the "glue" that combines the information from both streams and causes us to perceive all the features of an object as combined at one specific location. It is easy to consider perceiving one object in isolation, but when we consider multiple objects, numerous features exist at many locations. The perceptual system's task is to associate each of these features with the object to which it belongs. Feature integration theory proposes that in order for this to occur, we need to focus our attention on each object in turn. Once we attend to a particular location, the features at that location are bound together and are associated with the object at that location.

text: Treisman links the process of binding that occurs in the focused attention stage to physiology by noting that an object causes activity in both the '’what'’ and '’where'’ streams of the cortex (see

text: Two-streams hypothesis

text: ). Activity in the '’what'’ stream would include information about color and form, while activity in the '’where'’ stream would include information about location and motion. According to Treisman, attention is the "glue" that combines the information from both streams and causes us to perceive all the features of an object as combined at one specific location. It is easy to consider perceiving one object in isolation, but when we consider multiple objects, numerous features exist at many locations. The perceptual system's task is to associate each of these features with the object to which it belongs. Feature integration theory proposes that in order for this to occur, we need to focus our attention on each object in turn. Once we attend to a particular location, the features at that location are bound together and are associated with the object at that location.

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answers: attention

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: location and motion

answers: NDQ_006063

answers: the cortex

answers: NDQ_006064

answers: location

answers: NDQ_006065

answers: location and motion

answers: NDQ_006066

answers: the pacific ocean and on the east side the atlantic ocean

answers: NDQ_006067

answers: The salty ocean

answers: NDQ_006068

answers: location and motion

answers: NDQ_006069

answers: The perceptual system's task is to associate each of these features with the object to which it belongs

text: Nemegtomaia was discovered in the Nemegt Formation of southwestern Mongolia. Many genera of oviraptorosaur are known from this formation, and may have been ecologically divided. This geologic formation has never been dated radiometrically, but the fauna present in the fossil record indicate it was probably deposited during the early Maastrichtian stage, at the end of the Late Cretaceous about 70 million years ago. The rock facies of the Nemegt Formation suggest the presence of stream and river channels, mudflats, and shallow lakes. Such large river channels and soil deposits are evidence of a far more humid climate than those found in the older Barun Goyot and Djadochta formations. However, caliche deposits indicate at least periodic droughts occurred. Sediment was deposited in the channels and floodplains of large rivers.

text: Nemegtomaia was discovered in the Nemegt Formation of southwestern Mongolia. Many genera of oviraptorosaur are known from this formation, and may have been ecologically divided. This

text: geologic formation

text: has never been

text: dated radiometrically

text: , but the

text: fauna

text: present in the fossil record indicate it was probably deposited during the early

text: Maastrichtian

text: stage, at the end of the

text: Late Cretaceous

text: about 70 million years ago. The rock

text: facies

text: of the Nemegt Formation suggest the presence of stream and river channels, mudflats, and shallow lakes. Such large river channels and soil deposits are evidence of a far more humid climate than those found in the older

text: Barun Goyot

text: and

text: Djadochta

text: formations. However,

text: caliche

text: deposits indicate at least periodic droughts occurred. Sediment was deposited in the channels and floodplains of large rivers.

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answers: Nemegt Formation

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answers: no

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answers: Nemegt Formation

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answers: Nemegt Formation

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answers: Nemegt

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answers: periodic

answers: NDQ_006066

answers: west side of the continental divide

answers: NDQ_006067

answers: The rock facies of the Nemegt Formation

answers: NDQ_006068

answers: mudflats

answers: NDQ_006069

answers: caliche deposits indicate at least periodic droughts

text: There are several streams with the Tarkio name in the Missouri River bottoms near where the Tarkio meets the Missouri.  Almost none of the streams actually flows into the Tarkio although some are historically part of the river.

text: There are several streams with the Tarkio name in the Missouri River bottoms near where the Tarkio meets the Missouri.  Almost none of the streams actually flows into the Tarkio although some are historically part of the river.

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answers: 0

answers: NDQ_006060

answers: Missouri River bottoms

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Tarkio

answers: NDQ_006063

answers: Missouri River

answers: NDQ_006064

answers: Tarkio

answers: NDQ_006065

answers: Almost none

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: Tarkio

answers: NDQ_006068

answers: rivers provided water

answers: NDQ_006069

answers: Tarkio

text: Until about 1925, snails were collected from small sites located in Kalalau Stream, Hanakoa Stream, Hanakāpī`ai Stream, Wainiha River, and Keālia Stream. Three of these populations (Hanakoa Stream, Hanakāpī`ai Stream, Wainiha River) are now thought to be extirpated. Since about 1993, Federal and State agencies, academic researchers, and other interested parties have conducted opportunistic surveys at approximately 50 sites along numerous streams and their associated tributaries and springs on Kaua'i, and have located four previously unknown populations of Newcomb's snail. These recently discovered populations are located in Lumaha`i River, the Hanalei River, Makaleha Stream (a tributary to Kapa`a Stream), and the North Fork Wailua River. With the exception of the snails at Makaleha Springs, most of these populations have only been observed once or twice. Recently, two individual snails were reported from a single site in Limahuli Stream in the Hanalei District of Kauaʻi's north shore. However, if a viable population of Newcomb's snail exists in the Limahuli watershed, its location remains unknown, therefore Limahuli Stream is not considered to have a "population" of Newcomb's snails.

text: Until about 1925, snails were collected from small sites located in

text: Kalalau Stream

text: Hanakoa Stream

text: Hanakāpī`ai Stream

text: Wainiha River

text: , and

text: Keālia Stream

text: . Three of these populations (Hanakoa Stream, Hanakāpī`ai Stream, Wainiha River) are now thought to be extirpated. Since about 1993, Federal and State agencies, academic researchers, and other interested parties have conducted opportunistic surveys at approximately 50 sites along numerous streams and their associated tributaries and springs on Kaua'i, and have located four previously unknown populations of Newcomb's snail. These recently discovered populations are located in

text: Lumaha`i River

text: , the

text: Hanalei River

text: Makaleha Stream

text: (a tributary to

text: Kapa`a Stream

text: ), and the North Fork

text: Wailua River

text: . With the exception of the snails at Makaleha Springs, most of these populations have only been observed once or twice. Recently, two individual snails were reported from a single site in

text: Limahuli Stream

text: in the

text: Hanalei District

text: of Kauaʻi's north shore. However, if a viable population of Newcomb's snail exists in the Limahuli watershed, its location remains unknown, therefore Limahuli Stream is not considered to have a "

text: population

text: " of Newcomb's snails.

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answers: 4

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answers: 0

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answers: 0

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answers: 0

answers: NDQ_006060

answers: Makaleha Stream

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Kauai

answers: NDQ_006063

answers: Limahuli

answers: NDQ_006064

answers: site

answers: NDQ_006065

answers: opportunistic

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: no

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Limahuli Stream is not considered to have a "population" of Newcomb's snails

text: In addition to the Santry River (historically Skillings Glas), Raheny is also crossed by the Naniken River (previously parts of it named Ballyhoy after a townland through which it passes), the Fox Stream and the Blackbanks Stream, all monitored by Dublin City Council.  Both the Fox and Blackbanks Streams flow from the limestone area above Station Road (which used to hold caves and quarries), one either side of the steep Mount Olive hill on Station Road. The Fox Stream runs through Walmer lands, under Tuscany Downs, but is today smaller than historically, as some of its flow is diverted by pipe before the railway, into the already larger Blackbanks Stream.  According to a chronicle of the ceremony of "Riding the Franchises", the Fox Stream used to mark the northern boundary of Dublin City.

text: In addition to the

text: Santry River

text: (historically Skillings Glas), Raheny is also crossed by the

text: Naniken River

text: (previously parts of it named Ballyhoy after a townland through which it passes), the Fox Stream and the Blackbanks Stream, all monitored by Dublin City Council.  Both the Fox and Blackbanks Streams flow from the limestone area above Station Road (which used to hold caves and quarries), one either side of the steep Mount Olive hill on Station Road. The Fox Stream runs through Walmer lands, under Tuscany Downs, but is today smaller than historically, as some of its flow is diverted by pipe before the railway, into the already larger Blackbanks Stream.  According to a chronicle of the ceremony of "Riding the Franchises", the Fox Stream used to mark the northern boundary of Dublin City.

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text: Each course (year of study) have different streams that the student can choose between. A stream is a specific focus of study. There are five streams all in all, plus the ability to do a Bachelor of Theology. The student can change stream at the end of each year of study, so if a student chooses a stream that only runs for one or two years, and wishes to continue to study for higher awards, the student can transfer into the second or third year of a different stream that runs for longer.

text: Each course (year of study) have different streams that the student can choose between. A stream is a specific focus of study. There are five streams all in all, plus the ability to do a Bachelor of Theology. The student can change stream at the end of each year of study, so if a student chooses a stream that only runs for one or two years, and wishes to continue to study for higher awards, the student can transfer into the second or third year of a different stream that runs for longer.

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answers: The student can change stream

text: The main stream of the Matla River is divided into two arms near Purandar. One passes through Kultali-Garanbose and then passes through the Sundarbans. The other passes through Basanti, Pathankhali, Surjyaberia, Masjidbati and then meets Bidyadhari River.

text: The main stream of the Matla River is divided into two arms near Purandar. One passes through Kultali-Garanbose and then passes through the Sundarbans. The other passes through Basanti, Pathankhali, Surjyaberia, Masjidbati and then meets

text: Bidyadhari River

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answers: Sundarbans

text: While Chirimba industrial area is designated a heavy industrial area, it is the least developed in terms of number of industries. Apart from Makata, Ginnery corner industrial site is another active site followed by Limbe and Maselema. The least are Chirimba and Maone industrial sites. Chitawira and Maselema are classic examples of light industrial areas. All the industrial areas are located along the banks of the main rivers or streams of Blantyre city. Makata industrial area lies between Mudi and Nasolo streams whilst Ginnery Corner industrial area is along Mudi River. Maselema industrial area exists along the Naperi river and Chirimba stream hosts Chirimba industrial area.

text: While Chirimba industrial area is designated a heavy industrial area, it is the least developed in terms of number of industries. Apart from Makata, Ginnery corner industrial site is another active site followed by Limbe and Maselema. The least are Chirimba and Maone industrial sites. Chitawira and Maselema are classic examples of light industrial areas. All the industrial areas are located along the banks of the main rivers or streams of Blantyre city. Makata industrial area lies between Mudi and Nasolo streams whilst Ginnery Corner industrial area is along Mudi River. Maselema industrial area exists along the Naperi river and Chirimba stream hosts Chirimba industrial area.

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answers: NDQ_006067

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answers: NDQ_006068

answers: rivers or streams

answers: NDQ_006069

answers: Chirimba industrial area is designated a heavy industrial area

text: All rivers and streams are part of three major drainage systems. Coastal drainage system is characterized by small, ephemeral streams and hill torrents. Rivers and streams that do not possess any significant perennial flow constitute Inland system that dominates the central and northwestern area of the province. Nari, Kaha and Gaj rivers are part of Indus drainage system located in the northeastern margins of the province. The flow in rivers is typified by spring runoff and occasional flash floods. The rivers beds are dry and look like small streams. Stream gradients are high and the rate of run off is very rapid. The Zhob River Basin drains towards the northeast into the Gomal River which ultimately joins the Indus River. Streams along the border of Punjab and Sindh provinces flow toward the east and southeast into the Indus River. Central and western Balochistan drains towards the south and the southwest into the Arabian Sea. Some areas located in districts Chaghi, Kharan, and Panjgur drain into playa lakes, locally called " Hamun" such as Humun-e-Lora and Hamun-e-Mashkel etc.

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answers: playa lakes

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answers: NDQ_006062

answers: Coastal drainage system

answers: NDQ_006063

answers: Coastal drainage system

answers: NDQ_006064

answers: hill torrents

answers: NDQ_006065

answers: rate of run off is very rapid

answers: NDQ_006066

answers: the Arabian Sea

answers: NDQ_006067

answers: Arabian Sea

answers: NDQ_006068

answers: spring runoff and occasional flash floods

answers: NDQ_006069

answers: The Zhob River Basin

text: Three kinds of streams are formed by headward erosion: insequent streams, subsequent streams, and obsequent and resequent streams (See Fluvial landforms of streams.) Insequent streams form by random headward erosion, usually from sheetflow of water over the landform surface. The water collects in channels where the velocity and erosional power increase, cutting into and extending the heads of gullies. Subsequent streams form by selective headward erosion by cutting away at less resistive rocks in the terrain. Obsequent and resequent streams form after time in an area of insequent or subsequent streams. Obsequent streams are insequent streams that now flow in an opposite direction of the original drainage pattern. Resequent streams are subsequent streams that have also changed direction from their original drainage patterns. (Easterbrook, p. 149)

text: Three kinds of streams are formed by headward erosion: insequent streams, subsequent streams, and obsequent and resequent streams (See

text: Fluvial landforms of streams

text: .) Insequent streams form by random headward erosion, usually from sheetflow of water over the landform surface. The water collects in channels where the velocity and erosional power increase, cutting into and extending the heads of gullies. Subsequent streams form by selective headward erosion by cutting away at less resistive rocks in the terrain. Obsequent and resequent streams form after time in an area of insequent or subsequent streams. Obsequent streams are insequent streams that now flow in an opposite direction of the original drainage pattern. Resequent streams are subsequent streams that have also changed direction from their original drainage patterns. (Easterbrook, p. 149)

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answers: Insequent streams

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Insequent streams

answers: NDQ_006063

answers: landform surface

answers: NDQ_006064

answers: Fluvial landform

answers: NDQ_006065

answers: selective

answers: NDQ_006066

answers: Insequent streams form by random headward erosion, usually from sheetflow of water over the landform surface

answers: NDQ_006067

answers: Insequent streams form by random headward erosion

answers: NDQ_006068

answers: Insequent streams

answers: NDQ_006069

answers: Insequent streams form by random headward erosion, usually from sheetflow of water over the landform surface

text: Águas Emendadas lies on the height of land between the Tocantins River basin in the north and the Paraná River basin in the south.The Vereda Grande stream running to the north meets the Maranhão River, a tributary of the Tocantins.The Brejinho stream running south combines with the Fumal stream which feeds the São Bartolomeu River, which joins the Corumbá River, which in turn meets the Paranaíba River and forms the Paraná.Since the area is very flat, parts may flood during the rainy season from December to March. This allows fish from the two rivers basins to mingle.

text: Águas Emendadas lies on the

text: height of land

text: between the

text: Tocantins River

text: basin in the north and the

text: Paraná River

text: basin in the south.The Vereda Grande stream running to the north meets the

text: Maranhão River

text: , a tributary of the Tocantins.The Brejinho stream running south combines with the Fumal stream which feeds the

text: São Bartolomeu River

text: , which joins the

text: Corumbá River

text: , which in turn meets the

text: Paranaíba River

text: and forms the Paraná.Since the area is very flat, parts may flood during the rainy season from December to March. This allows fish from the two rivers basins to mingle.

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answers: may flood

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answers: NDQ_006069

answers: the Paraná

text: Although chalk streams are generally watercourses originating from chalk hills, including winterbournes, streams and rivers, the term chalk stream is used even for larger rivers, which would normally be too large for the term stream. Somme River is a chalk stream on a larger scale.

text: Although chalk streams are generally watercourses originating from chalk hills, including

text: winterbournes

text: stream

text: s and

text: river

text: s, the term chalk stream is used even for larger rivers, which would normally be too large for the term stream.

text: Somme River

text: is a chalk stream on a larger scale.

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answers: chalk streams are generally watercourses

text: Nubanusit Brook is a  stream located in southern New Hampshire in the United States.  It is a tributary of the Contoocook River, part of the Merrimack River watershed.

text: Nubanusit Brook is a

text: stream

text: located in southern

text: New Hampshire

text: in the

text: United States

text: .  It is a

text: tributary

text: of the

text: Contoocook River

text: , part of the

text: Merrimack River

text: watershed

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text: Kolli Hills are known for their medicinal herbs. A few kilometres into the forest, in the higher hills called Agaya Gangai (Heavenly Ganges), there are water falls, part of a river system that feeds the stream at Puliancholai. The stream is known locally as Iyyaar or Kallaar; it grows into a wild river during rains, and is believed to have medicinal properties.

text: Kolli Hills

text: are known for their medicinal herbs. A few kilometres into the forest, in the higher hills called

text: Agaya Gangai

text: (Heavenly Ganges), there are water falls, part of a river system that feeds the stream at Puliancholai. The stream is known locally as Iyyaar or Kallaar; it grows into a wild river during rains, and is believed to have medicinal properties.

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answers: No

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answers: medicinal herbs

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answers: Kolli Hills

text: According to the U.S. Census Bureau, the county has a total area of , of which  is land and  (0.7%) is water. Part of the county's eastern border is defined by the Wabash River. The North Fork of the Embarras River and Hurricane Creek are the main streams in western Clark County. Other than the Wabash River, Big Creek is the major stream in the eastern part of the county.

text: According to the

text: U.S. Census Bureau

text: , the county has a total area of , of which  is land and  (0.7%) is water. Part of the county's eastern border is defined by the

text: Wabash River

text: . The North Fork of the

text: Embarras River

text: and Hurricane Creek are the main streams in western Clark County. Other than the Wabash River, Big Creek is the major stream in the eastern part of the county.

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answers: (0.7%) is water

text: In North America, another, mainly non-mountainous divide, the Laurentian Divide (or Northern Divide), further separates the Hudson Bay-Arctic Ocean drainage region from the Atlantic watershed region. Secondary divides separate the watersheds that flow into the Great Lakes and Saint Lawrence River (ultimately into the Atlantic) from watersheds that flow to the Atlantic via the Missouri-Mississippi complex. Another secondary divide follows the Appalachian chain, which separates those streams and rivers that flow directly into the Atlantic Ocean from those that exit via the Mississippi River.

text: In North America, another, mainly non-mountainous divide, the

text: Laurentian Divide

text: (or Northern Divide), further separates the

text: Hudson Bay

text: Arctic Ocean

text: drainage region from the Atlantic watershed region. Secondary divides separate the watersheds that flow into the

text: Great Lakes

text: and

text: Saint Lawrence River

text: (ultimately into the Atlantic) from watersheds that flow to the Atlantic via the

text: Missouri-Mississippi complex

text: . Another secondary divide follows the Appalachian chain, which separates those streams and rivers that flow directly into the Atlantic Ocean from those that exit via the Mississippi River.

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answers: the Laurentian Divide

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answers: flow directly into the Atlantic Ocean

answers: NDQ_006066

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answers: NDQ_006067

answers: Atlantic Ocean

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The Appalachian chain

text: The Ohio River, which streams westward from Pittsburgh, Pennsylvania, to Cairo, Illinois, is the largest tributary, by volume, of the Mississippi River in the United States. At the confluence, the Ohio is considerably bigger than the Mississippi (Ohio at Cairo: 281,500 cu ft/s (7,960 m/s); Mississippi at Thebes: 208,200 cu ft/s (5,897 m/s)) and, thus, is hydrologically the main stream of the whole river system, including the Allegheny River further upstream.

text: The Ohio River, which streams westward from

text: Pittsburgh

text: Pennsylvania

text: , to

text: Cairo, Illinois

text: , is the largest

text: tributary

text: , by volume, of the

text: Mississippi River

text: in the

text: United States

text: . At the

text: confluence

text: , the Ohio is considerably bigger than the Mississippi (Ohio at Cairo: 281,500 cu ft/s (7,960 m/s); Mississippi at

text: Thebes

text: : 208,200 cu ft/s (5,897 m/s)) and, thus, is hydrologically the main stream of the whole river system, including the

text: Allegheny River

text: further upstream.

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answers: NDQ_006061

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answers: NDQ_006062

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answers: NDQ_006063

answers: Mississippi

answers: NDQ_006064

answers: Thebes

answers: NDQ_006065

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answers: NDQ_006066

answers: The Ohio River

answers: NDQ_006067

answers: Mississippi River

answers: NDQ_006068

answers: rivers provided water, plus

answers: NDQ_006069

answers: The Ohio River

text: Holes Creek is a stream in the U.S. state of Ohio. The  long stream is a tributary of the Great Miami River.

text: Holes Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Ohio

text: . The  long stream is a tributary of the

text: Great Miami River

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answers: NDQ_006063

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answers: NDQ_006064

answers: tributary

answers: NDQ_006065

answers: a tributary

answers: NDQ_006066

answers: Great Miami River

answers: NDQ_006067

answers: The Great Miami River

answers: NDQ_006068

answers: the Great Miami River

answers: NDQ_006069

answers: Great Miami River

text: The Mâtnic River is a tributary of the Timiş River in Romania.  It is referred to as the Lazewski River by Hungarians and as the Čamak River by the Serbians.  The Mâtnic River disintegrates into the Ramon Streams.

text: The Mâtnic River is a

text: tributary

text: of the

text: Timiş River

text: in

text: Romania

text: .  It is referred to as the Lazewski River by

text: Hungarians

text: and as the Čamak River by the

text: Serbians

text: .  The Mâtnic River disintegrates into the Ramon Streams.

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answers: NDQ_006061

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answers: Ramon Streams

answers: NDQ_006063

answers: Timiş River

answers: NDQ_006064

answers: tributary

answers: NDQ_006065

answers: disintegrates

answers: NDQ_006066

answers: the Atlantic Ocean

answers: NDQ_006067

answers: amak River

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Ramon Streams

text: Bighorn National Forest is located in northern Wyoming, United States and consists of over 1.1 million acres (4,500 km²). Created as a US Forest Reserve in 1897, it is one of the oldest government-protected forest lands in the U.S. The forest is well east of the continental divide and extends from the Montana border for a distance of 80 miles (130 km) along the spine of the Big Horn Mountains, an outlying mountain range separated from the rest of the Rocky Mountains by Bighorn Basin. Elevations range from 5,000 feet (1,500 m) along the sagebrush and grass-covered lowlands at the foot of the mountains, to 13,189 feet (4,020 m) on top of Cloud Peak, the highest point in the Big Horn Mountains. Around 99% of the land is above . The forest is named after the Bighorn River, which is partially fed by streams found in the forest. Streams in the range are fed primarily by snowmelt and snowmelt mixed with driving rainfall.

text: Bighorn National Forest is located in northern

text: Wyoming

text: United States

text: and consists of over 1.1 million acres (4,500 km²). Created as a US

text: Forest Reserve

text: in 1897, it is one of the oldest government-protected forest lands in the U.S. The forest is well east of the

text: continental divide

text: and extends from the

text: Montana

text: border for a distance of 80 miles (130 km) along the spine of the

text: Big Horn Mountains

text: , an outlying mountain range separated from the rest of the

text: Rocky Mountains

text: by

text: Bighorn Basin

text: . Elevations range from 5,000 feet (1,500 m) along the

text: sagebrush

text: and grass-covered lowlands at the foot of the mountains, to 13,189 feet (4,020 m) on top of

text: Cloud Peak

text: , the highest point in the Big Horn Mountains. Around 99% of the land is above . The forest is named after the

text: Bighorn River

text: , which is partially fed by streams found in the forest. Streams in the range are fed primarily by

text: snowmelt

text: and snowmelt mixed with driving

text: rainfall

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answers: 5,000 feet

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answers: NDQ_006065

answers: driven rainfall

answers: NDQ_006066

answers: the pacific ocean

answers: NDQ_006067

answers: Bighorn Basin

answers: NDQ_006068

answers: Streams

answers: NDQ_006069

answers: Bighorn Basin

text: The Iowa Flood Center at the University of Iowa operates the largest real-time flood monitoring system of its kind in the world.  It includes more than 200 real-time stream stage sensors that feed data into the Iowa Flood Information System where data can be viewed, online, by disaster management staff and the general public. The stream stage sensors, mounted on bridges and culverts, use ultrasonic sensors to monitor stream and river levels.

text: The Iowa Flood Center at the University of Iowa operates the largest real-time flood monitoring system of its kind in the world.  It includes more than 200 real-time stream stage sensors that feed data into the Iowa Flood Information System where data can be viewed, online, by disaster management staff and the general public. The stream stage sensors, mounted on bridges and culverts, use ultrasonic sensors to monitor stream and river levels.

