text: Although in former literature a height around 7,320 m was traditionally given, the mountain is more likely to be around 7,150 m high. The Russian military 1:100,000 topographical map shows a height of 7,120 m. The currently most accurate map of the region probably is that in the series of "Maps of Snow Mountains in China", which gives a height of 7,147 m. On this map the pass connecting to Gasherbrum III is 6,493 m high (654 m prominence).

text: Although in former literature a height around 7,320 m was traditionally given, the mountain is more likely to be around 7,150 m high. The Russian military 1:100,000 topographical map shows a height of 7,120 m. The currently most accurate map of the region probably is that in the series of "Maps of Snow Mountains in China", which gives a height of 7,147 m. On this map the pass connecting to Gasherbrum III is 6,493 m high (654 m prominence).

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prompt_style: Can the question be answered based on the available context? choose one:

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answers: The Russian military 1:100,000 topographical map

answers: NDQ_001587

answers: Maps of Snow Mountains in China

answers: NDQ_001588

answers: the pass connecting to Gasherbrum III

answers: NDQ_001589

answers: height of 7,120 m

answers: NDQ_001590

answers: 6,493 m

answers: NDQ_001591

answers: height

answers: NDQ_001592

answers: height

answers: NDQ_001593

answers: the mountain is more likely to be around 7,150

answers: NDQ_001594

answers: 7120 m

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: It can be used to determine the direction that rivers and streams flow

answers: NDQ_001598

answers: prominence

answers: NDQ_001600

answers: The pass

answers: NDQ_001603

answers: It is not possible to say

answers: NDQ_001605

answers: Snow Mountains in China

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographical map

answers: NDQ_001611

answers: prominence

answers: NDQ_001613

answers: 7120 m

answers: NDQ_001614

answers: height

answers: NDQ_001618

answers: elevation

answers: NDQ_001619

answers: Map of Snow Mountains in China

answers: NDQ_001620

answers: prominence

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answers: topographical map

answers: NDQ_001622

answers: prominence

answers: NDQ_001623

answers: prominence

answers: NDQ_001624

answers: pass

answers: NDQ_001625

answers: 6,493 m

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text: "EX1201" was the first expedition of the 2012 field season for NOAA Ship Okeanos Explorer. The primary objective of this shakedown cruise was to operationally test the vessel, its systems, and all mission equipment. A secondary objective of the expedition was to use the ship’s technologically advanced multibeam sonar to map three Northeast and Mid-Atlantic canyon areas in support of the benthic habitat identification and management efforts of NOAA's Northeast Fisheries Science Center (NEFSC).After departing its homeport of Davisville, Rhode Island, on February 14, Okeanos Explorer proceeded offshore to Veatch Canyon where a sonar patch test was conducted to ensure the proper calibration of the vessel’s multibeam echosounder. As part of successful patch test operations, approximately 280 square kilometers of Veatch Canyon were bathymetrically mapped, including the majority of the first priority area identified by NEFSC.  Later in the cruise, focused survey operations conducted at Block, Ryan, and McMaster Canyons mapped approximately 900 square kilometers of seafloor, including 65 percent of the second NEFSC priority area.Focused mapping operations at Hendrickson, Toms, and Berkeley Canyons covered approximately 1,400 square kilometers of seafloor. Finally, focused mapping operations at Hendrickson, Toms, and Berkeley Canyons covered approximately 1400 square kilometers of seafloor, including 85 percent of the third NEFSC priority area.While transiting along the continental shelf break between focused mapping areas, multibeam, single beam, and sub-bottom sonar data was collected, adding to the seafloor mapping coverage established on Okeanos Explorer cruise EX1106. In addition to successful shakedown testing and mapping operations, EX1201 also yielded a number of positive educational outcomes. During the cruise, two graduate interns were trained in seafloor mapping operations as part of the Okeanos Explorer internship program. Additionally, approximately 50 high school students, educators, and local media toured the vessel and learned about its mission at the conclusion of the expedition, in Charleston, South Carolina.