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answers: Iowa Flood Information System

text: The central stoneroller is widespread in freshwater streams throughout a large portion of the eastern, central, and midwestern United States. It is present in the Atlantic Ocean, Great Lakes, Mississippi River, and Hudson Bay basins in the US, from New York west to North Dakota and Wyoming and south to South Carolina and Texas.  Isolated populations are also found in Canada and Mexico.  The central stoneroller is benthopelagic, inhabiting either the midwaters or bottom of freshwater streams and rivers.   It requires some current and is most commonly found in riffles and pools of moderate to high gradient streams with a gravel substrate bottom.  However, it is a very tolerant species and can be found in almost any stream system with adequate food, leading to it widespread distribution.

text: The central stoneroller is widespread in freshwater streams throughout a large portion of the eastern, central, and midwestern

text: United States

text: . It is present in the

text: Atlantic Ocean

text: Great Lakes

text: Mississippi River

text: , and

text: Hudson Bay

text: basins in the US, from

text: New York

text: west to

text: North Dakota

text: and

text: Wyoming

text: and south to

text: South Carolina

text: and

text: Texas

text: .  Isolated populations are also found in

text: Canada

text: and

text: Mexico

text: .  The central stoneroller is

text: benthopelagic

text: , inhabiting either the midwaters or bottom of freshwater streams and rivers.   It requires some current and is most commonly found in

text: riffle

text: s and pools of moderate to high

text: gradient

text: streams with a gravel

text: substrate

text: bottom.  However, it is a very tolerant species and can be found in almost any stream system with adequate food, leading to it widespread distribution.

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answers: riffles

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answers: a gravel substrate bottom

answers: NDQ_006064

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answers: NDQ_006065

answers: high gradient

answers: NDQ_006066

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answers: NDQ_006067

answers: Atlantic Ocean

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: It is a very tolerant species

text: The Pacific Crest Trail follows, approximately, the high water divide of the Cascades, along the headwaters of many of the streams of the Naches River basin.

text: The

text: Pacific Crest Trail

text: follows, approximately, the high water divide of the Cascades, along the headwaters of many of the streams of the Naches River basin.

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answers: no

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answers: NDQ_006063

answers: Cascades

answers: NDQ_006064

answers: headwaters

answers: NDQ_006065

answers: high

answers: NDQ_006066

answers: Pacific

answers: NDQ_006067

answers: high water divide

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Cascades

text: Galaxiids are coolwater species, with many wholly freshwater species specialising in high-altitude upland streams (including very small streams), rivers, and lakes.  Some galaxiids include a marine stage in their lifecycles where larvae are washed out to sea to develop, and return to rivers as juveniles. This type of diadromous fish migration is known as amphidromy. These species are consequently also found in low-altitude habitats, but frequently migrate to high-altitude reaches of river systems in their adult stage.

text: Galaxiids are coolwater species, with many wholly freshwater species specialising in high-altitude upland streams (including very small streams), rivers, and lakes.  Some galaxiids include a marine stage in their lifecycles where larvae are washed out to sea to develop, and return to rivers as juveniles. This type of diadromous

text: fish migration

text: is known as amphidromy. These species are consequently also found in low-altitude habitats, but frequently migrate to high-altitude reaches of river systems in their adult stage.

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text: The topography is steep, rising from east to west and from south to north. The average elevation is about  above sea level and can be divided into two regions: low-lying regions on the left bank of the Red River basin and the high right bank of the Red River and in the plateau between the Red River and Da River there are many mountains. Besides the two main rivers, the Red and the Da, the province has about 200 canals, small streams and large lakes and swamps. Thác Bà Lake is situated in the province, an artificial lake which has an area of  and 1,331 islands and hills. It has a capacity of 3 to 3.9 billion cubic meters of water and its original intention was to run the Thác Bà hydroelectric plant, one of the first large hydropower projects in Vietnam. The water in the lake is blue and clear, and reflects the surrounding green forests. The thousands of hills and islands have many caves, including Hum, Cau Cuoi and Bach Xa. A Thác Bà Temple is located in the lake area. Thác Bà Lake has changed the climatic pattern in the western districts of the province, to a moderate condition from its  hot and dry status.

text: The topography is steep, rising from east to west and from south to north. The average elevation is about  above sea level and can be divided into two regions: low-lying regions on the left bank of the Red River basin and the high right bank of the Red River and in the plateau between the Red River and

text: Da River

text: there are many mountains. Besides the two main rivers, the Red and the Da, the province has about 200 canals, small streams and large lakes and swamps.

text: Thác Bà Lake

text: is situated in the province, an

text: artificial lake

text: which has an area of  and 1,331 islands and hills. It has a capacity of 3 to 3.9 billion cubic meters of water and its original intention was to run the Thác Bà

text: hydroelectric

text: plant, one of the first large hydropower projects in Vietnam. The water in the lake is blue and clear, and reflects the surrounding green forests. The thousands of hills and islands have many caves, including Hum, Cau Cuoi and Bach Xa. A Thác Bà Temple is located in the lake area. Thác Bà Lake has changed the climatic pattern in the western districts of the province, to a moderate condition from its  hot and dry status.

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text: In recent decades, the valley has also become a major wine producer, with multiple American Viticultural Areas of its own. With a cooler climate than California, the gently rolling hills surrounding the Willamette are home to some of the best (and most expensive) Pinot noir in the world, as well as a high-quality Pinot gris. Although this distinction is not officially recognized, many wine connoisseurs further divide the Willamette Valley into northern and southern regions, the dividing line being the approximate latitude of Salem (approximately 45° north latitude). Not all portions of the Willamette Valley are suitable for vineyards, however, and the largest concentration of wineries is found west of the Willamette River, on the leeward slopes of the Coast Range, or among the numerous river and stream valleys created by Willamette River tributaries.  By far, the largest concentration of wineries is in Yamhill County.

text: In recent decades, the valley has also become a major

text: wine

text: producer, with multiple

text: American Viticultural Area

text: s of its own. With a cooler

text: climate

text: than

text: California

text: , the gently rolling hills surrounding the Willamette are home to some of the best (and most expensive)

text: Pinot noir

text: in the world, as well as a high-quality

text: Pinot gris

text: . Although this distinction is not officially recognized, many wine connoisseurs further divide the Willamette Valley into northern and southern regions, the dividing line being the approximate latitude of Salem (approximately 45° north latitude). Not all portions of the Willamette Valley are suitable for vineyards, however, and the largest concentration of wineries is found west of the Willamette River, on the leeward slopes of the Coast Range, or among the numerous river and stream valleys created by Willamette River tributaries.  By far, the largest concentration of wineries is in Yamhill County.

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answers: cooler climate than California

text: Streams are processed differently from batch data – normal functions cannot operate on streams as a whole, as they have potentially unlimited data, and formally, streams are codata (potentially unlimited), not data (which is finite). Functions that operate on a stream, producing another stream, are known as filters, and can be connected in pipelines, analogously to function composition. Filters may operate on one item of a stream at a time, or may base an item of output on multiple items of input, such as a moving average.

text: Streams are processed differently from

text: batch data

text: – normal functions cannot operate on streams as a whole, as they have potentially unlimited data, and formally, streams are

text: codata

text: (potentially unlimited), not data (which is finite). Functions that operate on a stream, producing another stream, are known as

text: filters

text: , and can be connected in

text: pipelines

text: , analogously to

text: function composition

text: . Filters may operate on one item of a stream at a time, or may base an item of output on multiple items of input, such as a

text: moving average

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answers: Streams are processed differently

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answers: potential unlimited data

answers: NDQ_006069

answers: Streams are processed differently from batch data

text: The Cacapon River Watershed is made up of three major river segments and many smaller stream watersheds. The headwaters of the Cacapon River, known as the Lost River, is  long and receives water from a watershed covering . The largest tributary of the Cacapon is the North River, which drains , an area comparable to that of the Lost River. Overall, the Cacapon River watershed includes the Lost and North River watersheds, and those of many smaller streams for a total of . The Cacapon watershed is itself part of the Chesapeake Bay watershed.

text: The Cacapon River Watershed is made up of three major river segments and many smaller stream watersheds. The

text: headwaters

text: of the Cacapon River, known as the

text: Lost River

text: , is  long and receives water from a watershed covering . The largest tributary of the Cacapon is the

text: North River

text: , which drains , an area comparable to that of the Lost River. Overall, the Cacapon River watershed includes the Lost and North River watersheds, and those of many smaller streams for a total of . The Cacapon watershed is itself part of the

text: Chesapeake Bay

text: watershed.

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answers: NDQ_006068

answers: River Watershed

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answers: The Cacapon River Watershed

text: Arkansas contains approximately  of surface waters, including  of perennial streams and  of total streams. ADEQ uses six ultimate receiving streams to subdivide the state into primary watersheds: Arkansas River, Mississippi River, Ouachita River, Red River, St. Francis River, and White River. This six basins collect water from over 1600 smaller watersheds throughout the state via tributary streams, as described below.

text: Arkansas contains approximately  of surface waters, including  of perennial streams and  of total streams. ADEQ uses six ultimate receiving streams to subdivide the state into primary watersheds:

text: Arkansas River

text: Mississippi River

text: Ouachita River

text: Red River

text: St. Francis River

text: , and

text: White River

text: . This six basins collect water from over 1600 smaller watersheds throughout the state via tributary streams, as described below.

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answers: Arkansas contains approximately of surface waters

text: Adults are mainly found in still or slow-moving water in the lower parts of coastal streams and rivers, or around the edges of lagoons; they can tolerate a wide range of natural conditions. If oxygen levels are low as a result of eutrophication, they can jump out of the water (emerse) and take up oxygen through their skin as a last resort. They need access to riparian vegetation for spawning, and usually live in river systems with access to the sea, as their larval stage is marine. They tend to be found in lower-elevation streams as unlike other species of Galaxias they cannot climb past waterfalls.

text: Adults are mainly found in still or slow-moving water in the lower parts of coastal streams and rivers, or around the edges of lagoons; they can tolerate a wide range of natural conditions. If oxygen levels are low as a result of

text: eutrophication

text: , they can jump out of the water (emerse) and take up oxygen through their skin as a last resort. They need access to riparian vegetation for spawning, and usually live in river systems with access to the sea, as their larval stage is marine. They tend to be found in lower-elevation streams as unlike other species of Galaxias they cannot climb past waterfalls.

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answers: lower

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answers: NDQ_006065

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answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Galaxias

answers: NDQ_006068

answers: access to the sea

answers: NDQ_006069

answers: adult stage is marine

text: The southwest end of Big Spencer Mountain drains into Kidney Brook, then into Lobster Lake, and into the West Branch of the Penobscot River, and into Penobscot Bay. The northeast end of Big Spencer Mountain drains into spring-fed Blood Pond where the pond's outlet, Maxfield Brook, then empties into Lobster Lake. Part of the southeast side of Big Spencer Mountain drains into Bear Brook, then into Ragged Lake, Ragged Stream, Caribou Lake, Chesuncook Lake, Ripogenus Lake, and into the West Branch Penobscot River. The southern part of the southeast side of Big Spencer drains into Lazy Tom Stream, thene into the Roach River, and Moosehead Lake, the source of the Kennebec River.

text: The southwest end of Big Spencer Mountain drains into Kidney Brook, then into

text: Lobster Lake

text: , and into the

text: West Branch

text: of the

text: Penobscot River

text: , and into

text: Penobscot Bay

text: . The northeast end of Big Spencer Mountain drains into spring-fed Blood Pond where the pond's outlet, Maxfield Brook, then empties into Lobster Lake. Part of the southeast side of Big Spencer Mountain drains into Bear Brook, then into Ragged Lake, Ragged Stream,

text: Caribou Lake

text: Chesuncook Lake

text: Ripogenus Lake

text: , and into the West Branch Penobscot River. The southern part of the southeast side of Big Spencer drains into Lazy Tom Stream, thene into the

text: Roach River

text: , and

text: Moosehead Lake

text: , the source of the

text: Kennebec River

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text: List of New Jersey rivers includes streams formally designated as rivers.  There are also smaller streams (i.e., branches, creeks, drains, forks, licks, runs, etc.) in the state.  Major rivers include the Manasquan, Maurice, Mullica, Passaic, Rahway, Raritan, Musconetcong, Hudson and Delaware rivers.  Historically, the Delaware and Raritan rivers have provided transportation of goods and people inland from the Atlantic Ocean, and were once connected by the Delaware and Raritan Canal.  Today, these rivers, and the streams that feed them, provide sport and recreation for many people.

text: List of New Jersey rivers includes streams formally designated as

text: river

text: s.  There are also smaller streams (i.e., branches, creeks, drains, forks, licks, runs, etc.) in the state.  Major rivers include the

text: Manasquan

text: Maurice

text: Mullica

text: Passaic

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text: Musconetcong

text: Hudson

text: and

text: Delaware

text: rivers.  Historically, the Delaware and Raritan rivers have provided transportation of goods and people inland from the

text: Atlantic Ocean

text: , and were once connected by the

text: Delaware and Raritan Canal

text: .  Today, these rivers, and the streams that feed them, provide sport and recreation for many people.

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text: The audio stream is compressed to make the file size smaller using an

text: audio coding format

text: such as

text: Vorbis

text: AAC

text: or

text: Opus

text: . The video stream is compressed using a

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text: to make the file size smaller. Video coding formats include

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text: . Encoded audio and video streams are assembled in a container "

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text: . The bitstream is delivered from a streaming server to a streaming client (e.g., the computer user with their

text: Internet

text: -connected

text: laptop

text: ) using a transport protocol, such as Adobe's

text: RTMP

text: or

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text: . In the 2010s, technologies such as Apple's

text: HLS

text: , Microsoft's Smooth Streaming, Adobe's HDS and non-proprietary formats such as

text: MPEG-DASH

text: have emerged to enable

text: adaptive bitrate streaming

text: over

text: HTTP

text: as an alternative to using proprietary transport protocols. Often, a streaming transport protocol is used to send video from an event venue to a "

text: cloud

text: " transcoding service and CDN, which then uses HTTP-based transport protocols to distribute the video to individual homes and users. The streaming client (the end user) may interact with the streaming server using a control protocol, such as

text: MMS

text: or

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text: The main river in this area is the Cuencamé stream. All of the rivers in this area arrive to the Cuencamé stream. There are many small streams that in the rainy season are plenty of water. There is another stream near to San Pedro Ocuila and other named the “Arrieras”.In the recent years many of these streams have decreased substantially. The Cuencamé stream runs into the Nazas river in the point named Rancho de Fernández. In the 50's they were built two dams to keep the mountains water in the area. These dams have had helping to the agriculture needs in this north area.

text: The main river in this area is the Cuencamé stream. All of the rivers in this area arrive to the Cuencamé stream. There are many small streams that in the rainy season are plenty of water. There is another stream near to San Pedro Ocuila and other named the “Arrieras”.In the recent years many of these streams have decreased substantially. The Cuencamé stream runs into the

text: Nazas

text: river in the point named Rancho de Fernández. In the 50's they were built two dams to keep the mountains water in the area. These dams have had helping to the agriculture needs in this north area.

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answers: plenty of water

text: Divide is an unincorporated community in Frontier Rural Municipality No. 19, Saskatchewan, Canada. The community is located 35 km directly south of the community of Robsart and 85 km southwest of the town of Eastend on Highway 18. Very little remains in Divide. Only a church and post office still stand. Divide was the birthplace of hockey player Les Colwill.

text: Divide is an unincorporated community in

text: Frontier Rural Municipality No. 19

text: Saskatchewan

text: Canada

text: . The community is located 35 km directly south of the community of

text: Robsart

text: and 85 km southwest of the town of

text: Eastend

text: on

text: Highway 18

text: . Very little remains in Divide. Only a church and post office still stand. Divide was the birthplace of hockey player

text: Les Colwill

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answers: Divide

answers: NDQ_006063

answers: Rural Municipality

answers: NDQ_006064

answers: Divide

answers: NDQ_006065

answers: Very little

answers: NDQ_006066

answers: west side of the continental divide

answers: NDQ_006067

answers: It is impossible to say

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Saskatchewan

text: A wide variety of river and stream channel types exist in limnology, the study of inland waters. All these can be divided into two groups by using the water-flow gradient as either low gradient channels for streams or rivers with less than two percent (2%) flow gradient, or high gradient channels for those with greater than a 2% gradient.

text: A wide variety of

text: river

text: and

text: stream

text: channel types exist in

text: limnology

text: , the study of inland waters. All these can be divided into two groups by using the

text: water-flow gradient

text: as either low gradient channels for streams or rivers with less than two percent (2%) flow gradient, or high gradient channels for those with greater than a 2% gradient.

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answers: no

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answers: high gradient channels

answers: NDQ_006063

answers: two percent

answers: NDQ_006064

answers: high gradient

answers: NDQ_006065

answers: gradient

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: inland waters

answers: NDQ_006069

answers: low gradient channels

text: There are other tribes who are part of the Hupd'äh language family in the (Rio) Negro (black) river region. Each tribe has its own language and practically lives in the jungle, on the small streams. The Yohup people, for example, live on the streams on the right hand margin of the Tiquié river (Castanho, Samaúma, Cunuri and Ira streams), are fewer in number than the Hupda and barely have contact with them. The Kakwa people live on the streams on the left hand side of the Papuri River, in Colombia, and maintain sporadic contact with the Hupda who live on the streams flowing into the Papuri River. Still in Colombia, are the Nukak people on the Guaviri and Enírida rivers. The Dâw people, commonly known as the Kama, are the smallest tribe and are currently about 100 in number; they live around São Gabriel da Cachoeira although their traditional home is on the streams flowing into the Curicuriari River. Finally the Nadëb, in permanent contact with the merchants (regatões), live by extracting natural jungle products on the Jurubaxi and Uneuixi rivers that flow into the right hand side of the Rio Negro river.

text: There are other tribes who are part of the

text: Hupd'äh language family

text: in the (Rio) Negro (black) river region. Each tribe has its own language and practically lives in the jungle, on the small streams. The

text: Yohup

text: people, for example, live on the streams on the right hand margin of the Tiquié river (Castanho, Samaúma, Cunuri and Ira streams), are fewer in number than the Hupda and barely have contact with them. The

text: Kakwa people

text: live on the streams on the left hand side of the Papuri River, in

text: Colombia

text: , and maintain sporadic contact with the Hupda who live on the streams flowing into the Papuri River. Still in Colombia, are the

text: Nukak

text: people on the Guaviri and Enírida rivers. The

text: Dâw people

text: , commonly known as the Kama, are the smallest tribe and are currently about 100 in number; they live around

text: São Gabriel da Cachoeira

text: although their traditional home is on the streams flowing into the Curicuriari River. Finally the

text: Nadëb

text: , in permanent contact with the merchants (regatões), live by extracting natural jungle products on the Jurubaxi and Uneuixi rivers that flow into the right hand side of the Rio Negro river.

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answers: Rio Negro river

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Rio Negro river

answers: NDQ_006063

answers: language family

answers: NDQ_006064

answers: jungle

answers: NDQ_006065

answers: practically lives in the jungle

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answers: NDQ_006067

answers: (Rio Negro

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Papuri River

text: This is a list of streams and rivers in Vietnam:

text: This is a list of streams and rivers in

text: Vietnam

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answers: Fresh water streams do not flow into the ocean.

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answers: rivers were often built on rivers because they provided water

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answers: List of streams and rivers in Vietnam

text: The teams that finish in first place of the stream stage are promoted to the National First Division. They, then compete for an overall title with a substantial prize fund.

text: The teams that finish in first place of the stream stage are promoted to the National First Division. They, then compete for an overall title with a substantial prize fund.

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text: The name of the village means settlement on a stream from Lymn a Celtic word for stream or river.

text: The name of the village means settlement on a stream from Lymn a

text: Celtic

text: word for stream or river.

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text: There are extensive areas of farmland in the commune especially following the ridge line from north to south as well as steep mountain slopes. An extensive network of streams throughout the commune run into L'Escoutay river which runs south out of the commune then east to join the Rhone near Viviers. The western border of the commune is formed by the Ruisseau de Julieu. Le Rounei, and Le Ruisseau de Berg streams which flow into Le Salauzon stream which is part of the southern border of the commune before eventually joining L'Escoutay river.

text: There are extensive areas of farmland in the commune especially following the ridge line from north to south as well as steep mountain slopes. An extensive network of streams throughout the commune run into L'Escoutay river which runs south out of the commune then east to join the Rhone near Viviers. The western border of the commune is formed by the Ruisseau de Julieu. Le Rounei, and Le Ruisseau de Berg streams which flow into Le Salauzon stream which is part of the southern border of the commune before eventually joining L'Escoutay river.

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answers: rivers

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answers: The Rhone near Viviers

text: Obed River is a stream draining a part of the Cumberland Plateau in Tennessee.  It, and particularly its tributaries, are important streams for whitewater enthusiasts.

text: Obed River is a

text: stream

text: draining a part of the

text: Cumberland Plateau

text: in

text: Tennessee

text: .  It, and particularly its tributaries, are important streams for

text: whitewater

text: enthusiasts.

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answers: NDQ_006063

answers: Cumberland

answers: NDQ_006064

answers: Cumberland Plateau

answers: NDQ_006065

answers: important

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answers: the Pacific Ocean

answers: NDQ_006067

answers: Obed River

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: Obed River

text: River Falls lies on the banks of the Kinnickinnic River, a class one trout stream. The South Fork of the Kinnickinnic River runs through the city, dividing the campus of the University of Wisconsin-River Falls into two sections.

text: River Falls lies on the banks of the

text: Kinnickinnic River

text: , a class one trout stream. The South Fork of the Kinnickinnic River runs through the city, dividing the campus of the University of Wisconsin-River Falls into two sections.