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answers: 280 square kilometers

text: Villa del Sol is located northwest of the center of Cameron County at  (26.191502, -97.576620). It is on Texas State Highway 345, encompassing an area shown as "Lantana" on federal topographic maps. TX 345 leads southwest  to the center of San Benito.

text: Villa del Sol is located northwest of the center of Cameron County at  (26.191502, -97.576620). It is on

entity_name: Texas State Highway 345

text: Texas State Highway 345

text: , encompassing an area shown as "Lantana" on federal topographic maps. TX 345 leads southwest  to the center of

entity_name: San Benito, Texas

text: San Benito

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text: This method can be used to estimate the depth of the magnetic materials beneath the earth. The magnetic data is processed by the spectral methods such as Fourier transforms. The FFT algorithm makes the spectral analysis of signals fast, easy and efficient.The FFT computations can be performed in the machines which allow us to perform contour mapping. The upward continuation method attenuates the wave number anomalies associated with the shallow magnetic sources. Thus the signal components contain the information about the objects situated deep beneath the earth.

text: This method can be used to estimate the depth of the magnetic materials beneath the earth. The magnetic data is processed by the spectral methods such as Fourier transforms. The FFT algorithm makes the spectral analysis of signals fast, easy and efficient.The FFT computations can be performed in the machines which allow us to perform

entity_name: Contour line

text: contour mapping.

text: The upward continuation method attenuates the wave number anomalies associated with the shallow magnetic sources. Thus the signal components contain the information about the objects situated deep beneath the earth.

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answers: FFT algorithm makes the spectral analysis of signals fast, easy and efficient

answers: NDQ_001590

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answers: NDQ_001597

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answers: NDQ_001620

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answers: upward continuation

text: An isopycnal is a line connecting points of a specific density or potential density. Isopycnals are often displayed graphically to help visualize "layers" of water in the ocean or gasses in the atmosphere in a similar manner to how contour lines are used in topographic maps to help visualize topography.

text: An isopycnal is a line connecting points of a specific

entity_name: Density

text: density

text: or

entity_name: Potential density

text: potential density

text: . Isopycnals are often displayed graphically to help visualize "layers" of water in the ocean or gasses in the atmosphere in a similar manner to how

text: contour lines

text: are used in topographic maps to help visualize

entity_name: Topography

text: topography

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answers: NDQ_001587

answers: isopycnals

answers: NDQ_001588

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answers: NDQ_001589

answers: isopycnals are often displayed graphically

answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001592

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answers: NDQ_001594

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: isopycnals

answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001611

answers: isopycnal

answers: NDQ_001613

answers: Isopycnals

answers: NDQ_001614

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answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

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answers: NDQ_001623

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answers: NDQ_001624

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answers: NDQ_001625

answers: "layers"

text: A topographic map is the ordered projection of a sensory surface, like the retina or the skin, or an effector system, like the musculature, to one or more structures of the central nervous system.  Topographic maps can be found in all sensory systems and in many motor systems.

text: A topographic map is the ordered projection of a sensory surface, like the retina or the skin, or an effector system, like the musculature, to one or more structures of the

entity_name: Central nervous system

text: central nervous system

text: .  Topographic maps can be found in all

entity_name: Sensory system

text: sensory system

text: s and in many

entity_name: Motor system

text: motor system

text: s.

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text: USGS topographical maps show a common  elevation contour line running throughout a ridge along old Hwy 90 (Old Spanish Trail) on the western edge of the city. It was primarily this area which did not see the surge inundation of Hurricane Katrina.

text: USGS topographical maps show a common  elevation contour line running throughout a ridge along old Hwy 90 (

entity_name: Old Spanish Trail (auto trail)

text: Old Spanish Trail

text: ) on the western edge of the city. It was primarily this area which did not see the surge inundation of Hurricane Katrina.

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text: The Coordinates provided above were taken from the most current satellite photographs(Google Earth Pro) and as such represent the most accurate representation of the location of the boundary peak. Topographic maps of this area are dated (see USGS Historical Topographic maps) and do not provide the accuracy of the Global Positioning System that recent Satellite photographs have. Boundary Peaks 87-91 and 112-117 are not actually summits, but monuments (survey markers) placed by the USGS Geodetic Survey.

text: The Coordinates provided above were taken from the most current satellite photographs(Google Earth Pro) and as such represent the most accurate representation of the location of the boundary peak. Topographic maps of this area are dated (see

entity_name: Geospatial summary of the High Peaks/Summits of the Juneau Icefield

entity_section: USGS Historical Topographic Maps for the Juneau Icefield area

text: USGS Historical Topographic maps

text: ) and do not provide the accuracy of the

entity_name: Global Positioning System

text: Global Positioning System

text: that recent Satellite photographs have. Boundary Peaks 87-91 and 112-117 are not actually summits, but monuments (

entity_name: Survey marker

text: survey marker

text: s) placed by the

entity_name: U.S. National Geodetic Survey

text: USGS Geodetic Survey

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answers: 112-117

text: The ring-like nature of this feature was first observed by Thomas A. Edsall in 1990. It was first mapped in detail as part of a bathymetric map of Lake Ontario that was compiled from historic data sets by the National Oceanic and Atmospheric Administration’s (NOAA) National Geophysical Data Center, the NOAA Great Lakes Environmental Research Laboratory, and the Canadian Hydrographic Service. Based on this bathymetric map and field investigations, it was first proposed that Charity Creek Crater is an impact crater in 2001. In November 2010 and May 2011, high-resolution bathymetric and acoustic backscatter data were collected from the area of Charity Shoal and a 1 by 1 m grid model of its bathymetry was assembled by the Canadian Hydrographic Service. In July 2012, detailed magnetic and bathymetric surveys were conducted across a  area over Charity Shoal.

text: The ring-like nature of this feature was first observed by Thomas A. Edsall in 1990. It was first mapped in detail as part of a bathymetric map of Lake Ontario that was compiled from historic data sets by the

entity_name: National Oceanic and Atmospheric Administration

text: National Oceanic and Atmospheric Administration

text: ’s (NOAA)

entity_name: National Geophysical Data Center

text: National Geophysical Data Center

text: , the NOAA

entity_name: Great Lakes Environmental Research Laboratory

text: Great Lakes Environmental Research Laboratory

text: , and the

entity_name: Canadian Hydrographic Service

text: Canadian Hydrographic Service

text: . Based on this bathymetric map and field investigations, it was first proposed that Charity Creek Crater is an impact crater in 2001. In November 2010 and May 2011, high-resolution

entity_name: Bathymetry

text: bathymetric

text: and acoustic backscatter data were collected from the area of Charity Shoal and a 1 by 1 m grid model of its

text: bathymetry

text: was assembled by the Canadian Hydrographic Service. In July 2012, detailed

entity_name: Magnetic anomaly

text: magnetic

text: and bathymetric surveys were conducted across a  area over Charity Shoal.

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text: TERCOM – Terrain Contour Matching. A digital representation of an area of terrain is mapped based on digital terrain elevation data or stereo imagery. This map is then inserted into a TLAM mission which is then loaded onto the missile. When the missile is in flight it compares the stored map data with radar altimeter data collected as the missile overflies the map. Based on comparison results the missile's inertial navigation system is updated and the missile corrects its course. TERCOM was based on, and was a significant improvement on, "Fingerprint," a technology developed in 1964 for the SLAM.

entity_name: TERCOM

text: TERCOM

text: – Terrain Contour Matching. A digital representation of an area of terrain is mapped based on digital terrain elevation data or stereo imagery. This map is then inserted into a TLAM mission which is then loaded onto the missile. When the missile is in flight it compares the stored map data with radar altimeter data collected as the missile overflies the map. Based on comparison results the missile's inertial navigation system is updated and the missile corrects its course. TERCOM was based on, and was a significant improvement on, "Fingerprint," a technology developed in 1964 for the

entity_name: Supersonic Low Altitude Missile

text: SLAM

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answers: contour lines

answers: NDQ_001587

answers: a digital representation of an area of terrain is mapped

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: stereo imagery

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: area of terrain

answers: NDQ_001592

answers: TERCOM

answers: NDQ_001593

answers: terrain elevation data

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: terrain elevation data or stereo imagery