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answers: NDQ_006064

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answers: NDQ_006065

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answers: Kinnickinnic River

text: In limnology (the study of inland waters), a stream bank or river bank is the terrain alongside the bed of a river, creek, or stream. The bank consists of the sides of the channel, between which the flow is confined. Stream banks are of particular interest in fluvial geography, which studies the processes associated with rivers and streams and the deposits and landforms created by them. The descriptive terms left bank and right bank are relative to an observer looking downstream, in which the right bank is to the observer's right; a famous example of this is the naming of the two sides of the river Seine in Paris. The shoreline of ponds, swamps, estuarys, reservoirs, or lakes are also of interest in limnology, and are sometimes referred to as banks. The grade of all these banks or shorelines can vary from vertical to a shallow slope.

text: In

text: limnology

text: (the study of inland waters), a stream bank or river bank is the terrain alongside the

text: bed

text: of a

text: river

text: , creek, or

text: stream

text: . The bank consists of the sides of the

text: channel

text: , between which the

text: flow

text: is confined. Stream banks are of particular interest in

text: fluvial

text: geography, which studies the processes associated with rivers and streams and the

text: deposits

text: and

text: landform

text: s created by them. The descriptive terms left bank and right bank are relative to an observer looking

text: downstream

text: , in which the right bank is to the observer's right; a famous example of this is the naming of the two sides of the river

text: Seine

text: in Paris. The

text: shore

text: line of

text: pond

text: s,

text: swamp

text: s,

text: estuary

text: s,

text: reservoir

text: s, or

text: lake

text: s are also of interest in limnology, and are sometimes referred to as banks. The

text: grade

text: of all these banks or shorelines can vary from vertical to a shallow slope.

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answers: NDQ_006069

answers: a stream bank or river bank

text: A third important stream is Bala Dhaka. This stream lies in Berg-Sham Mauza of the Barkhan Tehsil. The stream is a tributary of the Narechi River (Duki Tehsil). Water in this stream comes down from the south-western slopes of hills located north of the Han pass. The stream irrigates a very small area of Mauza Berg-Sham, and then its water passes in the Duki Tehsil.

text: A third important stream is Bala Dhaka. This stream lies in Berg-Sham Mauza of the Barkhan Tehsil. The stream is a tributary of the Narechi River (Duki Tehsil). Water in this stream comes down from the south-western slopes of hills located north of the Han pass. The stream irrigates a very small area of Mauza Berg-Sham, and then its water passes in the Duki Tehsil.

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answers: Duki Tehsil

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answers: Narechi River

answers: NDQ_006063

answers: Barkhan Tehsil

answers: NDQ_006064

answers: Mauza

answers: NDQ_006065

answers: very small

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answers: the pacific ocean

answers: NDQ_006067

answers: It does not say

answers: NDQ_006068

answers: irrigates

answers: NDQ_006069

answers: tributary of the Narechi River

text: A stream  from underground (a subterranean ocean of fresh water?) fertilises Eden before dividing into four rivers that go out to the entire earth (Genesis 2:5-6); in Ezekiel 47:1-12 (see Ezekiel's Temple) and other prophets the stream issues from the Temple itself, makes the desert bloom, and turns the Dead Sea from salt to fresh. Yet the underground waters are ambiguous: they are the source of life-giving rivers, but they are also associated with death (Jeremiah 2:6 and Job 38:16-17 describe how the way to Sheol is through water, and its gates are located at the foot of the mountain at the bottom of the seas).

text: A stream  from underground (a subterranean ocean of fresh water?) fertilises Eden before dividing into four rivers that go out to the entire earth (Genesis 2:5-6); in Ezekiel 47:1-12 (see

text: Ezekiel's Temple

text: ) and other prophets the stream issues from the Temple itself, makes the desert bloom, and turns the

text: Dead Sea

text: from salt to fresh. Yet the underground waters are ambiguous: they are the source of life-giving rivers, but they are also associated with death (Jeremiah 2:6 and Job 38:16-17 describe how the way to Sheol is through water, and its gates are located at the foot of the mountain at the bottom of the seas).

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text: Timothy Bigelow was born on 2 Aug 1739 in a part of Worcester known as Pakachoag or College Hill, located in Worcester County, Massachusetts, USA. son of Daniel Bigelow and Elizabeth Whitney. Timothy Bigelow's father was a farmer, the owner of 100 acres of land on "Little Packachoag Hill" . Timothy and his brothers grew up in the ways and manners of the times. Chores, assisting their father and in "off hours"  the boys enjoyed swimming and fishing in the summertime,ice-fishing in the winter, because a stream, called the French River, divided the northerly section of the farm.

text: Timothy Bigelow was born on 2 Aug 1739 in a part of Worcester known as Pakachoag or College Hill, located in Worcester County, Massachusetts, USA. son of Daniel Bigelow and Elizabeth Whitney. Timothy Bigelow's father was a farmer, the owner of 100 acres of land on "Little Packachoag Hill" . Timothy and his brothers grew up in the ways and manners of the times. Chores, assisting their father and in "off hours"  the boys enjoyed swimming and fishing in the summertime,ice-fishing in the winter, because a stream, called the French River, divided the northerly section of the farm.

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text: In 2004, he launched his separate music project called Divided. The project had two hits "The Music, the People" credited to Divided featuring Diablo in 2004, followed by "Easy Lover" in 2005, credited to Diablo presents Divided, a dance remake of the joint hit of Philip Bailey and Phil Collins in 1985, Divided remake coming after twenty years of the release of the original.

text: In 2004, he launched his separate music project called Divided. The project had two hits "The Music, the People" credited to Divided featuring Diablo in 2004, followed by "

text: Easy Lover

text: " in 2005, credited to Diablo presents Divided, a dance remake of the joint hit of

text: Philip Bailey

text: and

text: Phil Collins

text: in 1985, Divided remake coming after twenty years of the release of the original.

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text: Waitekuri River, Opitonui River, Owera Stream, Otanguru Stream, and Mapauriki Stream all drain the surrounding hills that are part of the Coromandel Range into the 12 km harbour, which only has a single narrow mouth to the sea. Tidal flows have built up a bar at the 600m wide entrance, which makes navigation difficult in large swells. The entrance is flanked by the rocky Te Rehutae Point, rising to 85m to the west, and Omara Spit to the east.

text: Waitekuri River

text: Opitonui River

text: , Owera Stream, Otanguru Stream, and Mapauriki Stream all drain the surrounding hills that are part of the

text: Coromandel Range

text: into the 12 km harbour, which only has a single narrow mouth to the sea. Tidal flows have built up a bar at the 600m wide entrance, which makes navigation difficult in large swells. The entrance is flanked by the rocky Te Rehutae Point, rising to 85m to the west, and Omara Spit to the east.

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text: A stream flowed north out of the pond and then west through a salt marsh (which, after being drained, became a meadow by the name of "Lispenard Meadows") to the Hudson River, while another stream issued from the southeastern part of the pond in an easterly direction to the East River.

text: A stream flowed north out of the pond and then west through a

text: salt marsh

text: (which, after being drained, became a

text: meadow

text: by the name of "Lispenard Meadows") to the

text: Hudson River

text: , while another stream issued from the southeastern part of the pond in an easterly direction to the

text: East River

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text: The nation streams are segmented into different colours, each colour indicating the reign of a particular ruler or a certain type of government. In some cases, prime ministers are shown in the lower half of nation streams and presidents in the upper half. Coloured scrolls and strips near the top of the chart stand for important people other than the rulers and other political leaders shown on the nation streams. These streams grow wider or thinner in accordance to historical context. Some streams divide to indicate a split in the nation (e.g. to indicate the independence of a state) or flow into others to illustrate its conquest, invasion, or acquisition by such other nation.

text: The nation streams are segmented into different colours, each colour indicating the reign of a particular ruler or a certain type of government. In some cases,

text: prime minister

text: s are shown in the lower half of nation streams and

text: president

text: s in the upper half. Coloured scrolls and strips near the top of the chart stand for important people other than the rulers and other political leaders shown on the nation streams. These streams grow wider or thinner in accordance to historical context. Some streams divide to indicate a split in the nation (e.g. to indicate the independence of a state) or flow into others to illustrate its conquest, invasion, or acquisition by such other nation.

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answers: Its conquest, invasion, or acquisition

text: A stream bed is the channel bottom of a stream, river or creek, the physical confine of the normal water flow.  The lateral confines or channel margins are known as the stream banks or river banks, during all but flood stage. In fact, a flood occurs when a stream overflows its banks and flows onto its flood plain. As a general rule, the bed is that part of the channel up to the normal water line, and the banks are that part above the normal water line. However, because water flow varies, this differentiation is subject to local interpretation. Usually, the bed is kept clear of terrestrial vegetation, whereas the banks are subjected to water flow only during unusual or perhaps infrequent high water stages and therefore might support vegetation some or much of the time.

text: A stream bed is the channel bottom of a

text: stream

text: river

text: or creek, the physical confine of the normal water flow.  The lateral confines or channel margins are known as the stream

text: bank

text: s or river banks, during all but

text: flood stage

text: . In fact, a

text: flood

text: occurs when a stream overflows its banks and flows onto its

text: flood plain

text: . As a general rule, the bed is that part of the

text: channel

text: up to the normal water line, and the banks are that part above the normal water line. However, because water flow varies, this differentiation is subject to local interpretation. Usually, the bed is kept clear of terrestrial

text: vegetation

text: , whereas the banks are subjected to water flow only during unusual or perhaps infrequent high water stages and therefore might support vegetation some or much of the time.

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answers: the banks are that part above the normal water line

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answers: It does not

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answers: this differentiation is subject to local interpretation

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answers: Usually, the bed is kept clear

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answers: river banks

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answers: The lateral confines or channel margins

text: A river is a natural watercourse, usually freshwater, flowing toward an ocean, a lake, a sea or another river. In a few cases, a river simply flows into the ground and dries up completely before reaching another body of water. Small rivers may also be termed by several other names, including stream, creek and brook. In the United States a river is generally classified as a watercourse more than 60 feet (18 metres) wide. The water in a river is usually in a channel, made up of a stream bed between banks. In larger rivers there is also a wider floodplain shaped by waters over-topping the channel. Flood plains may be very wide in relation to the size of the river channel. Rivers are a part of the hydrological cycle. Water within a river is generally collected from precipitation through surface runoff, groundwater recharge, springs, and the release of water stored in glaciers and snowpacks.

text: A river is a natural

text: watercourse

text: , usually

text: freshwater

text: , flowing toward an

text: ocean

text: , a

text: lake

text: , a

text: sea

text: or another river. In a few cases, a river simply flows into the ground and dries up completely before reaching another body of water. Small rivers may also be termed by several other names, including

text: stream

text: , creek and brook. In the

text: United States

text: a river is generally classified as a watercourse more than 60 feet (18 metres) wide. The water in a river is usually in a

text: channel

text: , made up of a

text: stream bed

text: between

text: banks

text: . In larger rivers there is also a wider

text: floodplain

text: shaped by waters over-topping the channel. Flood plains may be very wide in relation to the size of the river channel. Rivers are a part of the

text: hydrological cycle

text: . Water within a river is generally collected from

text: precipitation

text: through

text: surface runoff

text: groundwater recharge

text: springs

text: , and the release of water stored in

text: glacier

text: s and snowpacks.

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answers: NDQ_006061

answers: In a few cases

answers: NDQ_006062

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answers: NDQ_006063

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answers: NDQ_006064

answers: springs

answers: NDQ_006065

answers: larger floodplain shaped by waters over-topping the channel

answers: NDQ_006066

answers: The water in a river is usually in a channel

answers: NDQ_006067

answers: The water in a river is usually in a channel

answers: NDQ_006068

answers: a wider floodplain

answers: NDQ_006069

answers: In the United States a river is generally classified as a watercourse more than 60 feet (18 metres) wide

text: The Song River is a river in Dehradun district that drains the central and eastern part of the Doon Valley. A tributary of  Sooswa river, which in turn is a tributary of the Ganges, it originates as spring-fed stream in the southern slopes of the Mussoorie ridge of the Himalayan range and runs from Dhanaulti towards Narendra Nagar. As is common in hilly areas, there are several streams running south from the mountains that merge into one river that emerges from the hills a little after Shahastradhara.

text: The Song River is a river in

text: Dehradun district

text: that drains the central and eastern part of the

text: Doon Valley

text: . A tributary of  Sooswa river, which in turn is a tributary of the

text: Ganges

text: , it originates as spring-fed stream in the southern slopes of the

text: Mussoorie

text: ridge of the

text: Himalaya

text: n range and runs from

text: Dhanaulti

text: towards

text: Narendra Nagar

text: . As is common in hilly areas, there are several streams running south from the mountains that merge into one river that emerges from the hills a little after Shahastradhara.

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answers: rivers

answers: NDQ_006069

answers: Doon Valley

text: Rivers with headwaters on the mountain include: Shiyan Stream (), Baimang Stream () and Mashan Stream ().

text: Rivers with

text: headwaters

text: on the mountain include: Shiyan Stream (), Baimang Stream () and Mashan Stream ().

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answers: NDQ_006069

answers: Mashan Stream

text: On February 9, 2016, David Linker of HarperCollins acquired the worldwide publishing rights for the book from the Creative Artists Agency, which it plans to publish on October 4, 2016. HarperCollins also announced an original lullaby recording written and performed by Clarkson would accompany the book in its release. The book, released for sale on October 4, 2016, includes a link to a HarperCollins' website where the lullaby, appropriately titled "River Rose's Magical Lullaby", can be heard. The HarperCollins' website also directs the user to SoundCloud as a means to stream the recording. "River Rose's Magical Lullaby" was eventually released as a promotional single digital download to online music stores or available to stream through music streaming services.

text: On February 9, 2016, David Linker of

text: HarperCollins

text: acquired the worldwide publishing rights for the book from the

text: Creative Artists Agency

text: , which it plans to publish on October 4, 2016. HarperCollins also announced an original lullaby recording written and performed by Clarkson would accompany the book in its release. The book, released for sale on October 4, 2016, includes a link to a HarperCollins' website where the lullaby, appropriately titled "

text: River Rose's Magical Lullaby

text: ", can be heard. The HarperCollins' website also directs the user to

text: SoundCloud

text: as a means to

text: stream

text: the recording. "River Rose's Magical Lullaby" was eventually released as a

text: promotional single

text: digital download

text: to

text: online music stores

text: or available to stream through

entity_name: Comparison of on-demand streaming music services

text: music streaming service

text: s.

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answers: "River Rose's Magical Lullaby

text: Dry Creek is a stream in the U.S. state of Missouri. It is a tributary of the Flat River.

text: Dry Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the Flat River.

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answers: The continental divide divides the United States into the Pacific Ocean and the Atlantic Ocean

answers: NDQ_006067

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answers: Dry Creek

answers: NDQ_006069

answers: Dry Creek

text: The stream was part of the Northwest Trail, and led to the Savanna Portage, a historic trade route between the Great Lakes and the Mississippi River basin in central North America.  Members of the First Nations, and later fur traders, missionaries, and explorers, ascended the Saint Louis River from its mouth at Fond du Lac (in modern Duluth, Minnesota), then went up the East Savanna to the portage, crossed the portage and the divide to the West Savanna, and descended that stream to the Prairie River and Big Sandy Lake to the Mississippi.

text: The stream was part of the Northwest Trail, and led to the

text: Savanna Portage

text: , a historic trade route between the Great Lakes and the Mississippi River basin in central North America.  Members of the First Nations, and later fur traders, missionaries, and explorers, ascended the Saint Louis River from its mouth at

text: Fond du Lac

text: (in modern

text: Duluth, Minnesota

text: ), then went up the East Savanna to the portage, crossed the portage and the

text: divide

text: to the West Savanna, and descended that stream to the

text: Prairie River

text: and

text: Big Sandy Lake

text: to the Mississippi.

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answers: Mississippi River basin

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answers: Mississippi River basin

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answers: Savanna

text: The north side of Snow Mountain drains into Indian Stream, then into Chain of Ponds, the North Branch of the Dead River, Flagstaff Lake, the Dead River, the Kennebec River, and into the Gulf of Maine. The southeast side of Snow Mountain drains into Little Alder Stream, then into Alder Stream, and the North Branch of the Dead River. The north side of Snow Mountain drains into Big Island Pond, then into the Kennebago River, and the Androscoggin River, which drains into Merrymeeting Bay, the estuary of the Kennebec River.

text: The north side of Snow Mountain drains into Indian Stream, then into

text: Chain of Ponds

text: , the

text: North Branch

text: of the

text: Dead River

text: Flagstaff Lake

text: , the Dead River, the

text: Kennebec River

text: , and into the

text: Gulf of Maine

text: . The southeast side of Snow Mountain drains into Little Alder Stream, then into Alder Stream, and the North Branch of the Dead River. The north side of Snow Mountain drains into Big Island Pond, then into the

text: Kennebago River

text: , and the

text: Androscoggin River

text: , which drains into

text: Merrymeeting Bay

text: , the

text: estuary

text: of the Kennebec River.

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answers: NDQ_006064

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answers: the Kennebec River

answers: NDQ_006069

answers: the Kennebec River

text: Dapa is located on the east slope of the  West Andes above the Cauca River Valley. The elevation ranges from  in the foothills to  along the highest ridges.  The lower section is called Pilas de Dapa where the road crosses the Arroyohondo River and starts the climb up the mountain.  The main population lives above  which is divided up into several sections: Medio Dapa is located about halfway up the mountain and consists mainly of homes and farms.  Miravalle is the main center of population farther up the mountain and has a police station, school, and several businesses, along with many homes and a church further along the road. Rincón Dapa is farther up the mountain and is situated in a bowl that is shaped by several streams that come together to form the Arroyohondo River.  It is an area of large estates, farms, homes, a school, and scattered businesses like stores and restaurants.  Alto Dapa is located above Miravalle and is mainly an area of estates and farms.

text: Dapa is located on the east slope of the

text: West Andes

text: above the

text: Cauca River

text: Valley. The elevation ranges from  in the foothills to  along the highest ridges.  The lower section is called Pilas de Dapa where the road crosses the Arroyohondo River and starts the climb up the mountain.  The main population lives above  which is divided up into several sections: Medio Dapa is located about halfway up the mountain and consists mainly of homes and farms.  Miravalle is the main center of population farther up the mountain and has a police station, school, and several businesses, along with many homes and a church further along the road. Rincón Dapa is farther up the mountain and is situated in a bowl that is shaped by several streams that come together to form the Arroyohondo River.  It is an area of large estates, farms, homes, a school, and scattered businesses like stores and restaurants.  Alto Dapa is located above Miravalle and is mainly an area of estates and farms.

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answers: Rincón Dapa

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Cauca River Valley

answers: NDQ_006063

answers: Pilas de Dapa

answers: NDQ_006064

answers: River

answers: NDQ_006065

answers: Bowl that is shaped by several streams

answers: NDQ_006066

answers: the pacific ocean

answers: NDQ_006067

answers: Arroyohondo River

answers: NDQ_006068

answers: streams

answers: NDQ_006069

answers: Arroyohondo River

text: Formed by the confluence of a number of smaller streams draining the north eastern slopes of the Macedon Ranges and the southern slopes of the Cobaw range, both ranges being constituent parts of the Great Dividing Range, the Deep Creek rises north of Mount Macedon, near Cobaw. The river flows generally east in a broad shallow valley, to the north of , before turning generally southwards towards  to enter the deeper, narrower valley that characterises the remainder of the watercourse. The creek then flows east again before resuming its southward course at , towards , joined by several minor tributaries. The Deep Creek reaches its confluence with the Jackson Creek near Bulla and together they form the Maribyrnong River. The deep and relatively narrow valley cut by the creek in its southward course through the surrounding basalt plains is particularly prominent at such localities as Darraweit Guim,  and Bulla. The creek descends approximately  over its  course.

text: Formed by the

text: confluence

text: of a number of smaller streams draining the north eastern slopes of the

text: Macedon Ranges

text: and the southern slopes of the

text: Cobaw

text: range, both ranges being constituent parts of the

text: Great Dividing Range

text: , the Deep Creek rises north of

text: Mount Macedon

text: , near Cobaw. The river flows generally east in a broad shallow valley, to the north of , before turning generally southwards towards  to enter the deeper, narrower valley that characterises the remainder of the watercourse. The creek then flows east again before resuming its southward course at , towards , joined by several minor

text: tributaries

text: . The Deep Creek reaches its confluence with the

text: Jackson Creek

text: near Bulla and together they form the

text: Maribyrnong River

text: . The deep and relatively narrow valley cut by the creek in its southward course through the surrounding

text: basalt

text: plains is particularly prominent at such localities as Darraweit Guim,  and Bulla. The creek descends approximately  over its

text: course

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answers: NDQ_006069

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text: The Coppermill Stream is in the London Borough of Waltham Forest at Walthamstow in the Lea Valley. It is a minor tributary of the River Lea and approximately  long. The stream is part of a Site of Metropolitan Importance.

text: The Coppermill Stream is in the

text: London Borough of Waltham Forest

text: at

text: Walthamstow

text: in the

text: Lea Valley

text: . It is a minor tributary of the

text: River Lea

text: and approximately  long. The stream is part of a

text: Site of Metropolitan Importance

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answers: NDQ_006068

answers: Rivers

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answers: Lea Valley

text: Divided We See, like Divided We Sing, was an offshoot of a larger Divided We Stand project. About

text: Divided We See, like Divided We Sing, was an offshoot of a larger Divided We Stand project. About

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answers: Divided We Stand

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answers: Divided We See

answers: NDQ_006069

answers: Divided We Stand

text: There are over 1,100 lakes covering  and an estimated  of temporary and permanent streams and rivers in the forest. Over  of streams are found in the Fairfield District, over  in the Ketchum District, and over  in the Minidoka District. The entire northern portion of the forest is in the watershed of the Snake River, a tributary of the Columbia River. The Salmon River's headwaters are in the upper Sawtooth Valley, and this river drains much of the SNRA and follows a tortuous, overall northwesterly course before flowing into the Snake River  downstream. The eastern side of the Sawtooth Mountains is drained by the South Fork of the Payette River. The northern Soldier Mountains, southern Smoky Mountains, and much of the Fairfield District are drained by the South Fork of the Boise River, which flows into Anderson Ranch Reservoir just west of the forest. The Ketchum District, part of the SNRA, and the southern slopes of the Fairfield District are drained by the Big Wood River. Much of the Minidoka District is also drained by the Snake River via the Raft River and other tributaries, but portions of the Black Pine and Raft River Mountains drain into the Great Salt Lake. The annual water yield from the forest is estimated just below .

text: There are over 1,100 lakes covering  and an estimated  of temporary and permanent streams and rivers in the forest. Over  of streams are found in the Fairfield District, over  in the Ketchum District, and over  in the Minidoka District. The entire northern portion of the forest is in the watershed of the

text: Snake River

text: , a tributary of the

text: Columbia River

text: . The

text: Salmon River's

text: headwaters are in the upper Sawtooth Valley, and this river drains much of the SNRA and follows a tortuous, overall northwesterly course before flowing into the Snake River  downstream. The eastern side of the Sawtooth Mountains is drained by the South Fork of the

text: Payette River

text: . The northern Soldier Mountains, southern Smoky Mountains, and much of the Fairfield District are drained by the

text: South Fork of the Boise River

text: , which flows into

text: Anderson Ranch Reservoir

text: just west of the forest. The Ketchum District, part of the SNRA, and the southern slopes of the Fairfield District are drained by the

text: Big Wood River

text: . Much of the Minidoka District is also drained by the Snake River via the

text: Raft River

text: and other tributaries, but portions of the Black Pine and Raft River Mountains drain into the

text: Great Salt Lake

text: . The annual water yield from the forest is estimated just below .

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answers: NDQ_006061

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answers: NDQ_006063

answers: annual water yield

answers: NDQ_006064

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answers: estimated

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answers: NDQ_006067

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answers: the Columbia River

answers: NDQ_006069

answers: the Columbia River

text: Hawlings River is a  tributary of the Patuxent River in Montgomery County, Maryland. The watershed covers an area of about . The headwaters of the river originate in the area north of Laytonsville, and the river flows southeast, entering the Patuxent about  below the Triadelphia Reservoir. Portions of Hawlings River flow through Rachel Carson Conservation Park and Hawlings River Stream Valley Park. Tributaries of the Hawlings River include Mount Zion Tributary, Reddy Branch, Olney Mill Tributary, Gregg Tributary, and James Creek.  The river and its tributaries total about  of streams.

text: Hawlings River is a

text: tributary

text: of the

text: Patuxent River

text: in

text: Montgomery County

text: Maryland

text: . The

text: watershed

text: covers an area of about . The headwaters of the river originate in the area north of

text: Laytonsville

text: , and the river flows southeast, entering the Patuxent about  below the

text: Triadelphia Reservoir

text: . Portions of Hawlings River flow through

text: Rachel Carson Conservation Park

text: and Hawlings River Stream Valley Park. Tributaries of the Hawlings River include Mount Zion Tributary, Reddy Branch, Olney Mill Tributary, Gregg Tributary, and James Creek.  The river and its tributaries total about  of streams.

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answers: Hawlings River

text: In addition to many small unnamed streams, the Chowchilla River receives the water from the following streams:

text: In addition to many small unnamed streams, the Chowchilla River receives the water from the following streams:

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answers: unnamed streams

text: The stream received cleanup as part of the River Sweep of the Ohio River watershed in 2010.

text: The stream received cleanup as part of the

text: River Sweep

text: of the

text: Ohio River

text: watershed in 2010.

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answers: NDQ_006068

answers: The Ohio River watershed

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answers: River Sweep of the Ohio River watershed

text: The Silao River, crosses the major part of the municipal territory. It is fed by the Magueyes, Pascuales, Hondo, and Tigre streams, as well as the Gigante River, which is its major tributary. Within the municipality are some streams of importance, like those of the Agua Zarca, San Francisco, El Paraíso, Pabileros, and Aguas Buenas.

text: The Silao River, crosses the major part of the municipal territory. It is fed by the Magueyes, Pascuales, Hondo, and Tigre streams, as well as the Gigante River, which is its major tributary. Within the municipality are some streams of importance, like those of the Agua Zarca, San Francisco, El Paraíso, Pabileros, and Aguas Buenas.

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answers: NDQ_006064

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answers: NDQ_006067

answers: The Silao River

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The Silao River

text: The Moose River is an  long stream in northern New Hampshire in the United States.  It is a tributary of the Androscoggin River, which flows south and east into Maine, joining the Kennebec River near the Atlantic Ocean.

text: The Moose River is an  long stream in northern

text: New Hampshire

text: in the

text: United States

text: .  It is a tributary of the

text: Androscoggin River

text: , which flows south and east into

text: Maine

text: , joining the

text: Kennebec River

text: near the

text: Atlantic Ocean

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answers: NDQ_006063

answers: Atlantic Ocean

answers: NDQ_006064

answers: northern New Hampshire

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answers: NDQ_006067

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answers: NDQ_006068

answers: Moose River

answers: NDQ_006069

answers: Moose River

text: In addition to the streams which break through to the Pacific, a number of larger streams which drain to the Gulf of Mexico or the Caribbean Sea have their sources in the highlands. The Motagua River, whose principal head stream is called the Rio Grande, has a something and is navigable to within 90 miles of Guatemala City, which is situated on one of its confluents, the Rio de las Vacas. It empties in the Gulf of Honduras, an arm of the Carbean. Of similar importane is the Polochic River, whih is about 180 miles in length, and navigable about 20 miles above the river-port of Telemán. A vast number of streams, among which are the Chixoy, Lacantún, and Ixcán, unite to form the Usumacinta River, which passes along the Mexican frontier, and flowing on through Chiapas and Tabasco, falls into the Bay of Campeche. The Grijalva and its tributaries the Cuilco and San Miguel rivers drain west into the Chiapas Depression, and from there into the Gulf of Mexico. Lake Atitlan is a land-locked basin encompassed with lofty mountains. About 9 miles south of Guatemala City lies Lake Amatitlan with the town Amatitlán.

text: In addition to the streams which break through to the Pacific, a number of larger streams which drain to the Gulf of Mexico or the

text: Caribbean Sea

text: have their sources in the highlands. The

text: Motagua River

text: , whose principal head stream is called the Rio Grande, has a something and is navigable to within 90 miles of

text: Guatemala City

text: , which is situated on one of its confluents, the

text: Rio de las Vacas

text: . It empties in the

text: Gulf of Honduras

text: , an arm of the Carbean. Of similar importane is the

text: Polochic River

text: , whih is about 180 miles in length, and navigable about 20 miles above the river-port of Telemán. A vast number of streams, among which are the

text: Chixoy

text: Lacantún

text: , and

text: Ixcán

text: , unite to form the

text: Usumacinta River

text: , which passes along the Mexican frontier, and flowing on through

text: Chiapas

text: and

text: Tabasco

text: , falls into the

text: Bay of Campeche

text: . The

text: Grijalva

text: and its tributaries the

text: Cuilco

text: and

text: San Miguel

text: rivers drain west into the Chiapas Depression, and from there into the Gulf of Mexico.

text: Lake Atitlan

text: is a land-locked basin encompassed with lofty mountains. About 9 miles south of Guatemala City lies

text: Lake Amatitlan

text: with the town

text: Amatitlán

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answers: NDQ_006061

answers: No

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answers: Lake Atitlan

answers: NDQ_006063

answers: Pacific

answers: NDQ_006064

answers: sources

answers: NDQ_006065

answers: about 180 miles in length

answers: NDQ_006066

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answers: NDQ_006067

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answers: NDQ_006068

answers: the Motagua River

answers: NDQ_006069

answers: Lake Atitlan

text: Little Piney Creek is a stream in the U.S. state of Missouri. It is a tributary of the Gasconade River.

text: Little Piney Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the

text: Gasconade River

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answers: Little Piney Creek

answers: NDQ_006063

answers: U.S.

answers: NDQ_006064

answers: tributary

answers: NDQ_006065

answers: tributary

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: It is a stream

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: Little Piney Creek

text: The Noatak River is a stream in the northwestern part of the U.S. state of Alaska. T

text: The Noatak River is a stream in the northwestern part of the

text: U.S. state

text: of

text: Alaska

text: . T

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answers: Noatak River

answers: NDQ_006061

answers: Noatak River

answers: NDQ_006062

answers: Noatak River

answers: NDQ_006063

answers: U.S.

answers: NDQ_006064

answers: Noatak

answers: NDQ_006065

answers: t

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: Noatak River

answers: NDQ_006068

answers: The Noatak River

answers: NDQ_006069

answers: Noatak River

text: Peruque Creek is a stream in the U.S. state of Missouri. It is a tributary of the Mississippi River.

text: Peruque Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the

text: Mississippi River

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answers: Mississippi River

answers: NDQ_006067

answers: Mississippi River

answers: NDQ_006068

answers: Mississippi River

answers: NDQ_006069

answers: Peruque Creek

text: There are 2 possible scenarios when the path of a stream is blocked by an uplifted block of rock. First scenario: the stream poses stream power that is high enough to cut through the uplifted rocks, so that the river course will not be significantly altered. A channel is opened in the uplifted rocks due to erosion, a landform known as water gap. It continues to flow until the rock is further uplifted and the river no longer has enough erosive power to cut through it, leading to the second scenario. Second scenario: the stream does not have enough erosive power to cut through the rocks, so it deflected to flow along the boundary of the uplifted block as aforementioned. The abandoned river channel is known as wind gap. From here, the river either flows along the boundary of the fold and bends around the fold tip, or it may cut through the rocks at some points despite the block, due to either, acquisition of enough stream power through stream capture of small tributaries along its flow, or the presence of a particularly weak spot in the rock.  In either way the river continues to flow until further uplift of rocks makes the rock too difficult for the river to cut through, which results in, again, the deflection of the channel and formation of a new wind gap.

text: There are 2 possible scenarios when the path of a stream is blocked by an uplifted block of rock. First scenario: the stream poses stream power that is high enough to cut through the uplifted rocks, so that the river course will not be significantly altered. A channel is opened in the uplifted rocks due to erosion, a landform known as

text: water gap

text: . It continues to flow until the rock is further uplifted and the river no longer has enough erosive power to cut through it, leading to the second scenario. Second scenario: the stream does not have enough erosive power to cut through the rocks, so it deflected to flow along the boundary of the uplifted block as aforementioned. The abandoned river channel is known as

text: wind gap

text: . From here, the river either flows along the boundary of the fold and bends around the fold tip, or it may cut through the rocks at some points despite the block, due to either, acquisition of enough stream power through stream capture of small tributaries along its flow, or the presence of a particularly weak spot in the rock.  In either way the river continues to flow until further uplift of rocks makes the rock too difficult for the river to cut through, which results in, again, the deflection of the channel and formation of a new wind gap.

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answers: NDQ_006065

answers: erosive power

answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: no

answers: NDQ_006068

answers: river course will not be significantly altered

answers: NDQ_006069

answers: water gap

text: The Santa Anas include a number of high-mountain streams that flow for all or most of the year, although once out of the foothills these waterways are ephemeral. The major streams rising from the western side of the range drain into the Pacific Ocean; these include Peters Canyon Wash, Serrano Creek, San Diego Creek, Aliso Creek, Trabuco Creek, San Juan Creek, and San Mateo Creek. The northern side of the range is defined by the Santa Ana River, which heads about  further east, in the San Bernardino Mountains. Santiago Creek drains much of the northern part of the range and empties into the Santa Ana River near downtown Orange.

text: The Santa Anas include a number of high-mountain streams that flow for all or most of the year, although once out of the foothills these waterways are

text: ephemeral

text: . The major streams rising from the western side of the range drain into the Pacific Ocean; these include

text: Peters Canyon Wash

text: Serrano Creek

text: San Diego Creek

text: Aliso Creek

text: Trabuco Creek

text: San Juan Creek

text: , and

text: San Mateo Creek

text: . The northern side of the range is defined by the

text: Santa Ana River

text: , which heads about  further east, in the

text: San Bernardino Mountains

text: Santiago Creek

text: drains much of the northern part of the range and empties into the Santa Ana River near downtown

text: Orange

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answers: rivers

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answers: high-mountain streams

text: To qualify as a stream a hydrological feature must be either recurring or perennial.  Recurring (or "intermittent") streams have water in the channel for at least part of the year. The index of a stream or river may range from 1 (a stream with no tributaries) to 12 (globally the most powerful river, the Amazon, at its mouth).  The Ohio River is of order eight and the Mississippi River is of order 10.  Estimates are that 80% of the streams on the planet are first to third order headwater streams.

text: To qualify as a stream a hydrological feature must be either recurring or

text: perennial

text: .  Recurring (or "intermittent") streams have water in the channel for at least part of the year. The index of a stream or river may range from 1 (a stream with no tributaries) to 12 (globally the most powerful river, the

text: Amazon

text: , at its mouth).  The

text: Ohio River

text: is of order eight and the

text: Mississippi River

text: is of order 10.  Estimates are that 80% of the streams on the planet are first to third order

text: headwater stream

text: s.

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text: After leaving the River Lee Flood Relief Channel (Horsemill Stream) at Fishers Green the stream flows south to form the western boundary with the former Waltham Abbey Royal Gunpowder Mills before flowing through the Waltham Abbey SSSI within the Gunpowder Mills property. Above Waltham Abbey the stream diverges from the Old River Lea  with both channels bordering the Cornmill Stream and Old River Lea, SSSI. The stream passes under the 14th-century Harold's Bridge and the B194 road (Abbey View) before flowing through a sluice in the abbey's grounds. The stream flows underground to emerge adjacent to Waltham Abbey town hall. After flowing through an urban area, it rejoins the  River Lee Flood Relief Channel beyond the town of Waltham Abbey.

text: After leaving the

text: River Lee Flood Relief Channel

text: (Horsemill Stream) at

text: Fishers Green

text: the stream flows south to form the western boundary with the former

text: Waltham Abbey Royal Gunpowder Mills

text: before flowing through the

text: Waltham Abbey SSSI

text: within the Gunpowder Mills property. Above

text: Waltham Abbey

text: the stream diverges from the

text: Old River Lea

text: with both channels bordering the

text: Cornmill Stream and Old River Lea

text: SSSI

text: . The stream passes under the 14th-century Harold's Bridge and the

entity_name: B roads in Zone 1 of the Great Britain numbering scheme

text: B194 road

text: (Abbey View) before flowing through a sluice in the abbey's grounds. The stream flows underground to emerge adjacent to Waltham Abbey town hall. After flowing through an urban area, it rejoins the  River Lee Flood Relief Channel beyond the town of Waltham Abbey.

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answers: River Lee Flood Relief Channel

text: The creek's use as a tribal boundary is disputed. As other southern California Native Americans have done, a tribe typically claimed both sides of a stream or river—and used drainage divides as boundaries instead. However, the presence of Aliso Canyon, a steep and difficult-to-traverse gorge, suggests the opposite. Kroeber (1907) was the first to support this theory, and many other archaeologists have followed as well. The Juaneño disagree, arguing that their boundary stretches north to the northern drainage divide of the Aliso Creek watershed, which supports the practice of claiming both sides of a stream.

text: The creek's use as a tribal boundary is disputed. As other southern California Native Americans have done, a tribe typically claimed both sides of a stream or river—and used

text: drainage divide

text: s as boundaries instead. However, the presence of Aliso Canyon, a steep and difficult-to-traverse gorge, suggests the opposite. Kroeber (1907) was the first to support this theory, and many other archaeologists have followed as well. The Juaneño disagree, arguing that their boundary stretches north to the northern drainage divide of the Aliso Creek watershed, which supports the practice of claiming both sides of a stream.

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answers: drainage divides as boundaries

answers: NDQ_006069

answers: Aliso Creek watershed

text: In mid-November Call tried again. His forces made it across the Withlacoochee this time, but found the Cove abandoned. Call divided his forces, and proceeded up the river (south) on both sides. On November 17 Seminoles were routed from a large camp. There was another battle the next day, and the Seminoles were assumed to be headed for the Wahoo Swamp. Call waited to bring the other column across the river, then entered the Wahoo Swamp on November 21. The Seminoles resisted the advance in the Battle of Wahoo Swamp, as their families were close by, but had to retreat across a stream. Major David Moniac, a mix-blooded Creek who was the first Native American to graduate from West Point, tried to determine how deep the stream was, but was shot and killed by the Seminoles.

text: In mid-November Call tried again. His forces made it across the Withlacoochee this time, but found the Cove abandoned. Call divided his forces, and proceeded up the river (south) on both sides. On November 17 Seminoles were routed from a large camp. There was another battle the next day, and the Seminoles were assumed to be headed for the Wahoo Swamp. Call waited to bring the other column across the river, then entered the Wahoo Swamp on November 21. The Seminoles resisted the advance in the

text: Battle of Wahoo Swamp

text: , as their families were close by, but had to retreat across a stream. Major David Moniac, a mix-blooded Creek who was the first Native American to graduate from

text: West Point

text: , tried to determine how deep the stream was, but was shot and killed by the Seminoles.

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answers: a mix-blooded Creek

text: The stream leaves the main stream of the Thames at a river junction known as Four Rivers, at the south west corner of Fiddler's Island opposite Sheepwash Channel.  It immediately flows past Tumbling Bay, the site of a bathing place in use from 1853 to 1990. Osney Ditch flows out of Bulstake Stream southeast towards Osney. Bulstake Stream follows a semi-circular course, west and then south, passing under bridges on Binsey Lane and Botley Road (Bulstake Bridge) to a confluence with Seacourt Stream near North Hinksey. It then flows east past Osney Mead Industrial Estate, and rejoins the Thames at the Osney Rail Bridge. The Thames Path crosses the stream on a bridge known as Boney's Bridge. Botley Stream flows into Bulstake Stream from Seacourt Stream just north of Botley Road.

text: The stream leaves the main stream of the Thames at a river junction known as Four Rivers, at the south west corner of

text: Fiddler's Island

text: opposite

text: Sheepwash Channel

text: .  It immediately flows past Tumbling Bay, the site of a bathing place in use from 1853 to 1990.

text: Osney Ditch

text: flows out of Bulstake Stream southeast towards

text: Osney

text: . Bulstake Stream follows a semi-circular course, west and then south, passing under bridges on

text: Binsey Lane

text: and

text: Botley Road

text: Bulstake Bridge

text: ) to a confluence with

text: Seacourt Stream

text: near

text: North Hinksey

text: . It then flows east past

text: Osney Mead

text: Industrial Estate, and rejoins the Thames at the

text: Osney Rail Bridge

text: . The

text: Thames Path

text: crosses the stream on a bridge known as Boney's Bridge.

text: Botley Stream

text: flows into Bulstake Stream from Seacourt Stream just north of Botley Road.

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answers: NDQ_006064

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answers: NDQ_006065

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answers: NDQ_006066

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answers: NDQ_006067

answers: Seacourt Stream

answers: NDQ_006068

answers: river junction known as Four Rivers

answers: NDQ_006069

answers: Bulstake Stream

text: Walnut Creek is a stream in the U.S. state of Missouri. It is a tributary of the Little Sac River.

text: Walnut Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the Little Sac River.

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answers: NDQ_006061

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answers: Little Sac River

answers: NDQ_006063

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answers: NDQ_006064

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answers: NDQ_006065

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answers: the Pacific Ocean

answers: NDQ_006067

answers: salty ocean

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: Little Sac River

text: The surrounding area is largely agricultural, and river stages change dramatically due to agricultural runoff. It flows through a mostly wooded corridor and some river bottom farmland. The stream bed is composed mostly of sand with some glacial till, hard clay, and mud. Fallen trees and log jams are common. Pools and rivers may change drastically after heavy flooding. Large sandbars are not uncommon. There is some siltation and mild to extreme bank erosion in areas due to agriculture. There are very isolated occurrences of sandstone outcroppings along the stream bed and banks.

text: The surrounding area is largely agricultural, and river stages change dramatically due to

text: agricultural runoff

text: . It flows through a mostly wooded corridor and some river bottom farmland. The stream bed is composed mostly of sand with some

text: glacial till

text: , hard clay, and mud. Fallen trees and log jams are common. Pools and rivers may change drastically after heavy flooding. Large

text: sandbar

text: s are not uncommon. There is some

text: silt

text: ation and mild to extreme bank erosion in areas due to agriculture. There are very isolated occurrences of sandstone outcroppings along the stream bed and banks.

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answers: NDQ_006061

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answers: NDQ_006063

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answers: NDQ_006064

answers: river

answers: NDQ_006065

answers: mild to extreme

answers: NDQ_006066

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answers: NDQ_006067

answers: saltwater

answers: NDQ_006068

answers: agricultural runoff

answers: NDQ_006069

answers: the surrounding area is largely agricultural

text: The northern section of the Black Mountains are drained by the Cane River to the west and the South Toe River to the east, both of which are part of the upper Nolichucky River watershed.  The southwestern part of the range is drained by the upper French Broad River which, like the Nolichucky, is west of the Eastern Continental Divide and thus its waters eventually wind up in the Gulf of Mexico.  A few of the streams in the southeastern section of the range are part of the Catawba River watershed, and are thus east of the Eastern Continental Divide.

text: The northern section of the Black Mountains are drained by the

text: Cane River

text: to the west and the

text: South Toe River

text: to the east, both of which are part of the upper

text: Nolichucky River

text: watershed.  The southwestern part of the range is drained by the upper

text: French Broad River

text: which, like the Nolichucky, is west of the Eastern Continental Divide and thus its waters eventually wind up in the

text: Gulf of Mexico

text: .  A few of the streams in the southeastern section of the range are part of the

text: Catawba River

text: watershed, and are thus east of the Eastern Continental Divide.

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answers: NDQ_006061

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answers: Gulf of Mexico

answers: NDQ_006063

answers: Eastern Continental Divide

answers: NDQ_006064

answers: watershed

answers: NDQ_006065

answers: drained

answers: NDQ_006066

answers: Gulf of Mexico

answers: NDQ_006067

answers: Gulf of Mexico

answers: NDQ_006068

answers: River watershed

answers: NDQ_006069

answers: Catawba River watershed

text: Parent material transported by streams is called alluvium of which there are three main types. Floodplains are the parts of river valleys that are covered with water during floods. Due to their seasonal nature, floods create stratified layers in which larger particles tend to settle nearer the channel and smaller particles settle nearer the edges of the flooding area. Alluvial fans are sedimentary areas formed by narrow valley streams that suddenly drop to lowlands and widen dramatically. Sedimentary in these types of deposits tend to be larger closer to the uplands and finer near the edges of the fan. Delta deposits, the third of type of alluvium, are finer sediments that are discharged from streams into lakes and eventually settle near the mouth of the river.

text: Parent material transported by streams is called

text: alluvium

text: of which there are three main types.

text: Floodplain

text: s are the parts of river valleys that are covered with water during floods. Due to their seasonal nature, floods create stratified layers in which larger particles tend to settle nearer the channel and smaller particles settle nearer the edges of the flooding area. Alluvial fans are sedimentary areas formed by narrow valley streams that suddenly drop to lowlands and widen dramatically. Sedimentary in these types of deposits tend to be larger closer to the uplands and finer near the edges of the fan. Delta deposits, the third of type of alluvium, are finer sediments that are discharged from streams into lakes and eventually settle near the mouth of the river.

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answers: NDQ_006068

answers: alluvium

answers: NDQ_006069

answers: Alluvial fans

text: Stage School offers several streams of training which, depending on the age of the young people, can be conducted separately or concurrently.  Most streams have a hierarchical structure wherein students may be promoted to a more advanced group, based on the student's skill level and experience.

text: Stage School offers several streams of training which, depending on the age of the young people, can be conducted separately or concurrently.  Most streams have a hierarchical structure wherein students may be promoted to a more advanced group, based on the student's skill level and experience.

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answers: depending on the age

answers: NDQ_006066

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answers: NDQ_006067

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answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: stream

text: In a slow-flowing stream or river, the difference in speed between one bank and the other is not sufficient to provide a credible explanation as to why all the deposition occurs on one bank, and none on the other.  Similarly, the fallacy has no explanation as to why all the deposition occurs at a stream bend, and little or none occurs where the stream is following a straight course.  (The speed of water in a stream does not slow just because the stream enters a bend.)

text: In a slow-flowing stream or river, the difference in speed between one bank and the other is not sufficient to provide a credible explanation as to why all the deposition occurs on one bank, and none on the other.  Similarly, the fallacy has no explanation as to why all the deposition occurs at a stream bend, and little or none occurs where the stream is following a straight course.  (The speed of water in a stream does not slow just because the stream enters a bend.)