answers: NDQ_001598

answers: terrain elevation data

answers: NDQ_001600

answers: TLAM

answers: NDQ_001603

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answers: NDQ_001605

answers: TERCOM – Terrain Contour Matching

answers: NDQ_001606

answers: contour interval

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001619

answers: altimeter

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text: In the 1970s, the Hawaiian seafloor was mapped using ship-based sonar. Computed SYNBAPS (Synthetic Bathymetric Profiling System) data filled holes between the ship-based sonar bathymetric measurements. From 1994 to 1998 the Japan Agency for Marine-Earth Science and Technology (JAMSTEC) mapped Hawaii in detail and studied its ocean floor, making it one of the world's best-studied marine features. The JAMSTEC project, a collaboration with USGS and other agencies, utilized manned submersibles, remotely operated underwater vehicles, dredge samples, and core samples. The Simrad EM300 multibeam  side-scanning sonar system collected bathymetry and backscatter data.

text: In the 1970s, the Hawaiian seafloor was mapped using ship-based

entity_name: Sonar

text: sonar

text: . Computed SYNBAPS (Synthetic Bathymetric Profiling System) data filled holes between the ship-based sonar

text: bathymetric

text: measurements. From 1994 to 1998 the

entity_name: Japan Agency for Marine-Earth Science and Technology

text: Japan Agency for Marine-Earth Science and Technology

text: (JAMSTEC) mapped Hawaii in detail and studied its ocean floor, making it one of the world's best-studied marine features. The JAMSTEC project, a collaboration with USGS and other agencies, utilized manned

entity_name: Submersible

text: submersibles

entity_name: Remotely operated underwater vehicle

text: remotely operated underwater vehicle

text: s,

entity_name: Dredging

text: dredge sample

text: s, and

entity_name: Core sample

text: core sample

text: s. The Simrad EM300 multibeam

entity_name: Side-scan sonar

text: side-scanning sonar

text: system collected bathymetry and

entity_name: Backscatter

text: backscatter

text: data.

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answers: 4

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answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: The JAMSTEC project

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: manned submersibles, remotely operated underwater vehicles, dredge samples, and core samples

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: depth

answers: NDQ_001592

answers: bathymetric measurements

answers: NDQ_001593

answers: topographic map

answers: NDQ_001594

answers: bathymetry

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: topographic map

answers: NDQ_001598

answers: bathymetric measurements

answers: NDQ_001600

answers: bathymetry

answers: NDQ_001603

answers: JAMSTEC

answers: NDQ_001605

answers: The JAMSTEC project

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: contour lines

answers: NDQ_001611

answers: SYNBAPS

answers: NDQ_001613

answers: the side of the circle with the higher elevation

answers: NDQ_001614

answers: topographic maps

answers: NDQ_001618

answers: bathymetric

answers: NDQ_001619

answers: bathymetry

answers: NDQ_001620

answers: bathymetric

answers: NDQ_001621

answers: bathymetry

answers: NDQ_001622

answers: bathymetric

answers: NDQ_001623

answers: bathymetric

answers: NDQ_001624

answers: bathymetric

answers: NDQ_001625

answers: Bathymetric

text: Topographic maps show the shape of Earth’s surface by using contour lines, the lines on the map that join points of equal elevation. They are among the most well-known symbols on modern maps as they are self-explanatory and accurately represent their phenomena. They make it possible to the depict height, depth, and even slope. Contour lines will be closer together or spaced apart to show the steepness of the area. If the line is spaced closer together, it means that there is a steeper slope. If they are farther apart, the area has a low slope. An area of low slope generally uses contour intervals of 10 feet or less. Areas that contain mountain or other high slope can use an interval of 100 feet.

entity_name: Topographic map

text: Topographic map

text: s show the shape of Earth’s surface by using

text: contour line

text: s, the lines on the map that join points of equal elevation. They are among the most well-known symbols on modern maps as they are self-explanatory and accurately represent their phenomena. They make it possible to the depict height, depth, and even

entity_name: Slope

text: slope

text: . Contour lines will be closer together or spaced apart to show the steepness of the area. If the line is spaced closer together, it means that there is a steeper slope. If they are farther apart, the area has a low slope. An area of low slope generally uses

text: contour interval

text: s of 10 feet or less. Areas that contain mountain or other high slope can use an interval of 100 feet.

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answers: 5

answers: NDQ_001624

answers: 0

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answers: NDQ_001586

answers: The lines on the map that join points of equal elevation

answers: NDQ_001587

answers: shows the shape of Earth’s surface

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: high slope can use an interval of 100 feet

answers: NDQ_001590

answers: The lines on the map that join points of equal elevation

answers: NDQ_001591

answers: steeper slope

answers: NDQ_001592

answers: depict height, depth

answers: NDQ_001593

answers: contour lines will be closer together or spaced apart to show the steepness of the area

answers: NDQ_001594

answers: depth

answers: NDQ_001595

answers: 10 feet

answers: NDQ_001597

answers: The lines on the map that join points of equal elevation

answers: NDQ_001598

answers: If the line is spaced closer together

answers: NDQ_001600

answers: If they are farther apart, the area has a low slope

answers: NDQ_001603

answers: They make it possible to the depict height, depth, and even slope

answers: NDQ_001605

answers: None of the above choices.

answers: NDQ_001606

answers: spaced apart

answers: NDQ_001608

answers: The lines on the map that join points of equal elevation

answers: NDQ_001611

answers: If they are farther apart

answers: NDQ_001613

answers: If they are farther apart, the area has a low slope

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Earth’s surface

answers: NDQ_001619

answers: depth

answers: NDQ_001620

answers: slope

answers: NDQ_001621

answers: Topographic

answers: NDQ_001622

answers: Earth’s surface

answers: NDQ_001623

answers: contour lines

answers: NDQ_001624

answers: slope

answers: NDQ_001625

answers: 10 feet or less

text: In 1890, Peano discovered a continuous curve, now called the Peano curve, that passes through every point of the unit square (). His purpose was to construct a continuous mapping from the unit interval  onto the unit square. Peano was motivated by Georg Cantor's earlier counterintuitive result that the infinite number of points in a unit interval is the same cardinality as the infinite number of points in any finite-dimensional manifold, such as the unit square.  The problem Peano solved was whether such a mapping could be continuous; i.e., a curve that fills a space. Peano's solution does not set up a continuous one-to-one correspondence between the unit interval and the unit square, and indeed such a correspondence does not exist (see below).

text: In 1890,

entity_name: Giuseppe Peano

text: Peano

text: discovered a continuous curve, now called the

entity_name: Peano curve

text: Peano curve

text: , that passes through every point of the unit square (). His purpose was to construct a

entity_name: Continuous function

text: continuous mapping

text: from the

entity_name: Unit interval

text: unit interval

text: onto the

entity_name: Unit square

text: unit square

text: . Peano was motivated by

entity_name: Georg Cantor

text: Georg Cantor

text: 's earlier counterintuitive result that the infinite number of points in a unit interval is the same

entity_name: Cardinality

text: cardinality

text: as the infinite number of points in any finite-dimensional

entity_name: Manifold

text: manifold

text: , such as the unit square.  The problem Peano solved was whether such a mapping could be continuous; i.e., a curve that fills a space. Peano's solution does not set up a continuous

entity_name: Bijection

text: one-to-one correspondence

text: between the unit interval and the unit square, and indeed such a correspondence does not exist (see below).

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text: Detailed military surveys in Britain (beginning in the late eighteenth century) were called Ordnance Surveys, and this term was used into the 20th century as generic for topographic surveys and maps. The earliest scientific surveys in France were called the Cassini maps after the family who produced them over four generations. The term "topographic surveys" appears to be American in origin. The earliest detailed surveys in the United States were made by the “Topographical Bureau of the Army,” formed during the War of 1812, which became the Corps of Topographical Engineers in 1838. After the work of national mapping was assumed by the U.S. Geological Survey in 1878, the term topographical remained as a general term for detailed surveys and mapping programs, and has been adopted by most other nations as standard.