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answers: NDQ_006067

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answers: NDQ_006068

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answers: NDQ_006069

answers: speed of water in a stream

text: The intermediate interface between the two stages is made of a byte-aligned data stream of which there are two commands, a literal ("add") with length and data:

text: The intermediate interface between the two stages is made of a byte-aligned data stream of which there are two commands, a literal ("add") with length and data:

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answers: NDQ_006063

answers: byte

answers: NDQ_006064

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answers: a data stream

text: In hydrology, stage refers to the water level in a river or stream with respect to a chosen reference height. Stage is important because direct measurements of river discharge are very difficult while water surface elevation measurements are comparatively easy. In order to convert stage into discharge, scientists can use a combination of tracer studies, observations of high water marks, numerical modeling, and/or satellite or aerial photography. The relationship between stage and discharge is called a rating curve.

text: In

text: hydrology

text: , stage refers to the

text: water level

text: in a

text: river

text: or

text: stream

text: with respect to a chosen reference height. Stage is important because direct measurements of

text: river discharge

text: are very difficult while water surface elevation measurements are comparatively easy. In order to convert stage into discharge, scientists can use a combination of

text: tracer studies

text: , observations of

text: high water mark

text: s,

text: numerical model

text: ing, and/or

text: satellite

text: or

text: aerial photography

text: . The relationship between stage and discharge is called a

text: rating curve

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answers: Rivers

answers: NDQ_006069

answers: The relationship between stage and discharge is called a rating curve

text: Typically, streams are said to have a particular profile, beginning with steep gradients, no flood plain, and little shifting of channels, eventually evolving into streams with low gradients, wide flood plains, and extensive meanders. The initial stage is sometimes termed a "young" or "immature" stream, and the later state a "mature" or "old" stream.  However, a stream may meander for some distance before falling into a "young" stream condition.

text: Typically, streams are said to have a particular profile, beginning with steep gradients, no flood plain, and little shifting of channels, eventually evolving into streams with low gradients, wide flood plains, and extensive meanders. The initial stage is sometimes termed a "young" or "immature" stream, and the later state a "mature" or "old" stream.  However, a stream may meander for some distance before falling into a "young" stream condition.

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answers: NDQ_006068

answers: flood plains

answers: NDQ_006069

answers: low gradients, wide flood plains

text: These streams are very strong, especially during the rainy seasons spring, autumn, and at the end of winter, and cause erosion along the stream and river beds. The water in these streams is potable, especially at the beginning of their flows. The many rivers and streams contribute to sports and tourism in these regions.

text: These streams are very strong, especially during the rainy seasons spring, autumn, and at the end of winter, and cause erosion along the stream and river beds. The water in these streams is potable, especially at the beginning of their flows. The many rivers and streams contribute to sports and tourism in these regions.

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text: The range forms the main drainage divide between the Pacific and Atlantic river systems. On the Pacific side the distance to the sea is short, and the streams, while very numerous, are consequently small and rapid. A few of the streams of the Pacific slopes rise in the Guatemalan Highlands, and force a way through the Sierra Madre at the bottom of deep ravines. On the eastern side a number of the rivers of the Atlantic slopes attain a considerable volume and size.

text: The range forms the main

text: drainage divide

text: between the Pacific and Atlantic river systems. On the Pacific side the distance to the sea is short, and the streams, while very numerous, are consequently small and rapid. A few of the streams of the Pacific slopes rise in the

text: Guatemalan Highlands

text: , and force a way through the Sierra Madre at the bottom of deep ravines. On the eastern side a number of the rivers of the Atlantic slopes attain a considerable volume and size.

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answers: Atlantic

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answers: rivers

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answers: On the Pacific side the distance to the sea is short

text: The temporal lobes are very important in the visual system as well as in the production and comprehension of language. The left temporal lobe contains Wernicke's area and Broca's area, which are both important in the production and comprehension of language.The right temporal lobe is a part of the ventral stream in the visual pathway. The ventral stream is involved in object perception and visual recognition such as faces and objects, and is therefore often referred to in relation to the McGill Picture Anomaly test. The ventral stream is often referred to as the "what" stream and provides a portrayal of the objects in the receptive field that ultimately aids in identifying the importance of the object. The different functions of each lobe account for the "disturbance of non-language capacities" experienced after the removal of the right temporal lobe. If the ventral stream is disturbed or altered, the subject will not lose his vision but the ability to recognize "what" the object is in his receptive field. Disturbances in the ventral stream can be caused by damage or deterioration to any part of the brain involved in the ventral stream including the right temporal lobe.

text: The

text: temporal lobes

text: are very important in the visual system as well as in the production and comprehension of language. The left temporal lobe contains

text: Wernicke's area

text: and

text: Broca's area

text: , which are both important in the production and comprehension of language.The right temporal lobe is a part of the

text: ventral stream

text: in the visual pathway. The

text: ventral stream

text: is involved in object perception and visual recognition such as faces and objects, and is therefore often referred to in relation to the McGill Picture Anomaly test. The

text: ventral stream

text: is often referred to as the "what" stream and provides a portrayal of the objects in the

text: receptive field

text: that ultimately aids in identifying the importance of the object. The different functions of each lobe account for the "disturbance of non-language capacities" experienced after the removal of the right temporal lobe. If the

text: ventral stream

text: is disturbed or altered, the subject will not lose his vision but the ability to recognize "what" the object is in his

text: receptive field

text: . Disturbances in the

text: ventral stream

text: can be caused by damage or deterioration to any part of the brain involved in the

text: ventral stream

text: including the right

text: temporal lobe

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answers: The ventral stream

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answers: Disturbances in the ventral stream

answers: NDQ_006069

answers: left temporal lobe contains Wernicke's area and Broca's area

text: Floyd County is situated atop a high plateau of the Blue Ridge Mountains which divides the eastward flowing from the westward flowing waters. With the high topography, no streams flow into Floyd County. The county is drained primarily by Little River and its tributaries which flow into New River below the Claytor Lake Dam and, in turn, by way of the Kanawha River, the Ohio River and the Mississippi River, into the Gulf of Mexico.  The headwaters of the south fork of the Roanoke River are in the northeastern part of the county. No water flows into Floyd County - it all flows out - one particular fast stream is Shooting Creek. Named for its speed over rocks. This creek today follows Shooting Creek Road from Floyd into Franklin County. In later  years, it would become the site of moonshine liquor  distilleries and the lawlessness that surrounded this industry.

text: Floyd County is situated atop a high plateau of the Blue Ridge Mountains which divides the eastward flowing from the westward flowing waters. With the high topography, no streams flow into Floyd County. The county is drained primarily by

text: Little River

text: and its tributaries which flow into New River below the

text: Claytor Lake

text: Dam and, in turn, by way of the

text: Kanawha River

text: , the

text: Ohio River

text: and the

text: Mississippi River

text: , into the

text: Gulf of Mexico

text: .  The headwaters of the south fork of the

text: Roanoke River

text: are in the northeastern part of the county. No water flows into Floyd County - it all flows out - one particular fast stream is Shooting Creek. Named for its speed over rocks. This creek today follows Shooting Creek Road from Floyd into Franklin County. In later  years, it would become the site of moonshine liquor  distilleries and the lawlessness that surrounded this industry.

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answers: Shooting Creek

answers: NDQ_006061

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answers: the Mississippi River

answers: NDQ_006069

answers: high topography

text: The Atlas of Oregon ranks 31 rivers in the state by average streamflow; the top five are the Columbia, Snake, Willamette, Santiam, and Umpqua.  Not all Oregon rivers with high average flows are on this list of longest streams because neither their main stems nor any of their tributaries (including what are called "forks") are at least 50 miles (80 km) long. High-flow streams mentioned in the Atlas but not included in this long-stream list are the Metolius, Hood, Youngs, and Coos rivers. On the other hand, the list includes four low-flow intermittent streams—Dry River, Rattlesnake Creek, Rock Creek, and Dry Creek—that cross parts of the Oregon High Desert.

text: The Atlas of Oregon ranks 31 rivers in the state by average

text: streamflow

text: ; the top five are the Columbia, Snake,

text: Willamette

text: Santiam

text: , and

text: Umpqua

text: .  Not all Oregon rivers with high average flows are on this list of longest streams because neither their

text: main stem

text: s nor any of their

text: tributaries

text: (including what are called "forks") are at least 50 miles (80 km) long. High-flow streams mentioned in the Atlas but not included in this long-stream list are the

text: Metolius

text: Hood

text: Youngs

text: , and

text: Coos

text: rivers. On the other hand, the list includes four low-flow

text: intermittent streams

text: Dry River

text: Rattlesnake Creek

text: Rock Creek

text: , and

text: Dry Creek

text: —that cross parts of the

text: Oregon High Desert

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answers: NDQ_006065

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answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: It does not say

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answers: tributaries

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answers: the Oregon High Desert

text: Two streams, the Cuckoo Stream and the Turnapin Stream, pass through Dardistown; they later meet to form the Mayne River.

text: Two streams, the Cuckoo Stream and the Turnapin Stream, pass through Dardistown; they later meet to form the Mayne River.

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answers: NDQ_006064

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answers: NDQ_006065

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answers: NDQ_006067

answers: no

answers: NDQ_006068

answers: Streams

answers: NDQ_006069

answers: Cuckoo Stream

text: Ludlow Creek is a stream in the U.S. state of Ohio. The  long stream is a tributary of the Stillwater River.

text: Ludlow Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Ohio

text: . The  long stream is a tributary of the

text: Stillwater River

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answers: No

answers: NDQ_006062

answers: Stillwater River

answers: NDQ_006063

answers: Ohio

answers: NDQ_006064

answers: tributary

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answers: NDQ_006067

answers: salty ocean

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answers: NDQ_006069

answers: Ludlow Creek

text: This is a List of rivers in Alaska, which are at least fifth-order according to the Strahler method of stream classification, and an incomplete list of otherwise-notable rivers and streams.  Alaska has more than 12,000 rivers, and thousands more streams and creeks.  According to United States Geological Survey Geographic Names Information System, Alaska has about 9,728 officially named rivers, creeks, and streams.  The length of the river is given if it is available from the United States Geological Survey Geographic Names Information System (GNIS).

text: This is a List of rivers in Alaska, which are at least fifth-order according to the

text: Strahler

text: method of stream classification, and an incomplete list of otherwise-notable rivers and streams.

text: Alaska

text: has more than 12,000

text: river

text: s, and thousands more

text: stream

text: s and

text: creek

text: s.  According to

text: United States Geological Survey

text: Geographic Names Information System

text: , Alaska has about 9,728 officially named rivers, creeks, and streams.  The length of the

text: river

text: is given if it is available from the

text: United States Geological Survey

text: Geographic Names Information System

text: (GNIS).

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answers: List of rivers in Alaska

answers: NDQ_006063

answers: fifth-order

answers: NDQ_006064

answers: Alaska

answers: NDQ_006065

answers: at least fifth-order

answers: NDQ_006066

answers: Alaska has more than 12,000 rivers

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answers: salty ocean

answers: NDQ_006068

answers: rivers and streams

answers: NDQ_006069

answers: Alaska has more than 12,000 rivers, and thousands more streams and creeks

text: The municipality is watered by Verde and Sapucaí rivers (dammed in Furnas), belonging to Grand River Drainage. It also has the Araras and Espera streams, that are formed by the joining of several smaller streams. The Arara stream rises near the town and moves west to flow into the reservoir of Furnas. The Espera stream rises near the Três Pontas Mountain and flows into Furnas near a farm with the same name. Other streams that rises on the north of Três Pontas Mountain go north and flow into Rio Grande.

text: The municipality is watered by Verde and Sapucaí rivers (dammed in Furnas), belonging to Grand River Drainage. It also has the Araras and Espera streams, that are formed by the joining of several smaller streams. The Arara stream rises near the town and moves west to flow into the reservoir of Furnas. The Espera stream rises near the Três Pontas Mountain and flows into Furnas near a farm with the same name. Other streams that rises on the north of Três Pontas Mountain go north and flow into Rio Grande.

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answers: Grand River Drainage

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answers: Grand River Drainage

answers: NDQ_006063

answers: Rio Grande

answers: NDQ_006064

answers: Três Pontas

answers: NDQ_006065

answers: by the joining of several smaller streams

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: Rio Grande

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Grand River Drainage

text: Saddleback Junior stands within the watershed of the Kennebec River, which drains into the Gulf of Maine. The northeast and northwest sides of Saddleback Jr. drain into Redington Stream, then into the South Branch of the Dead River, and the Kennebec River. The east and south sides of Saddleback Jr. drain into Hardy Stream, then into Orbeton Stream, and the Sandy River, another tributary of the Kennebec.

text: Saddleback Junior stands within the

text: watershed

text: of the Kennebec River, which drains into the

text: Gulf of Maine

text: . The northeast and northwest sides of Saddleback Jr. drain into Redington Stream, then into the

text: South Branch

text: of the

text: Dead River

text: , and the Kennebec River. The east and south sides of Saddleback Jr. drain into Hardy Stream, then into Orbeton Stream, and the

text: Sandy River

text: , another

text: tributary

text: of the Kennebec.

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answers: NDQ_006064

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answers: NDQ_006067

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answers: NDQ_006068

answers: Rivers

answers: NDQ_006069

answers: Kennebec River

text: Coburn Mtn. lies within the watershed of the Kennebec River. The northern end of the southeast side of Coburn drains into Mountain Brook, then into Cold Stream and the Kennebec River. The southern end drains into Salmon Stream, then into the Dead River, another tributary of the Kennebec River. The southwest end of Coburn drains into Enchanted Pond and Enchanted Stream, then into the Dead River. The northwest side of Coburn drains into Horse Brook and Fourmile Brook, then into the Moose River and the Kennebec. The north end of Coburn drains into Piel Brook, then into Parlin Stream and the Moose River.

text: Coburn Mtn. lies within the

text: watershed

text: of the

text: Kennebec River

text: . The northern end of the southeast side of Coburn drains into Mountain Brook, then into Cold Stream and the Kennebec River. The southern end drains into Salmon Stream, then into the

text: Dead River

text: , another

text: tributary

text: of the Kennebec River. The southwest end of Coburn drains into

text: Enchanted Pond

text: and Enchanted Stream, then into the Dead River. The northwest side of Coburn drains into Horse Brook and Fourmile Brook, then into the

text: Moose River

text: and the Kennebec. The north end of Coburn drains into Piel Brook, then into Parlin Stream and the Moose River.

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answers: NDQ_006061

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answers: NDQ_006062

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answers: NDQ_006063

answers: Kennebec River

answers: NDQ_006064

answers: Watershed

answers: NDQ_006065

answers: watershed

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: Dead River

answers: NDQ_006068

answers: the Kennebec

answers: NDQ_006069

answers: Coburn Mtn

text: Spring Hollow Creek is a stream in the U.S. state of Missouri. It is a tributary of the Niangua River.

text: Spring Hollow Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the Niangua River.

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answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Niangua River

answers: NDQ_006063

answers: U.S.

answers: NDQ_006064

answers: Spring Hollow Creek

answers: NDQ_006065

answers: tributary

answers: NDQ_006066

answers: Spring Hollow Creek is a stream

answers: NDQ_006067

answers: Niangua River

answers: NDQ_006068

answers: rivers provided water

answers: NDQ_006069

answers: Spring Hollow Creek

text: Before the pre-output function can begin to output its pre-output stream it has to be clocked 256 times to warm up, during this stage the pre-output stream is fed into the feedback polynomials

text: Before the pre-output function can begin to output its pre-output stream it has to be clocked 256 times to warm up, during this stage the pre-output stream is fed into the feedback polynomials

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answers: NDQ_006061

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answers: NDQ_006062

answers: Pacific Ocean

answers: NDQ_006063

answers: pre-output

answers: NDQ_006064

answers: Pre-output function

answers: NDQ_006065

answers: 256 times to warm up

answers: NDQ_006066

answers: warm up

answers: NDQ_006067

answers: pre-output function

answers: NDQ_006068

answers: feedback polynomials

answers: NDQ_006069

answers: feedback polynomials

text: The Coldwater River is a  stream in the U.S. state of Michigan. Located in western Michigan, the river is a part of the Grand River drainage basin.

text: The Coldwater River is a

text: stream

text: in the

text: U.S. state

text: of

text: Michigan

text: . Located in

text: western Michigan

text: , the river is a part of the

text: Grand River

text: drainage basin.

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answers: NDQ_006066

answers: Atlantic Ocean

answers: NDQ_006067

answers: The Coldwater River

answers: NDQ_006068

answers: river drainage basin

answers: NDQ_006069

answers: Grand River drainage basin

text: They are typically found in warmer parts of streams and rivers in the drainages of the Columbia River, Fraser River, and the Harney-Malheur system of the Great Basin. Some are found in lakes, migrating into streams to spawn. Although abundant in many parts of their range, behavior remains little-known. Chiselmouth were among the fishes typically utilized by the Nez Perce people as food.

text: They are typically found in warmer parts of streams and rivers in the drainages of the

text: Columbia River

text: Fraser River

text: , and the

text: Harney-Malheur

text: system of the

text: Great Basin

text: . Some are found in lakes, migrating into streams to spawn. Although abundant in many parts of their range, behavior remains little-known. Chiselmouth were among the fishes typically utilized by the

text: Nez Perce people

text: as food.

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answers: NDQ_006063

answers: streams and rivers

answers: NDQ_006064

answers: Great Basin

answers: NDQ_006065

answers: little-known

answers: NDQ_006066

answers: Columbia River

answers: NDQ_006067

answers: Chiselmouth

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Chiselmouth

text: The second stage is that of the  (Sanskrit: ), literally meaning "one who once () comes ()". The once-returner will at most return to the realm of the senses (the lowest being human and the highest being the devas wielding power over the creations of others) one more time. Both the stream-enterer and the once-returner have abandoned the first three fetters. The stream-enterer and once-returner are distinguished by the fact that the once-returner has weakened lust, hate, and delusion to a greater degree. The once-returner therefore has fewer than seven rebirths. Once-returners do not have only one more rebirth, as the name suggests, for that may not even be said with certainty about the non-returner who can take multiple rebirths in the five "Pure Abodes". They do, however, only have one more rebirth in the realm of the senses, excluding, of course, the planes of hell, animals and hungry ghosts.

text: The second stage is that of the  (Sanskrit: ), literally meaning "one who once () comes ()". The once-returner will at most return to the realm of the senses (the lowest being human and the highest being the devas wielding power over the creations of others) one more time. Both the stream-enterer and the once-returner have abandoned the first three fetters. The stream-enterer and once-returner are distinguished by the fact that the once-returner has weakened lust, hate, and delusion to a greater degree. The once-returner therefore has fewer than seven rebirths. Once-returners do not have only one more rebirth, as the name suggests, for that may not even be said with certainty about the non-returner who can take multiple rebirths in the five "Pure Abodes". They do, however, only have one more rebirth in the realm of the senses, excluding, of course, the planes of hell, animals and hungry ghosts.

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answers: The second stage

answers: NDQ_006061

answers: It does not

answers: NDQ_006062

answers: The stream-enterer

answers: NDQ_006063

answers: human

answers: NDQ_006064

answers: Pure Abodes

answers: NDQ_006065

answers: a greater degree

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: None

answers: NDQ_006068

answers: The once-returner

answers: NDQ_006069

answers: The once-returner

text: The Piako River has two major stems: the first, and main, stem drains the northern Te Miro-Tahuroa hills, and the Pakaroa Range. The dominant tributaries on the eastern slopes of these hills are the Piakonui and Piakoiti Streams. These streams, together with the smaller Toenepi Stream, converge just south of Kereone to become the Piako River. The western slopes are drained by the Waitakaruru Stream which joins the Piako River at Morrinsville. As the Piako River progresses north, it is fed by numerous small streams draining the eastern slopes of the Hangawera Hills.

text: The Piako River has two major stems: the first, and main, stem drains the northern Te Miro-Tahuroa hills, and the Pakaroa Range. The dominant tributaries on the eastern slopes of these hills are the Piakonui and Piakoiti Streams. These streams, together with the smaller Toenepi Stream, converge just south of Kereone to become the Piako River. The western slopes are drained by the

text: Waitakaruru Stream

text: which joins the Piako River at

text: Morrinsville

text: . As the Piako River progresses north, it is fed by numerous small streams draining the eastern slopes of the Hangawera Hills.

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answers: 3

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answers: 4

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answers: 4

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answers: NDQ_006067

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answers: NDQ_006068

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answers: NDQ_006069

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answers: NDQ_006060

answers: Piako River

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Piako River

answers: NDQ_006063

answers: Toenepi Stream

answers: NDQ_006064

answers: slope

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answers: NDQ_006066

answers: Pacific Ocean

answers: NDQ_006067

answers: The Piako River

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Te Miro-Tahuroa hills

text: The Pend Oreille River watershed divide is formed on the east side by the Continental Divide. On the south, the Spokane River and Snake River drainage basins border on the Clark Fork. To the west smaller rivers such as the Colville River and tributaries of the Spokane drain the lands past the watershed divide. In the north is the Kootenay River, a similar-sized tributary of the Columbia. To the east, in Montana, is the Missouri River and tributaries such as the Marias River and Milk River. In the southwest the watershed borders on the Big Hole River and Jefferson River, headwater streams of the Missouri. The Pend Oreille/Clark Fork system is notable in that it cuts right between the Bitterroot Range and Selkirk Range, two major chains of the Rocky Mountains. The only other river to do so is the Kootenay, just to the north. The Rocky Mountain Trench runs across the northeast part of the watershed, through the Flathead Valley, and eventually terminating in mountains near the Clark Fork's confluence with the Flathead.

text: The Pend Oreille River watershed divide is formed on the east side by the

text: Continental Divide

text: . On the south, the

text: Spokane River

text: and Snake River drainage basins border on the Clark Fork. To the west smaller rivers such as the

text: Colville River

text: and tributaries of the Spokane drain the lands past the watershed divide. In the north is the Kootenay River, a similar-sized tributary of the Columbia. To the east, in Montana, is the

text: Missouri River

text: and tributaries such as the

text: Marias River

text: and

text: Milk River

text: . In the southwest the watershed borders on the

text: Big Hole River

text: and

text: Jefferson River

text: , headwater streams of the Missouri. The Pend Oreille/Clark Fork system is notable in that it cuts right between the

text: Bitterroot Range

text: and

text: Selkirk Range

text: , two major chains of the

text: Rocky Mountains

text: . The only other river to do so is the Kootenay, just to the north. The

text: Rocky Mountain Trench

text: runs across the northeast part of the watershed, through the Flathead Valley, and eventually terminating in mountains near the Clark Fork's confluence with the Flathead.

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answers: Clark Fork

answers: NDQ_006061

answers: No

answers: NDQ_006062

answers: Rocky Mountain Trench

answers: NDQ_006063

answers: Continental Divide

answers: NDQ_006064

answers: headwater

answers: NDQ_006065

answers: watershed

answers: NDQ_006066

answers: the Atlantic Ocean

answers: NDQ_006067

answers: The Rocky Mountain Trench

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: Kootenay River

text: The northwest side of Saddleback drains into Saddleback Lake, then into Redington Stream, the South Branch of the Dead River, the Kennebec River, and into the Gulf of Maine. The southeast side of Saddleback drains into Winship and Conant Streams, then Orbeton Stream, and the Sandy River, another tributary of the Kennebec. The southwest end of Saddleback drains into Cascade Stream, then into Rangeley Lake, Rangeley River, Mooselookmeguntic Lake, Upper and Lower Richardson Lakes, Rapid River, Umbagog Lake, and the Androscoggin River, which drains into Merrymeeting Bay, the estuary of the Kennebec River.

text: The northwest side of Saddleback drains into Saddleback Lake, then into Redington Stream, the

text: South Branch

text: of the

text: Dead River

text: , the

text: Kennebec River

text: , and into the

text: Gulf of Maine

text: . The southeast side of Saddleback drains into Winship and Conant Streams, then Orbeton Stream, and the

text: Sandy River

text: , another

text: tributary

text: of the Kennebec. The southwest end of Saddleback drains into Cascade Stream, then into

text: Rangeley Lake

text: Rangeley River

text: Mooselookmeguntic Lake

text: Upper

text: and

text: Lower Richardson Lake

text: s,

text: Rapid River

text: Umbagog Lake

text: , and the

text: Androscoggin River

text: , which drains into

text: Merrymeeting Bay

text: , the

text: estuary

text: of the Kennebec River.

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answers: Merrymeeting Bay

answers: NDQ_006061

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answers: Merrymeeting Bay

answers: NDQ_006063

answers: Saddleback Lake

answers: NDQ_006064

answers: tributary

answers: NDQ_006065

answers: depends on the terrain

answers: NDQ_006066

answers: Gulf of Maine

answers: NDQ_006067

answers: Gulf of Maine

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: the Kennebec River

text: The north part of the island sits between the River Thames and the top end of Castle Mill Stream, a Thames backwater. Fiddler's Island Stream flows to the east of the southern part of the island. To the south of the island, there is a short stretch of water known as the Sheepwash Channel linking back to the Castle Mill Stream and the Oxford Canal. The Thames Path runs the length of the complete island.  At the northern end, the island has a row of trees along it. On the Castle Mill Stream side there is extensive mooring. The rainbow-shaped Medley Footbridge crosses the main stream of the Thames to the west at the northern end and a flat iron Bailey bridge crosses Castle Mill Stream further south, linking it to Port Meadow to the east.  A small footbridge takes the Thames Path along the bank towards Osney Bridge. The northern part of Fiddler's Island is very thin. The southern part, connected by a footbridge, is wider. To the east is Cripley Meadow, largely consisting of allotments.

text: The north part of the island sits between the River Thames and the top end of

text: Castle Mill Stream

text: , a Thames backwater. Fiddler's Island Stream flows to the east of the southern part of the island. To the south of the island, there is a short stretch of water known as the

text: Sheepwash Channel

text: linking back to the Castle Mill Stream and the

text: Oxford Canal

text: . The

text: Thames Path

text: runs the length of the complete island.  At the northern end, the island has a row of trees along it. On the Castle Mill Stream side there is extensive mooring. The rainbow-shaped

text: Medley Footbridge

text: crosses the main stream of the Thames to the west at the northern end and a flat iron

text: Bailey bridge

text: crosses Castle Mill Stream further south, linking it to

text: Port Meadow

text: to the east.  A small footbridge takes the Thames Path along the bank towards

text: Osney Bridge

text: . The northern part of Fiddler's Island is very thin. The southern part, connected by a footbridge, is wider. To the east is

text: Cripley Meadow

text: , largely consisting of

text: allotments

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answers: Sheepwash Channel

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Fiddler's Island

answers: NDQ_006063

answers: River Thames

answers: NDQ_006064

answers: backwater

answers: NDQ_006065

answers: extensive mooring

answers: NDQ_006066

answers: west side of the continental divide

answers: NDQ_006067

answers: Sheepwash Channel

answers: NDQ_006068

answers: River Thames

answers: NDQ_006069

answers: Fiddler's Island Stream

text: Turkey Creek is a stream in the U.S. state of Missouri. It is a tributary of the Little Sac River.

text: Turkey Creek is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the Little Sac River.

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answers: NDQ_006063

answers: Little Sac River

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answers: Atlantic Ocean

answers: NDQ_006067

answers: Salty ocean

answers: NDQ_006068

answers: the Little Sac River

answers: NDQ_006069

answers: Little Sac River

text: Early tributaries include the Athdown Brook, Shankill River, Ballylow Brook, Brittas River and Woodend Brook, as well as the substantial King's River.Downstream of Poulaphouca are the Lemonstown Stream, Kilcullen Stream and Pinkeen Stream, followed by the Painestown River (with tributaries including the Morell River), Rye Water (with tributaries including the Lyreen), and the Griffeen River.

text: Early tributaries include the Athdown Brook, Shankill River, Ballylow Brook, Brittas River and Woodend Brook, as well as the substantial King's River.Downstream of Poulaphouca are the Lemonstown Stream, Kilcullen Stream and Pinkeen Stream, followed by the

text: Painestown River

text: (with tributaries including the

text: Morell River

text: ), Rye Water (with tributaries including the Lyreen), and the Griffeen River.

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answers: Poulaphouca

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answers: no

answers: NDQ_006062

answers: Poulaphouca

answers: NDQ_006063

answers: King's River

answers: NDQ_006064

answers: tributary

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answers: substantial

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: tributaries

answers: NDQ_006068

answers: tributaries

answers: NDQ_006069

answers: tributaries

text: The major rivers in the region include the French Broad River, Nolichucky River, Watauga River, Little Tennessee River, and Hiwassee River flowing into the Tennessee River valley; the New River flowing into the Ohio River valley; and the headwaters and upper valleys of the Catawba River, Yadkin River, Broad River, and Saluda River flowing through the foothills towards the Atlantic.  The Eastern Continental Divide runs through the region, dividing Tennessee-bound streams from those flowing through the Carolinas.

text: The major rivers in the region include the

text: French Broad River

text: Nolichucky River

text: Watauga River

text: Little Tennessee River

text: , and

text: Hiwassee River

text: flowing into the Tennessee River valley; the

text: New River

text: flowing into the Ohio River valley; and the headwaters and upper valleys of the

text: Catawba River

text: Yadkin River

text: Broad River

text: , and

text: Saluda River

text: flowing through the foothills towards the Atlantic.  The

text: Eastern Continental Divide

text: runs through the region, dividing

text: Tennessee

text: -bound

text: stream

text: s from those flowing through the

text: Carolinas

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answers: The Eastern Continental Divide

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Atlantic

answers: NDQ_006063

answers: Tennessee

answers: NDQ_006064

answers: headwaters

answers: NDQ_006065

answers: flowing into the Tennessee River valley

answers: NDQ_006066

answers: Atlantic

answers: NDQ_006067

answers: Atlantic

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The Eastern Continental Divide

text: Low gradient channels of rivers and streams can be divided into braided rivers, wandering rivers, single thread sinuous rivers (meandering), and anastomosing rivers. The channel type developed depends on stream gradient, riparian vegetation and sediment supply. Braided rivers tend to occur on steeper gradients where there is a large supply of sediment for braid bars, while single thread sinous channels occur where there is a lower sediment supply for point bars. Anastomosing channels are multithreaded, but are much more stable than braided channels and commonly have thick clay and silt banks and occur at lower gradients of stream bed. Wandering rivers fall between sinuous single thread and braided streams and are relatively stable multi-channel gravel bed rivers.

text: Low gradient channels of rivers and streams can be divided into

text: braided river

text: s, wandering rivers, single thread

text: sinuous

text: rivers (meandering), and

text: anastomosing

text: rivers. The channel type developed depends on stream gradient,

text: riparian

text: vegetation and sediment supply.

text: Braided river

text: s tend to occur on steeper gradients where there is a large supply of sediment for

text: braid bar

text: s, while single thread sinous channels occur where there is a lower sediment supply for

text: point bar

text: s. Anastomosing channels are multithreaded, but are much more stable than braided channels and commonly have thick clay and silt

text: bank

text: s and occur at lower gradients of

text: stream bed

text: . Wandering rivers fall between sinuous single thread and braided streams and are relatively stable multi-channel gravel bed rivers.

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answers: 0

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answers: The channel type developed depends on stream gradient, riparian vegetation and sediment supply

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answers: 0

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answers: 1

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answers: 4

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answers: 0

answers: NDQ_006069

answers: 0

answers: NDQ_006060

answers: Wandering rivers

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: anastomosing rivers

answers: NDQ_006063

answers: Low gradient

answers: NDQ_006064

answers: riparian

answers: NDQ_006065

answers: depends on stream gradient

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: no

answers: NDQ_006068

answers: sediment supply

answers: NDQ_006069

answers: Low gradient channels of rivers and streams

text: The Groot Letaba River headwater streams originate in the Drakensberg Escarpment, descending in long runs with an occasional riffle or pool, mostly in the Limpopo province of South Africa. At the higher level the Broederstroom River, Politsi River, Debengeni River, Letsitele River, and Thabina River, join the Groot Letaba. Lower down the Molototsi River (a seasonal stream) and Nsama River join before the Nsami Dam. Just before the Kruger National Park the Klein Letaba River flows into the river. From here the combined rivers are simply known as the Letaba River.

text: The Groot Letaba River headwater streams originate in the Drakensberg Escarpment, descending in long runs with an occasional riffle or pool, mostly in the

text: Limpopo

text: province of

text: South Africa

text: . At the higher level the

text: Broederstroom River

text: Politsi River

text: Debengeni River

text: Letsitele River

text: , and

text: Thabina River

text: , join the Groot Letaba. Lower down the

text: Molototsi River

text: (a seasonal stream) and

text: Nsama River

text: join before the

text: Nsami Dam

text: . Just before the

text: Kruger National Park

text: the

text: Klein Letaba River

text: flows into the river. From here the combined rivers are simply known as the

text: Letaba River

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answers: Drakensberg

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answers: Drakensberg Escarpment

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answers: It does not say

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answers: Rivers

answers: NDQ_006069

answers: Drakensberg Escarpment

text: The Catoosa WMA lies within the Emory River drainage, which is divided by a number of major stream drainages, including the Obed River, Daddy's Creek, Clear Creek, and Otter Creek. The Emory River meets the Obed River in the southeast corner of the area. The terrain is moderately rolling, ranging in elevation from  to , with deep canyons cut by the streams.

text: The Catoosa WMA lies within the

text: Emory River

text: drainage, which is divided by a number of major stream drainages, including the

text: Obed River

text: Daddy's Creek

text: Clear Creek

text: , and

text: Otter Creek

text: . The Emory River meets the Obed River in the southeast corner of the area. The terrain is moderately rolling, ranging in elevation from  to , with deep canyons cut by the streams.

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answers: The Emory River drainage

text: Faulbach is a river of Bavaria, Germany. The name of this  long stream is from the vûl for lazy or foul, and Bach, stream. The Faulbach is a tributary of the Main River.

text: Faulbach is a river of

text: Bavaria

text: Germany

text: . The name of this  long stream is from the vûl for lazy or foul, and Bach, stream. The Faulbach is a tributary of the

text: Main River

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answers: long

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answers: It is not possible to tell

answers: NDQ_006068

answers: rivers provided water, plus

answers: NDQ_006069

answers: Faulbach

text: Starting about 1865, the river was used for massive logging drives from Third Connecticut Lake to initially water powered sawmills near Enfield Falls. Trees cut adjacent to tributary streams including Perry Stream and Indian Stream in Pittsburg, New Hampshire, Halls Stream on the Quebec–New Hampshire border, Simms Stream, the Mohawk River, and the Nulhegan River basin in Essex County, Vermont, would be flushed into the main river by the release of water impounded behind splash dams. Several log drivers died trying to move logs through Perry Falls in Pittsburg. Teams of men would wait at Canaan, Vermont, to protect the bridges from log jams. Men guided logs through a  drop along the length of Fifteen-Mile Falls (now submerged under Moore and Comerford reservoirs), and through Logan's Rips at Fitzdale, Mulligan's Lower Pitch, and Seven Islands. The White River from Vermont and Ammonoosuc River from New Hampshire brought more logs into the Connecticut. A log boom was built between Wells River, Vermont, and Woodsville, New Hampshire, to hold the logs briefly and release them gradually to avoid jams in the Ox Bow. Men detailed to this work utilized Woodsville's saloons and red-light district. Some of the logs were destined for mills in Wilder and Bellows Falls, Vermont, while others were sluiced over the Bellows Falls dam. North Walpole, New Hampshire, contained twelve to eighteen saloons, patronized by the log drivers. Mount Tom was the landmark the log drivers used to gauge the distance to the final mills near Holyoke, Massachusetts. These spring drives were stopped after 1915, when pleasure boat owners complained about the hazards to navigation. The final drive included 500 workers controlling 65 million feet of logs. A final pulp drive consisted of 100,000 cords of four-foot logs in 1918. This was to take advantage of the wartime demand.

text: Starting about 1865, the river was used for massive

text: logging drives

text: from

text: Third Connecticut Lake

text: to initially

text: water power

text: ed

text: sawmill

text: s near Enfield Falls. Trees cut adjacent to tributary streams including

text: Perry Stream

text: and

text: Indian Stream

text: in

text: Pittsburg, New Hampshire

text: Halls Stream

text: on the

text: Quebec

text: –New Hampshire border,

text: Simms Stream

text: , the

text: Mohawk River

text: , and the

text: Nulhegan River

text: basin in

text: Essex County, Vermont

text: , would be flushed into the main river by the release of water impounded behind

text: splash dam

text: s. Several log drivers died trying to move logs through Perry Falls in Pittsburg. Teams of men would wait at

text: Canaan, Vermont

text: , to protect the bridges from log jams. Men guided logs through a  drop along the length of Fifteen-Mile Falls (now submerged under

text: Moore

text: and

text: Comerford

text: reservoirs), and through Logan's Rips at Fitzdale, Mulligan's Lower Pitch, and Seven Islands. The

text: White River

text: from Vermont and

text: Ammonoosuc River

text: from New Hampshire brought more logs into the Connecticut. A

text: log boom

text: was built between

text: Wells River, Vermont

text: , and

text: Woodsville, New Hampshire

text: , to hold the logs briefly and release them gradually to avoid jams in the Ox Bow. Men detailed to this work utilized Woodsville's saloons and

text: red-light district

text: . Some of the logs were destined for mills in

text: Wilder

text: and

text: Bellows Falls, Vermont

text: , while others were sluiced over the Bellows Falls dam.

text: North Walpole, New Hampshire

text: , contained twelve to eighteen saloons, patronized by the log drivers.

text: Mount Tom

text: was the landmark the log drivers used to gauge the distance to the final mills near

text: Holyoke, Massachusetts

text: . These spring drives were stopped after 1915, when pleasure boat owners complained about the hazards to navigation. The final drive included 500 workers controlling 65 million feet of logs. A final pulp drive consisted of 100,000 cords of four-foot logs in 1918. This was to take advantage of the wartime demand.

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answers: These spring drives were stopped after 1915

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answers: This was to take advantage of the wartime demand

text: The drainage area of the Rocky River covers 111 square miles. The Tennessee Valley Divide, which separates the Cumberland and Tennessee watersheds, crosses Jakes Mountain a few hundred yards south of the source of the Rocky River.  Streams on the north side of the mountain flow into the Rocky, while streams on the south side are part of the Sequatchie River watershed.  A string of ridges extending from the Cumberland Plateau, among them Long Mountain and Barnett Mountain, split the watershed of the Rocky from the watershed of the Collins River to the west.

text: The drainage area of the Rocky River covers 111 square miles. The Tennessee Valley Divide, which separates the Cumberland and

text: Tennessee

text: watersheds, crosses Jakes Mountain a few hundred yards south of the source of the Rocky River.  Streams on the north side of the mountain flow into the Rocky, while streams on the south side are part of the

text: Sequatchie River

text: watershed.  A string of ridges extending from the Cumberland Plateau, among them Long Mountain and Barnett Mountain, split the watershed of the Rocky from the watershed of the

text: Collins River

text: to the west.

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text: An ice divide is the boundary on an ice sheet, ice cap or glacier separating opposing flow directions of ice, analogous to a water divide. Such ice divides are important for geochronology investigations using ice cores, because such coring is typically made on top of a dome of an ice sheet to avoid interference caused by horizontal ice movement. Ice divides are used for looking at what the atmosphere was like in history. The ice is very accurate because instead of shifting horizontally like normal ice, it moves vertically downward with time trapping gases into its layers. Scientist find these ice divides and take ice cores from them, which are typically long cylinder poles of ice, and evaluate them. Once they have these ice cores, they are able to look through it and find elements that the snow and ice carried down with it during that time period such as sulfate, nitrate, and other ions. These ice cores are important in determining how our atmosphere has changed for the better or worse, and how we can fix it such as the greenhouse effect which discovered when scientist found how much more greenhouse gasses was in our atmosphere than there was in the past.

text: An ice divide is the boundary on an

text: ice sheet

text: ice cap

text: or

text: glacier

text: separating opposing flow directions of

text: ice

text: , analogous to a

text: water divide

text: . Such ice divides are important for

text: geochronology

text: investigations using

text: ice core

text: s, because such coring is typically made on top of a dome of an ice sheet to avoid interference caused by horizontal ice movement. Ice divides are used for looking at what the atmosphere was like in history. The ice is very accurate because instead of shifting horizontally like normal ice, it moves vertically downward with time trapping gases into its layers. Scientist find these ice divides and take ice cores from them, which are typically long cylinder poles of ice, and evaluate them. Once they have these ice cores, they are able to look through it and find elements that the snow and ice carried down with it during that time period such as sulfate, nitrate, and other ions. These ice cores are important in determining how our atmosphere has changed for the better or worse, and how we can fix it such as the greenhouse effect which discovered when scientist found how much more greenhouse gasses was in our atmosphere than there was in the past.

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answers: The ice moves vertically downward with time trapping gases into its layers

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answers: Ice divides are used for looking at what the atmosphere was like in history

answers: NDQ_006068

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text: Antigua and Barbuda does not have any permanent rivers.  Following is a list of streams in Antigua.  Barbuda does not have any streams.

text: Antigua and Barbuda

text: does not have any permanent rivers.  Following is a list of streams in

text: Antigua

text: Barbuda

text: does not have any streams.

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answers: NDQ_006063

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answers: NDQ_006064

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answers: NDQ_006065

answers: permanent

answers: NDQ_006066

answers: Atlantic Ocean

answers: NDQ_006067

answers: no streams

answers: NDQ_006068

answers: rivers provided water, plus

answers: NDQ_006069

answers: Antigua and Barbuda

text: Flat River is a stream in the U.S. state of Missouri. It is a tributary of the Big River.

text: Flat River is a

text: stream

text: in the

text: U.S. state

text: of

text: Missouri

text: . It is a tributary of the

text: Big River

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text: Hydrography of rivers and streams is also an integral part of water management. Most reservoirs in the United States use dedicated stream gauging and rating tables to determine inflows into the reservoir and outflows to irrigation districts, water municipalities and other users of captured water. River/stream hydrographers use handheld and bank mounted devices, to capture a sectional flow rate of moving water through a section.

text: Hydrography of rivers and streams is also an integral part of water management. Most reservoirs in the United States use dedicated stream gauging and rating tables to determine inflows into the reservoir and outflows to irrigation districts, water municipalities and other users of captured water. River/stream hydrographers use handheld and bank mounted devices, to capture a sectional flow rate of moving water through a section.

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text: A transport stream encapsulates a number of other substreams, often packetized elementary streams (PES) which in turn wrap the main data stream of an MPEG codec, as well as any number of non-MPEG codecs (such as AC3 or DTS audio, and MJPEG or JPEG 2000 video), text and pictures for subtitles, tables identifying the streams, and even broadcaster-specific information such as an electronic program guide. Many unrelated streams are often mixed together, such as several different television channels, or multiple angles of a movie. Each stream is chopped into (at most) 188-byte sections and interleaved together; because of the tiny packet size, streams can be interleaved with less latency and greater error resilience compared to program streams and common containers such as AVI, MOV/MP4, and MKV, which generally wrap each frame into one packet. This is particularly important for videoconferencing, where even one large frame may introduce unacceptable audio delay.

text: A transport stream encapsulates a number of other substreams, often

text: packetized elementary stream

text: s (PES) which in turn wrap the

text: main data stream

text: of an MPEG codec, as well as any number of non-MPEG codecs (such as

text: or

text: DTS

text: audio, and

text: MJPEG

text: or

text: JPEG 2000

text: video), text and pictures for subtitles, tables identifying the streams, and even broadcaster-specific information such as an

text: electronic program guide

text: . Many unrelated streams are often mixed together, such as several different television channels, or multiple

text: angles

text: of a movie. Each stream is chopped into (at most) 188-byte sections and interleaved together; because of the tiny packet size, streams can be interleaved with less latency and greater error resilience compared to

text: program streams

text: and common containers such as

text: AVI

text: MOV

text: , and

text: MKV

text: , which generally wrap each frame into one packet. This is particularly important for videoconferencing, where even one large frame may introduce unacceptable audio delay.

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text: Markandeya Purana and Brahmanda Purana divide Jambudvipa into four vast regions shaped like four petals of a lotus with Mount Meru being located at the center like a pericarp. The city of Brahmapuri is said to be enclosed by a river, known as Akash Ganga. Akash Ganga is said to issue forth from the foot of Lord Vishnu and after washing the lunar region falls "through the skies" and after encircling the Brahmapuri "splits up into four mighty streams", which are said to flow in four opposite directions from the landscape of Mount Meru and irrigate the vast lands of Jambudvipa.

text: Markandeya Purana and

text: Brahmanda Purana

text: divide Jambudvipa into four vast regions shaped like four petals of a

text: lotus

text: with Mount Meru being located at the center like a

text: pericarp

text: . The city of Brahmapuri is said to be enclosed by a river, known as Akash Ganga. Akash Ganga is said to issue forth from the foot of Lord

text: Vishnu

text: and after washing the lunar region falls "through the skies" and after encircling the Brahmapuri "splits up into four mighty streams", which are said to flow in four opposite directions from the landscape of Mount Meru and irrigate the vast lands of Jambudvipa.

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text: The verse 1.5, for example, states, "we meditate on the river whose water consists of five streams, which is wild and winding with its five springs, whose waves are the five vital breaths, whose fountainhead is the mind, of course of the five kinds of perceptions. It has five whirlpools, its rapids are the five pains, it has fifty kinds of sufferings, and five branches." Adi Shankara and other scholars have explained, using more ancient Indian texts, what each of these numbers correspond to. For example, the five streams are five receptive organs of a human body, the five waves are the five active organs of a human body, and five rapids are the major health-related life stages.

text: The verse 1.5, for example, states, "we meditate on the river whose water consists of five streams, which is wild and winding with its five springs, whose waves are the five vital breaths, whose fountainhead is the mind, of course of the five kinds of perceptions. It has five whirlpools, its rapids are the five pains, it has fifty kinds of sufferings, and five branches."

text: Adi Shankara

text: and other scholars have explained, using more ancient Indian texts, what each of these numbers correspond to. For example, the five streams are five receptive organs of a human body, the five waves are the five active organs of a human body, and five rapids are the major health-related life stages.

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text: Underlying the world-view is an account of the creation and re-creation of this middle-earth where the Dayak dwell, arising out of a cosmic battle in the beginning of time between a primal couple, a male and female bird/dragon (serpent). Representations of this primal couple are amongst the most pervasive motifs of Dayak art. The primal mythic conflict ended in a mutual, procreative murder, from the body parts of which the present universe arose stage by stage. This primal sacrificial creation of the universe in all its levels is the paradigm for, and is re-experienced and ultimately harmoniously brought together (according to Dayak beliefs) in the seasons of the year, the interdependence of river (up-stream and down-stream) and land, the tilling of the earth and fall of the rain, the union of male and female, the distinctions between and co-operation of social classes, the wars and trade with foreigners, indeed in all aspects of life, even including tattoos on the body, the lay-out of dwellings and the annual cycle of renewal ceremonies, funeral rites, etc.

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answers: the tilling of the earth and fall of the rain

text: The stream rises in mountains  high between Lakina River on the east and Kuskulana River on the west. It is about  long and joins the Chitina River  below the Lakina. Three miles from the Chitina, it forks. The west branch, which is called the Chokosna, drains an area of  and is nearly as large as the main stream above the forks. The upper  of the Gilahina in its course through the mountains has a grade of about  per mile. As it approaches the Chitina Valley, the grade increases, and for the lower , the average grade is about  per mile. There are no glaciers in the basin, and at normal stages, the water is clear and free from sediment. The valley floor is made up of gravel, boulders, sand, and clay, and at high stages, the stream transports considerable material, causing marked changes in the channel.

text: The stream rises in mountains  high between

text: Lakina River

text: on the east and

text: Kuskulana River

text: on the west. It is about  long and joins the

text: Chitina River

text: below the Lakina. Three miles from the Chitina, it forks. The west branch, which is called the Chokosna, drains an area of  and is nearly as large as the main stream above the forks. The upper  of the Gilahina in its course through the mountains has a grade of about  per mile. As it approaches the Chitina Valley, the grade increases, and for the lower , the average grade is about  per mile. There are no glaciers in the basin, and at normal stages, the water is clear and free from sediment. The valley floor is made up of gravel, boulders, sand, and clay, and at high stages, the stream transports considerable material, causing marked changes in the channel.

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answers: There are no glaciers in the basin

text: In natural streams, n values vary greatly along its reach, and will even vary in a given reach of channel with different stages of flow. Most research shows that n will decrease with stage, at least up to bank-full. Overbank n values for a given reach will vary greatly depending on the time of year and the velocity of flow. Summer vegetation will typically have a significantly higher n value due to leaves and seasonal vegetation. Research has shown, however, that n values are lower for individual shrubs with leaves than for the shrubs without leaves.This is due to the ability of the plant's leaves to streamline and flex as the flow passes them thus lowering the resistance to flow. High velocity flows will cause some vegetation (such as grasses and forbs) to lay flat, where a lower velocity of flow through the same vegetation will not.

text: In natural streams, n values vary greatly along its reach, and will even vary in a given reach of channel with different stages of flow. Most research shows that n will decrease with stage, at least up to bank-full. Overbank n values for a given reach will vary greatly depending on the time of year and the velocity of flow. Summer vegetation will typically have a significantly higher n value due to leaves and seasonal vegetation. Research has shown, however, that n values are lower for individual shrubs with leaves than for the shrubs without leaves.This is due to the ability of the plant's leaves to streamline and flex as the flow passes them thus lowering the resistance to flow. High velocity flows will cause some vegetation (such as grasses and forbs) to lay flat, where a lower velocity of flow through the same vegetation will not.

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answers: depends on the time of year

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answers: the continental divide

answers: NDQ_006067

answers: It does not say.

answers: NDQ_006068

answers: n

answers: NDQ_006069

answers: High velocity flows

text: Split by the Eastern Continental Divide, the mountain generates feeder streams to the North Fork Catawba River on its eastern slopes and to the North Toe River on its western slopes.

text: Split by the

text: Eastern Continental Divide

text: , the mountain generates feeder streams to the

text: North Fork Catawba River

text: on its eastern slopes and to the

text: North Toe River

text: on its western slopes.

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answers: Eastern Continental Divide

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answers: Split by the Eastern Continental Divide

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answers: Eastern Continental Divide

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answers: Divide

answers: NDQ_006065

answers: its western slopes

answers: NDQ_006066

answers: Atlantic Ocean

answers: NDQ_006067

answers: no

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answers: Rivers

answers: NDQ_006069

answers: Split by the Eastern Continental Divide

text: In the Oxford area the river splits into several streams across the floodplain, which create numerous islands.   On the right bank a large island is created by Seacourt Stream, Botley Stream and Bulstake Stream, and there are smaller islands, including the island now known as Osney, created by streams between Bulstake Stream and the Thames, including Osney Ditch.  The Oxford suburbs of Grandpont and New Hinksey are on an island created by Bulstake Stream, Hinksey Stream and Weirs Mill Stream.  Iffley Meadows is an island west of Iffley Lock, between Weirs Mill Stream, Hinksey Stream and the Thames.

text: In the

text: Oxford

text: area the river splits into several streams across the

text: floodplain

text: , which create numerous islands.   On the right bank a large island is created by

text: Seacourt Stream

text: Botley Stream

text: and

text: Bulstake Stream

text: , and there are smaller islands, including the island now known as

text: Osney

text: , created by streams between Bulstake Stream and the Thames, including

text: Osney Ditch

text: .  The Oxford suburbs of

text: Grandpont

text: and

text: New Hinksey

text: are on an island created by Bulstake Stream,

text: Hinksey Stream

text: and

text: Weirs Mill Stream

text: Iffley Meadows

text: is an island west of

text: Iffley Lock

text: , between Weirs Mill Stream, Hinksey Stream and the Thames.

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answers: created numerous islands

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answers: NDQ_006069

answers: river splits into several streams across the floodplain

text: The Tidbinbilla River, a perennial stream that is part of the Murrumbidgee catchment within the Murray-Darling basin, is located in the Australian Capital Territory, Australia.

text: The Tidbinbilla River, a

text: perennial stream

text: that is part of the

text: Murrumbidgee

text: catchment within the

text: Murray-Darling basin

text: , is located in the

text: Australian Capital Territory

text: Australia

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answers: The Tidbinbilla River

answers: NDQ_006068

answers: Rivers

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answers: Murray-Darling basin

text: Part of the South Branch's river bed is the plain of an ancient lake. The river wanders over moraines throughout its course. The substrate is rock strewn with sand and gravel; north of Sycamore the river has been mined for gravel. The average width of the South Branch is . It has the lowest natural flow rate of any stream in the Kishwaukee River watershed. The stream, however, also receives the largest discharge of any of the streams in the watershed due to treated wastewater from the city of DeKalb.

text: Part of the South Branch's

text: river bed

text: is the plain of an

text: ancient lake

text: . The river wanders over

text: moraine

text: s throughout its course. The substrate is rock strewn with sand and gravel; north of

text: Sycamore

text: the river has been

text: mined for gravel

text: . The average width of the South Branch is . It has the lowest natural

text: flow rate

text: of any stream in the Kishwaukee River watershed. The stream, however, also receives the largest discharge of any of the streams in the watershed due to treated wastewater from the city of

text: DeKalb

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answers: It has the lowest natural flow rate

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answers: an ancient lake

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answers: an ancient lake

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answers: Kishwaukee River

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answers: gravel

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answers: Kishwaukee River watershed

text: A total of seventy streams that are at least  long flow through the U.S. state of Idaho. All of these streams originate in the United States except the Kootenai River (third-longest) and the Moyie River (thirty-first-longest), both of which begin in the Canadian province of British Columbia. At , the Snake River is the longest and the only stream of more than  in total length. It begins in Wyoming and flows through Idaho for , and then through Oregon and Washington. Some of the other streams also cross borders between Idaho and Montana, Nevada, Oregon, Utah, Washington, or Wyoming, but the majority flow entirely within Idaho, the longest of which is the Salmon River at .

text: A total of seventy streams that are at least  long flow through the

text: U.S. state

text: of

text: Idaho

text: . All of these streams originate in the United States except the

text: Kootenai River

text: (third-longest) and the

text: Moyie River

text: (thirty-first-longest), both of which begin in the

text: Canadian

text: province

text: of

text: British Columbia

text: . At , the

text: Snake River

text: is the longest and the only stream of more than  in total length. It begins in

text: Wyoming

text: and flows through Idaho for , and then through

text: Oregon

text: and

text: Washington

text: . Some of the other streams also cross borders between Idaho and

text: Montana

text: Nevada

text: , Oregon,

text: Utah

text: , Washington, or Wyoming, but the majority flow entirely within Idaho, the longest of which is the

text: Salmon River

text: at .

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answers: No

answers: NDQ_006062

answers: the Salmon River

answers: NDQ_006063

answers: United States

answers: NDQ_006064

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answers: Pacific Ocean

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answers: Salty ocean

answers: NDQ_006068

answers: The Snake River

answers: NDQ_006069

answers: All of these streams originate in the United States

text: Since August 1921, Lees Ferry has been the site of a stream gage operated by the U.S. Geological Survey and has since accumulated one of the most extensive streamflow records ever made in the United States. The river flow here is the principal factor in allocating water to the seven U.S. and two Mexican states in the Colorado River basin. The Colorado River Compact of 1922 apportioned an equal portion of the river's flow to the Upper Basin (the U.S. states of Colorado, New Mexico, Utah, Wyoming and northern Arizona) and the Lower Basin (Arizona, California and Nevada), with the individual "basins" divided by an imaginary line at Lees Ferry.

text: Since August 1921, Lees Ferry has been the site of a

text: stream gage

text: operated by the

text: U.S. Geological Survey

text: and has since accumulated one of the most extensive streamflow records ever made in the United States. The river flow here is the principal factor in allocating water to the seven U.S. and two Mexican states in the Colorado River basin. The

text: Colorado River Compact

text: of 1922 apportioned an equal portion of the river's flow to the Upper Basin (the U.S. states of

text: Colorado

text: , New Mexico, Utah,

text: Wyoming

text: and northern Arizona) and the Lower Basin (Arizona,

text: California

text: and

text: Nevada

text: ), with the individual "basins" divided by an imaginary line at Lees Ferry.

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answers: no

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answers: Colorado River basin

answers: NDQ_006063

answers: Lower Basin

answers: NDQ_006064

answers: Basin

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answers: extensive

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answers: Colorado River

answers: NDQ_006067

answers: Salty ocean

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answers: the principal factor in allocating water

answers: NDQ_006069

answers: The Colorado River Compact of 1922

text: The streams formed in the Serra da Juréia are clear, with a pH of 5-6.5, and are low in nutrients.A few originate in springs in the campo, but most are rain-fed and intermittent.Quiet streams may become torrential during times of heavy rainfall.The Una do Prelado River, a blackwater river, meanders in a northeast direction through the plain between the Serra da Juréia and the Serra dos Itatins.The Serra da Juréia is divided by the valley of the Rio Verde, which flows south to the ocean.

text: The streams formed in the Serra da Juréia are clear, with a pH of 5-6.5, and are low in nutrients.A few originate in springs in the campo, but most are rain-fed and intermittent.Quiet streams may become torrential during times of heavy rainfall.The

text: Una do Prelado River

text: , a

text: blackwater river

text: , meanders in a northeast direction through the plain between the Serra da Juréia and the Serra dos Itatins.The Serra da Juréia is divided by the valley of the

text: Rio Verde

text: , which flows south to the ocean.

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answers: torrential

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answers: valley of the Rio Verde

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: Serra da Juréia

answers: NDQ_006063

answers: low in nutrients

answers: NDQ_006064

answers: campo

answers: NDQ_006065

answers: torrential

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: The Serra da Juréia

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: low in nutrients

text: For two-dimensional potential flow, streamlines are perpendicular to equipotential lines. Taken together with the velocity potential, the stream function may be used to derive a complex potential. In other words, the stream function accounts for the solenoidal part of a two-dimensional Helmholtz decomposition, while the velocity potential accounts for the irrotational part.

text: For two-dimensional

text: potential flow

text: , streamlines are perpendicular to

text: equipotential

text: lines. Taken together with the

text: velocity potential

text: , the stream function may be used to derive a

text: complex

text: potential. In other words, the stream function accounts for the

text: solenoidal

text: part of a two-dimensional

text: Helmholtz decomposition

text: , while the velocity potential accounts for the

text: irrotational

text: part.

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answers: accounts for the solenoidal part

answers: NDQ_006066

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answers: It does not say

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answers: NDQ_006069

answers: streamlines are perpendicular to equipotential lines

text: The Korang River is a stream in Punjab, Pakistan. It originates from Murree Hills and flows towards Islamabad. Korang Stream along with some other small streams coming from Margalla Hills have been set to form the artificial Rawal Lake in Islamabad. Korang River is the outlet stream of Rawal Dam. This stream crosses Islamabad Express Highway from between Korang Town and Judicial Colony. The terrain of this stream is eye catching and the Loi Bhair Wildlife Safari Park is located on the beautiful terrain of the left bank of Korang Stream. Onward, this stream joins Soan River before reaching the Grand Trunk Road. Just after this point, Lai Nullah also joins Soan River.

text: The Korang River is a stream in

text: Punjab, Pakistan

text: . It originates from

text: Murree

text: Hills and flows towards

text: Islamabad

text: . Korang Stream along with some other small streams coming from

text: Margalla Hills

text: have been set to form the artificial

text: Rawal Lake

text: in Islamabad. Korang River is the outlet stream of Rawal Dam. This stream crosses Islamabad Express Highway from between Korang Town and Judicial Colony. The terrain of this stream is eye catching and the Loi Bhair Wildlife Safari Park is located on the beautiful terrain of the left bank of Korang Stream. Onward, this stream joins

text: Soan River

text: before reaching the

text: Grand Trunk Road

text: . Just after this point,

text: Lai Nullah

text: also joins

text: Soan River

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answers: NDQ_006066

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answers: NDQ_006068

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answers: Korang River

text: or any tributary stream that runs parallel to, and within the floodplain of a larger river for considerable distance, before eventually joining it. This is especially the characteristic when such a stream is forced to flow along the base of the main river's natural levee. Where the two meet is known as a 'belated' confluence or a 'deferred' junction. The name is derived from a now vanished Native American tribe, the Yazoo Indians. The Choctaw word is translated to "River of Death" because of the strong flows under its bank full stage.

text: or any

text: tributary

text: stream

text: that runs parallel to, and within the

text: floodplain

text: of a larger

text: river

text: for considerable distance, before eventually joining it. This is especially the characteristic when such a stream is forced to flow along the base of the main river's

text: natural levee

text: . Where the two meet is known as a 'belated'

text: confluence

text: or a 'deferred' junction. The name is derived from a now vanished Native American tribe, the Yazoo Indians. The Choctaw word is translated to "River of Death" because of the strong flows under its bank full stage.

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answers: no

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answers: NDQ_006063

answers: levee

answers: NDQ_006064

answers: floodplain

answers: NDQ_006065

answers: strong

answers: NDQ_006066

answers: The name is derived from a now vanished Native American tribe

answers: NDQ_006067

answers: River of Death

answers: NDQ_006068

answers: strong flows under its bank

answers: NDQ_006069

answers: strong flows under its bank

text: River miles are used in a variety of ways. The Commonwealth of Pennsylvania, in its 2001 Pennsylvania Gazetteer of Streams, lists every named stream and every unnamed stream in a named geographic feature in the state, and gives the drainage basin area, mouth coordinates, and river mile, specifically the distance from the mouth of the tributary to the mouth of its parent stream. Some islands are named for their river mile distance, for example the Allegheny River in Pennsylvania has Six Mile Island, Nine Mile Island, Twelve Mile Island, and Fourteen Mile Island. (The last two islands form Allegheny Islands State Park, although Fourteen Mile Island was split into two parts by a dam).

text: River miles are used in a variety of ways. The Commonwealth of

text: Pennsylvania

text: , in its 2001 Pennsylvania Gazetteer of Streams, lists every named stream and every unnamed stream in a named geographic feature in the state, and gives the

text: drainage basin

text: area, mouth coordinates, and river mile, specifically the distance from the mouth of the tributary to the mouth of its parent stream. Some islands are named for their river mile distance, for example the

text: Allegheny River

text: in Pennsylvania has Six Mile Island, Nine Mile Island, Twelve Mile Island, and Fourteen Mile Island. (The last two islands form

text: Allegheny Islands State Park

text: , although Fourteen Mile Island was split into two parts by a dam).

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answers: mouth of its parent stream

answers: NDQ_006061

answers: no

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answers: Islands State Park

answers: NDQ_006063

answers: The Commonwealth of Pennsylvania

answers: NDQ_006064

answers: river mile

answers: NDQ_006065

answers: drainage basin area

answers: NDQ_006066

answers: Atlantic Ocean

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text: The brook played a very important role in the Roman settlement of Londinium, the city now known as London. The stream started in what is now Finsbury and flowed through the centre of the walled city, bringing a supply of fresh water whilst carrying waste away to the River Thames. Effectively dividing the settlement in two, it emerged just to the west of the present-day Cannon Street Railway Bridge. During Roman times it was also used for transport, with the limit of navigation some 200m from the Thames, at a point now known as Bucklersbury building. It was there the Romans built a port and temple to Mithras on the east bank of the stream. The temple was found and later excavated during rebuilding work after World War II. The Roman Governor's palace was found further down the east bank of the stream, near its entry into the Thames. The etymology begins soon after Londinium  was captured by the invading Anglo-Saxons during the late 6th century (also known then as Caer Lundein). It is thought that the brook was named because it ran through or under the London Wall; another theory is the name comes from Weala broc meaning 'brook of the Welsh'. Walbrook formed one division in the city: Ludgate Hill to the west and Cornhill to the east.

text: The

text: brook

text: played a very important role in the

text: Roman

text: settlement of

text: Londinium

text: , the city now known as

text: London

text: . The stream started in what is now

text: Finsbury

text: and flowed through the centre of the walled city, bringing a supply of fresh water whilst carrying waste away to the

text: River Thames

text: . Effectively dividing the settlement in two, it emerged just to the west of the present-day

text: Cannon Street Railway Bridge

text: . During Roman times it was also used for transport, with the limit of navigation some 200m from the Thames, at a point now known as Bucklersbury building. It was there the Romans built a port and temple to

text: Mithras

text: on the east bank of the stream.

text: The temple

text: was found and later excavated during rebuilding work after

text: World War II

text: . The Roman Governor's palace was found further down the east bank of the stream, near its entry into the Thames. The etymology begins soon after Londinium  was captured by the invading Anglo-Saxons during the late 6th century (also known then as Caer Lundein). It is thought that the brook was named because it ran through or under the

text: London Wall

text: ; another theory is the name comes from Weala broc meaning 'brook of the Welsh'. Walbrook formed one division in the city: Ludgate Hill to the west and Cornhill to the east.

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text: Historically, these rivers and streams were used to power various types of mills (i.e. grist mills, fulling mills, etc.), transport goods to market, and later to generate electric power (after 1880).  Today, these rivers are chiefly used in local recreational activities—including canoeing and fishing. The Fish Culture Unit of the New Jersey Division of Fish and Wildlife stocks these waterways each year with various species of trout. Some of these rivers—especially the Flat Brook, Paulins Kill and Pequest—have become well known as trout streams and for their suitability for fly-fishing.  The Flat Brook and its tributary the Big Flat Brook are regarded as the state's premiere trout stream.

text: Historically, these rivers and streams were used to power various types of mills (i.e. grist mills, fulling mills, etc.), transport goods to market, and later to generate electric power (after 1880).  Today, these rivers are chiefly used in local

text: recreational activities

text: —including

text: canoeing

text: and

text: fishing

text: . The Fish Culture Unit of the

entity_name: New Jersey Department of Environmental Protection

text: New Jersey Division of Fish and Wildlife

text: stocks these waterways each year with various species of

text: trout

text: . Some of these rivers—especially the Flat Brook, Paulins Kill and Pequest—have become well known as trout streams and for their suitability for

text: fly-fishing

text: .  The Flat Brook and its tributary the Big Flat Brook are regarded as the state's premiere trout stream.

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text: Below the col the Gravona valley is considered one of the most scenic in Corsica. The river begins with a low gradient and then falls sharply over rapids and falls by stages. Each stage is a pool containing native brown trout. The river is popular for fly fishing and also for white-water canoeing. The road and the rail line remain close to the stream.

text: Below the col the Gravona valley is considered one of the most scenic in Corsica. The river begins with a low gradient and then falls sharply over rapids and falls by stages. Each stage is a pool containing native brown trout. The river is popular for fly fishing and also for white-water canoeing. The road and the rail line remain close to the stream.

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text: The north side of Mount Kelsey drains into the West Branch of Clear Stream, a tributary of the Androscoggin River, which flows south and east into Maine, joining the Kennebec River near the Atlantic Ocean. The southeast side of Kelsey drains into North Inlet Stream, thence into Millsfield Pond Brook, and into Clear Stream. The west side of Kelsey drains into Phillips Brook, thence into the Upper Ammonoosuc River, the upper Connecticut River, and into Long Island Sound in Connecticut.

text: The north side of Mount Kelsey drains into the West Branch of

text: Clear Stream

text: , a

text: tributary

text: of the

text: Androscoggin River

text: , which flows south and east into

text: Maine

text: , joining the

text: Kennebec River

text: near the

text: Atlantic Ocean

text: . The southeast side of Kelsey drains into North Inlet Stream, thence into Millsfield Pond Brook, and into Clear Stream. The west side of Kelsey drains into

text: Phillips Brook

text: , thence into the

text: Upper Ammonoosuc River

text: , the upper

text: Connecticut River

text: , and into

text: Long Island Sound

text: in

text: Connecticut

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answers: the Kennebec River

text: Like most karst areas, Cedars of Lebanon State Forest is drained in large part by underground streams.  The water in the forest probably ends up in nearby streams, such as Hurricane Creek.  These streams empty into the Stones River's J. Percy Priest Lake impoundment, which is located just a few miles to the west.

text: Like most karst areas, Cedars of Lebanon State Forest is drained in large part by underground streams.  The water in the forest probably ends up in nearby streams, such as Hurricane Creek.  These streams empty into the

text: Stones River's

text: J. Percy Priest Lake

text: impoundment, which is located just a few miles to the west.

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text: Streaming technology is used to distribute Internet radio, typically using a lossy audio codec. Streaming audio formats include MP3, Ogg Vorbis, Windows Media Audio, RealAudio, and HE-AAC (or aacPlus).  Audio data is continuously transmitted serially (streamed) over the local network or internet in TCP or UDP packets, then reassembled at the receiver and played a second or two later. The delay is called lag, and is introduced at several stages of digital audio broadcasting.

text: Streaming

text: technology is used to distribute Internet radio, typically using a

text: lossy

text: audio codec

text: . Streaming audio formats include

text: Ogg Vorbis

text: Windows Media Audio

text: RealAudio

text: , and

text: HE-AAC

text: (or

text: aacPlus

text: ).  Audio data is continuously transmitted serially (streamed) over the local network or internet in

text: TCP

text: or

text: UDP

text: packets

text: , then reassembled at the receiver and played a second or two later. The delay is called

text: lag

text: , and is introduced at several stages of digital audio broadcasting.

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answers: at the receiver

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answers: Streaming

answers: NDQ_006069

answers: Streaming technology is used to distribute Internet radio

text: A stream is a flowing body of water with a current, confined within a bed and stream banks. Streams play an important corridor role in connecting fragmented habitats and thus in conserving biodiversity. The study of streams and waterways in general is known as surface hydrology. Types of streams include creeks, tributaries, which do not reach an ocean and connect with another stream or river, brooks, which are typically small streams and sometimes sourced from a spring or seep and tidal inlets

text: A stream is a flowing body of

text: water

text: with a

text: current

text: , confined within a

text: bed

text: and

text: stream bank

text: s. Streams play an important

text: corridor

text: role in connecting

text: fragmented habitats

text: and thus in conserving

text: biodiversity

text: . The study of streams and waterways in general is known as surface

text: hydrology

text: . Types of streams include

text: creeks

text: tributaries

text: , which do not reach an ocean and connect with another stream or river,

text: brooks

text: , which are typically small streams and sometimes sourced from a

text: spring

text: or

text: seep

text: and tidal inlets

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answers: tidal inlets

text: Today the Diocese covers an area of  and comprises the territory immediately west of the Great Dividing Range. The eastern boundary, except from Mt. Coricudgy by the Great Dividing Range southerly to Mt. Boonbourwa by a range generally south-easterly and then south-westerly, by a line west to the junction of Coorongooba and Running Stream Creeks, by Running Stream Creek downwards to Capertee River, by a line south and a line west to Mt. Canobla by a range generally south-westerly to the Great Dividing Range at Mt. McLean. The southern boundary is the Abercrombie and Lachlan Rivers (including West Cowra). The western boundary is the Eurow-Nyrang Mountains, the Harvey Range, a line from the junction of the Brummagen Creek and the Macquarie River to a point on the Macquarie River 16 km north of Warren, thence in a northerly straight line to a point on the Barwon River, 16 km west of Walgett. The northern boundary is a south-easterly line from this point on the Barwon River to the parish of Gunnedah.

text: Today the Diocese covers an area of  and comprises the territory immediately west of the

text: Great Dividing Range

text: . The eastern boundary, except from Mt. Coricudgy by the Great Dividing Range southerly to Mt. Boonbourwa by a range generally south-easterly and then south-westerly, by a line west to the junction of Coorongooba and Running Stream Creeks, by Running Stream Creek downwards to Capertee River, by a line south and a line west to Mt. Canobla by a range generally south-westerly to the Great Dividing Range at Mt. McLean. The southern boundary is the Abercrombie and Lachlan Rivers (including West Cowra). The western boundary is the Eurow-Nyrang Mountains, the Harvey Range, a line from the junction of the Brummagen Creek and the Macquarie River to a point on the Macquarie River 16 km north of Warren, thence in a northerly straight line to a point on the Barwon River, 16 km west of Walgett. The northern boundary is a south-easterly line from this point on the Barwon River to the parish of Gunnedah.

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text: The headwaters of the Hawkesbury River, the Avon River, the Cataract River, and the Cordeaux River, rise only a few miles from the sea, about  south of Sydney. These streams start on the inland-facing slopes of the plateau which forms the escarpment behind Wollongong. Flowing north-west, away from the sea, these streams combine to form the Nepean River, and flow north past the towns of Camden and Penrith. Near Penrith, the Warragamba River emerges from its canyon through the Blue Mountains and joins the Nepean. The Warragamba, formed by the joining of the Wollondilly River, the Nattai River, the Kowmung River and Coxs River drains a broad region of New South Wales on the eastern side of the Great Dividing Range. The other principal component of the upper Hawkesbury river system, the Grose River, rises in the area of Mount Victoria in the Blue Mountains.

text: The headwaters of the Hawkesbury River, the

text: Avon River

text: , the

text: Cataract River

text: , and the

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text: , rise only a few miles from the sea, about  south of Sydney. These streams start on the inland-facing slopes of the plateau which forms the escarpment behind

text: Wollongong

text: . Flowing north-west, away from the sea, these streams combine to form the Nepean River, and flow north past the towns of

text: Camden

text: and

text: Penrith

text: . Near Penrith, the

text: Warragamba River

text: emerges from its canyon through the

text: Blue Mountains

text: and joins the Nepean. The Warragamba, formed by the joining of the

text: Wollondilly River

text: , the

text: Nattai River

text: , the

text: Kowmung River

text: and

text: Coxs River

text: drains a broad region of New South Wales on the eastern side of the

text: Great Dividing Range

text: . The other principal component of the upper Hawkesbury river system, the

text: Grose River

text: , rises in the area of

text: Mount Victoria

text: in the Blue Mountains.

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text: The Divide trilogy is a fantasy young adult novel trilogy by Elizabeth Kay, which takes place in an alternate universe. The three books are The Divide (2002), Back to The Divide (2005), and Jinx on The Divide (2006). The first novel was originally published by the small press publisher Chicken House (now a division of Scholastic), with subsequent volumes published by Scholastic, which also reprinted the first novel. The books have been translated into French, German, Spanish, Finnish, Chinese, Japanese, Portuguese, Italian, Romanian and Dutch. Interior illustrations are by Ted Dewan.

text: The Divide trilogy is a

text: fantasy

text: young adult novel

text: trilogy

text: by

text: Elizabeth Kay

text: , which takes place in an

text: alternate universe

text: . The three books are The Divide (2002), Back to The Divide (2005), and Jinx on The Divide (2006). The first novel was originally published by the small press publisher Chicken House (now a division of Scholastic), with subsequent volumes published by

text: Scholastic

text: , which also reprinted the first novel. The books have been translated into French, German, Spanish, Finnish, Chinese, Japanese, Portuguese, Italian, Romanian and Dutch. Interior illustrations are by

text: Ted Dewan

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answers: The Divide trilogy

answers: NDQ_006068

answers: rivers

answers: NDQ_006069

answers: The Divide trilogy

text: The river has been popular as a trout stream since the early 19th century, when it became one of the first resort destinations in the United States. The subsequent depletion of the brook trout population by the 1850s led to an early conservation movement to preserve the river, including the introduction of hatcheries for brown trout. Its popularity as a trout stream arises in part from the many cold springs and deep pools in the upper river that keep the water at an even cold temperature. The fly fishing industry is centered on Roscoe, home to several fly-shops and bed and breakfasts catering to fishermen from around the world. More local fly fishing history and information can be found at the Catskill Fly Fishing Center and Museum located in Livingston Manor.

text: The river has been popular as a trout stream since the early 19th century, when it became one of the first resort destinations in the United States. The subsequent depletion of the

text: brook trout

text: population by the 1850s led to an early conservation movement to preserve the river, including the introduction of hatcheries for

text: brown trout

text: . Its popularity as a trout stream arises in part from the many cold springs and deep pools in the upper river that keep the water at an even cold temperature. The

text: fly fishing

text: industry is centered on

text: Roscoe

text: , home to several fly-shops and bed and breakfasts catering to fishermen from around the world. More local fly fishing history and information can be found at the

text: Catskill Fly Fishing Center and Museum

text: located in

text: Livingston Manor

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answers: NDQ_006063

answers: cold springs

answers: NDQ_006064

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answers: depletion

answers: NDQ_006066

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answers: NDQ_006068

answers: Cold springs

answers: NDQ_006069

answers: many cold springs and deep pools in the upper river that keep the water at an even cold temperature

text: MD 27 runs on top of or in the vicinity of a long ridge known for most of its length as Parr's Ridge. This ridge separates several sets of watersheds in central Maryland, with the result that MD 27 bridges no significant streams. From Germantown to south of Damascus, the ridge separates the waters of Little Seneca Creek to the west and Great Seneca Creek to the east; these creeks come together at Dawsonville and flow into the Potomac River. From Damascus north, all streams west of the ridge flow into the Monocacy River, including Bennett Creek, Bush Creek, and Little and Big Pipe Creek from south to north. All east-side streams flow into the Patuxent River from Damascus to south of Mount Airy, the South Branch of the Patapsco River from Mount Airy to Taylorsville, and the Patapsco River North Branch from Taylorsville to Manchester. MD 27 is part of the National Highway System as a principal arterial in five sections: from MD 355 in Germantown to Gue Road in Damascus; from Penn Shop Road south of Mount Airy to the Frederick–Carroll county line; from I-70 to the northern town limit of Mount Airy; from Chapel Road south of Westminster to Old Manchester Road in Mexico; and from the southern town limit of Manchester to MD 30.

text: MD 27 runs on top of or in the vicinity of a long ridge known for most of its length as

text: Parr's Ridge

text: . This ridge separates several sets of watersheds in central Maryland, with the result that MD 27 bridges no significant streams. From Germantown to south of Damascus, the ridge separates the waters of

text: Little Seneca Creek

text: to the west and

text: Great Seneca Creek

text: to the east; these creeks come together at

text: Dawsonville

text: and flow into the

text: Potomac River

text: . From Damascus north, all streams west of the ridge flow into the

text: Monocacy River

text: , including Bennett Creek, Bush Creek, and

text: Little and Big Pipe Creek

text: from south to north. All east-side streams flow into the

text: Patuxent River

text: from Damascus to south of Mount Airy, the South Branch of the

text: Patapsco River

text: from Mount Airy to

text: Taylorsville

text: , and the Patapsco River North Branch from Taylorsville to Manchester. MD 27 is part of the

text: National Highway System

text: as a principal arterial in five sections: from MD 355 in Germantown to Gue Road in Damascus; from Penn Shop Road south of Mount Airy to the Frederick–Carroll county line; from I-70 to the northern town limit of Mount Airy; from Chapel Road south of Westminster to Old Manchester Road in Mexico; and from the southern town limit of Manchester to MD 30.

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answers: The Potomac River

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answers: streams

answers: NDQ_006069

answers: Parr's Ridge

text: The Yuzui or Fish Mouth Levee, named for its conical head that is said to resemble the mouth of a fish, is the key part of Li Bing's construction. It is an artificial levee that divides the water into inner and outer streams. The inner stream is deep and narrow, while the outer stream is relatively shallow but wide. This special structure ensures that the inner stream carries approximately 60% of the river’s flow into the irrigation system during dry season. While during flood, this amount decreases to 40% to protect the people from flooding. The outer stream drains away the rest, flushing out much of the silt and sediment.

text: The Yuzui or Fish Mouth Levee, named for its conical head that is said to resemble the mouth of a fish, is the key part of Li Bing's construction. It is an artificial

text: levee

text: that divides the water into inner and outer streams. The inner stream is deep and narrow, while the outer stream is relatively shallow but wide. This special structure ensures that the inner stream carries approximately 60% of the river’s flow into the irrigation system during dry season. While during flood, this amount decreases to 40% to protect the people from flooding. The outer stream drains away the rest, flushing out much of the silt and sediment.

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answers: Fish Mouth Levee

answers: NDQ_006063

answers: 60%

answers: NDQ_006064

answers: Levee

answers: NDQ_006065

answers: during dry season

answers: NDQ_006066

answers: the pacific ocean

answers: NDQ_006067

answers: Fish Mouth Levee

answers: NDQ_006068

answers: irrigation

answers: NDQ_006069

answers: the inner stream carries approximately 60% of the river’s flow into the irrigation system during dry season

text: The Colorado begins at La Poudre Pass in the Southern Rocky Mountains of Colorado, at just under  above sea level. After a short run south, the river turns west below Grand Lake, the largest natural lake in the state. For the first  of its course, the Colorado carves its way through the mountainous Western Slope, a sparsely populated region defined by the portion of the state west of the Continental Divide. As it flows southwest, it gains strength from many small tributaries, as well as larger ones including the Blue, Eagle and Roaring Fork rivers. After passing through De Beque Canyon, the Colorado emerges from the Rockies into the Grand Valley, a major farming and ranching region where it meets one of its largest tributaries, the Gunnison River, at Grand Junction. Most of the upper river is a swift whitewater stream ranging from  wide, the depth ranging from , with a few notable exceptions, such as the Blackrocks reach where the river is nearly  deep. In a few areas, such as the marshy Kawuneeche Valley near the headwaters and the Grand Valley, it exhibits braided characteristics.

text: The Colorado begins at

text: La Poudre Pass

text: in the

text: Southern Rocky Mountains

text: of Colorado, at just under  above sea level. After a short run south, the river turns west below

text: Grand Lake

text: , the largest natural lake in the state. For the first  of its course, the Colorado carves its way through the mountainous

text: Western Slope

text: , a sparsely populated region defined by the portion of the state west of the

text: Continental Divide

text: . As it flows southwest, it gains strength from many small tributaries, as well as larger ones including the

text: Blue

text: Eagle

text: and

text: Roaring Fork

text: rivers. After passing through

text: De Beque Canyon

text: , the Colorado emerges from the Rockies into the

text: Grand Valley

text: , a major farming and ranching region where it meets one of its largest tributaries, the

text: Gunnison River

text: , at

text: Grand Junction

text: . Most of the upper river is a swift whitewater stream ranging from  wide, the depth ranging from , with a few notable exceptions, such as the Blackrocks

text: reach

text: where the river is nearly  deep. In a few areas, such as the marshy Kawuneeche Valley near the headwaters and the Grand Valley, it exhibits

text: braided

text: characteristics.

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text: Around 1900 there was a livestock market on the town square, and for a period in the middle of the 20th century a bus station. 2014/2015 the town square was renovated/renewed as it also was in 2003. 2003 landscape architect Charlotte Horn was inspired by the stream/river of Varde and the characteristic Varde clam with the black pearl, when reshaping the town square. In front of the old town hall of Varde is a basin with a big black round rock symbolizing the Varde pearl. From here a stream symbolizing the stream/river of Varde runs through a part of the town square. The webcam of the library of Varde takes pictures of the square around the clock and here the "stream" is visible.

text: Around 1900 there was a livestock market on the town square, and for a period in the middle of the

text: 20th century

text: a bus station. 2014/2015 the town square was renovated/renewed as it also was in 2003. 2003 landscape architect Charlotte Horn was inspired by the stream/river of Varde and the characteristic Varde clam with the black pearl, when reshaping the town square. In front of the old town hall of Varde is a basin with a big black round rock symbolizing the Varde pearl. From here a stream symbolizing the

text: stream/river of Varde

text: runs through a part of the town square. The webcam of the library of Varde takes pictures of the square around the clock and here the "stream" is visible.

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text: In the early stages of the network, ES5 tried to attract users by streaming movies in addition to in-network sharing. To do this, ES5 created a website at es5.org which provided links to dozens of Hollywood films immediately available for streaming.

text: In the early stages of the network, ES5 tried to attract users by streaming movies in addition to in-network sharing. To do this, ES5 created a website at es5.org which provided links to dozens of Hollywood films immediately available for streaming.

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text: The mountains of Shennongjia form a divide between two parts of the district: the central and northern part drains north, into the Han River (a tributary of the Yangtze which joins the Yangtze much farther east, in Wuhan), while the southern section drains into the Yangtze in a more direct way, via a number of short streams flowing south, such as Shen Nong Stream.

text: The mountains of Shennongjia form a divide between two parts of the district: the central and northern part drains north, into the

text: Han River

text: (a tributary of the

text: Yangtze

text: which joins the Yangtze much farther east, in

text: Wuhan

text: ), while the southern section drains into the Yangtze in a more direct way, via a number of short streams flowing south, such as

text: Shen Nong Stream

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text: The hydrology of Little Cottonwood Creek is typical of that of many urban streams along the Wasatch Front and in the Intermountain West. A system of diversions for withdrawal of irrigation water began to be developed on many Wasatch Front streams soon after settlers arrived in Salt Lake Valley in 1847. As the population of the Wasatch Front increased, more of the water in valley streams was needed for drinking and domestic purposes. To meet domestic needs, water is withdrawn from several Wasatch Front streams, including Little Cottonwood Creek, as they emerge from headwater canyons and enter Salt Lake Valley. The water needs of irrigators downstream from the canyon mouths are satisfied with water diverted out of the Jordan River and transported across the valley in a system of canals. Some of the water from the Jordan River is imported to the urbanized reach of Little Cottonwood Creek.The flood stage for the urban waterways is 5.7 feet. Notable flooding is rare, with significant flooding in 1983 and as recently as the summer of 2010, when the waterline was 6.3 feet above bank level.

text: The hydrology of Little Cottonwood Creek is typical of that of many urban streams along the

text: Wasatch Front

text: and in the

text: Intermountain West

text: . A system of diversions for withdrawal of irrigation water began to be developed on many Wasatch Front streams soon after settlers arrived in Salt Lake Valley in 1847. As the population of the Wasatch Front increased, more of the water in valley streams was needed for drinking and domestic purposes. To meet domestic needs, water is withdrawn from several Wasatch Front streams, including Little Cottonwood Creek, as they emerge from headwater canyons and enter Salt Lake Valley. The water needs of irrigators downstream from the canyon mouths are satisfied with water diverted out of the Jordan River and transported across the valley in a system of canals. Some of the water from the Jordan River is imported to the urbanized reach of Little Cottonwood Creek.The flood stage for the urban waterways is 5.7 feet. Notable flooding is rare, with significant flooding in 1983 and as recently as the summer of 2010, when the waterline was 6.3 feet above bank level.

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text: The list is arranged by drainage basin, with respective tributaries indented under each larger stream's name and ordered from downstream to upstream. Mato Grosso is divided by those streams that flow north to the Amazon and east to the Tocontins rivers and those that flow south to the Paraná river.  All rivers in Mato Grosso ultimately drain to the Atlantic Ocean.

text: The list is arranged by drainage basin, with respective tributaries indented under each larger stream's name and ordered from downstream to upstream. Mato Grosso is divided by those streams that flow north to the

text: Amazon

text: and east to the

text: Tocontins

text: rivers and those that flow south to the

text: Paraná

text: river.  All rivers in Mato Grosso ultimately drain to the Atlantic Ocean.

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answers: All rivers in Mato Grosso ultimately drain to the Atlantic Ocean

text: This page shows the results of the Taekwondo Competition at the 1995 Pan American Games, held from July 23 to August 8, 1995 in Mar del Plata, Argentina. There were a total number of eight medal events, four for both men and women.

text: This page shows the results of the

text: Taekwondo Competition

text: at the

text: 1995 Pan American Games

text: , held from July 23 to August 8, 1995 in

text: Mar del Plata, Argentina

text: . There were a total number of eight medal events, four for both men and women.

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text: The area around the settlement of Štrbské Pleso is a drainage divide for two drainage basins. To the east of this divide, streams are the headwaters of the Poprad River, of the Baltic Sea drainage basin. To the west of the divide streams are tributaries of the Váh, of the Black Sea drainage basin. The most popular waterfalls include Studenovodské vodopády, Kmeťov vodopád, Vajanského vodopád, Roháčsky vodopád, and Vodopád Skok.

text: The area around the settlement of

text: Štrbské Pleso

text: is a

text: drainage divide

text: for two

text: drainage basin

text: s. To the east of this divide,

text: streams

text: are the

text: headwater

text: s of the

text: Poprad River

text: , of the

text: Baltic Sea

text: drainage basin. To the west of the divide streams are

text: tributaries

text: of the

text: Váh

text: , of the

text: Black Sea

text: drainage basin. The most popular waterfalls include Studenovodské vodopády, Kmeťov vodopád, Vajanského vodopád, Roháčsky vodopád, and Vodopád Skok.

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answers: Baltic Sea

answers: NDQ_006064

answers: waterfalls

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answers: popular

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answers: Atlantic Ocean

answers: NDQ_006067

answers: Black Sea

answers: NDQ_006068

answers: Poprad River

answers: NDQ_006069

answers: Poprad River, of the Baltic Sea drainage basin

text: Dasysphinx mucescens is a moth of the Arctiidae family. It was described by Felder in 1874. It is found in Colombia.

text: Dasysphinx mucescens is a

text: moth

text: of the

text: Arctiidae

text: family. It was described by Felder in 1874. It is found in

text: Colombia

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answers: sedimentation

answers: NDQ_006066

answers: Arctiidae

answers: NDQ_006067

answers: It is found in Colombia

answers: NDQ_006068

answers: It was described by Felder

answers: NDQ_006069

answers: Arctiidae family

text: Use of the word as "image" is relatively common in Attic texts; the use in the singular is found in Plato (Phaedra 250a) and Aristotle (Rhetorica 1356a31). The word is found in inscriptions on ostraca and in the Tebtunis papyri.

text: Use of the word as "image" is relatively common in Attic texts; the use in the singular is found in

text: Plato

text: (Phaedra 250a) and

text: Aristotle

text: (Rhetorica 1356a31). The word is found in inscriptions on ostraca and in the Tebtunis papyri.

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answers: NDQ_006069

answers: The word is found in inscriptions on ostraca

text: Menu driven DOS with enhanced features. Sorts disk directory listings and can set display options. File directory can be compressed. Can display deleted files and undelete them. Some advanced features required a proprietary TOP-DOS format.

text: Menu driven DOS with enhanced features. Sorts disk directory listings and can set display options. File directory can be compressed. Can display deleted files and undelete them. Some advanced features required a proprietary TOP-DOS format.

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answers: TOP-DOS

text: A stream rises above Bearsted. It powered two mills.

text: A stream rises above Bearsted. It powered two mills.

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answers: Bearsted

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answers: Bearsted

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answers: Bearsted

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answers: It powered two mills

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answers: no

answers: NDQ_006068

answers: power

answers: NDQ_006069

answers: It powered two mills

text: Wild animals found living in the reserve include red deer, roe deer, otter, red fox, mountain hare, badger, pine marten and Britain's most threatened mammal, the water vole. Brown trout and salmon are found in the rivers and streams. The moors are clad in ling and bell heather and are home to black grouse, red grouse and ptarmigan. Other large birds found in the reserve include the golden eagle, white-tailed eagle, osprey, buzzard, peregrine falcon, merlin, kestrel and raven.

text: Wild animals found living in the reserve include

text: red deer

text: roe deer

text: otter

text: red fox

text: mountain hare

text: badger

text: pine marten

text: and Britain's most threatened mammal, the

text: water vole

text: Brown trout

text: and

text: salmon

text: are found in the rivers and streams. The moors are clad in

text: ling

text: and

text: bell heather

text: and are home to

text: black grouse

text: red grouse

text: and

text: ptarmigan

text: . Other large birds found in the reserve include the

text: golden eagle

text: white-tailed eagle

text: osprey

text: buzzard

text: peregrine falcon

text: merlin

text: kestrel

text: and

text: raven

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answers: NDQ_006060

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answers: NDQ_006061

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answers: NDQ_006063

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answers: NDQ_006064

answers: 2

answers: NDQ_006065

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answers: NDQ_006066

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answers: NDQ_006067

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answers: NDQ_006068

answers: 0

answers: NDQ_006069

answers: 0

answers: NDQ_006060

answers: moors

answers: NDQ_006061

answers: no

answers: NDQ_006062

answers: a barrier reef

answers: NDQ_006063

answers: wild animals

answers: NDQ_006064

answers: moors

answers: NDQ_006065

answers: Britain's

answers: NDQ_006066

answers: the Pacific Ocean

answers: NDQ_006067

answers: Salmon

answers: NDQ_006068

answers: rivers and streams

answers: NDQ_006069

answers: Britain's most threatened mammal