text: Detailed military surveys in

entity_name: Great Britain

text: Britain

text: (beginning in the late eighteenth century) were called

entity_name: Ordnance Survey

text: Ordnance Survey

text: s, and this term was used into the 20th century as generic for topographic surveys and maps. The earliest scientific surveys in France were called the

entity_name: French cartography

text: Cassini maps

text: after the family who produced them over four generations. The term "topographic surveys" appears to be American in origin. The earliest detailed surveys in the United States were made by the “Topographical Bureau of the Army,” formed during the

entity_name: War of 1812

text: War of 1812

text: , which became the

entity_name: Corps of Topographical Engineers

text: Corps of Topographical Engineers

text: in 1838. After the work of national mapping was assumed by the

entity_name: United States Geological Survey

text: U.S. Geological Survey

text: in 1878, the term topographical remained as a general term for detailed surveys and mapping programs, and has been adopted by most other nations as standard.

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answers: NDQ_001586

answers: Ordnance Surveys

answers: NDQ_001587

answers: Detailed military surveys in Britain

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: The term "topographic surveys" appears to be American in origin

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: topographic surveys

answers: NDQ_001592

answers: national mapping

answers: NDQ_001593

answers: topographic

answers: NDQ_001594

answers: Bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Ordnance Surveys

answers: NDQ_001598

answers: It has been adopted by most other nations as standard

answers: NDQ_001600

answers: Plain or plateau

answers: NDQ_001603

answers: most other nations

answers: NDQ_001605

answers: Geologic maps

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic

answers: NDQ_001611

answers: Cassini maps

answers: NDQ_001613

answers: the side of the circle with the higher elevation

answers: NDQ_001614

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answers: NDQ_001618

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answers: 1 km

text: The African superswell is a region including the Southern and Eastern African plateaus and the Southeastern Atlantic basin where exceptional tectonic uplift has occurred, resulting in terrain much higher than its surroundings. The average elevation of cratons is about 400–500 meters above sea level. Southern Africa exceeds these elevations by more than 500 m, and stands at over 1 km above sea level. The Southern and Eastern African plateaus show similar uplift histories, allowing them to be considered as one topographic unit. When considered this way, the swell is one of the largest topographic anomalies observed on any continent, and spans an area of over 10 million km. Uplift extends beyond the continents into the Atlantic ocean, where extremely shallow ocean depths are visible through bathymetric survey.  The region can indeed be considered as one large swell because the bathymetric anomaly to the southwest of Africa is on the same order as the topographic anomaly of the plateaus (approximately 500 m).

text: The African superswell is a region including the Southern and

text: Eastern African

text: plateaus and the Southeastern Atlantic basin where exceptional

text: tectonic uplift

text: has occurred, resulting in

text: terrain

text: much higher than its surroundings. The average elevation of

text: craton

text: s is about 400–500 meters above sea level. Southern Africa exceeds these elevations by more than 500 m, and stands at over 1 km above

text: sea level

text: . The Southern and Eastern African plateaus show similar uplift histories, allowing them to be considered as one

text: topographic

text: unit. When considered this way, the swell is one of the largest topographic anomalies observed on any continent, and spans an area of over 10 million km. Uplift extends beyond the continents into the Atlantic ocean, where extremely shallow ocean depths are visible through

text: bathymetric

text: survey.  The region can indeed be considered as one large swell because the bathymetric anomaly to the southwest of Africa is on the same order as the topographic anomaly of the plateaus (approximately 500 m).

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answers: The African superswell

answers: NDQ_001587

answers: Uplift extends beyond the continents

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: The average elevation of cratons is about 400–500 meters above sea level

answers: NDQ_001590

answers: 500 m

answers: NDQ_001591

answers: terrain much higher than its surroundings

answers: NDQ_001592

answers: bathymetric survey

answers: NDQ_001593

answers: The average elevation of cratons is about 400–500 meters

answers: NDQ_001594

answers: extremely shallow ocean depths

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Southeastern Atlantic basin

answers: NDQ_001598

answers: topographic anomaly

answers: NDQ_001600

answers: Southern and Eastern African

answers: NDQ_001603

answers: It is not possible to tell

answers: NDQ_001605

answers: Southern and Eastern African plateaus

answers: NDQ_001606

answers: The African superswell

answers: NDQ_001608

answers: topographic unit

answers: NDQ_001611

answers: The Southern and Eastern African plateaus show similar uplift histories

answers: NDQ_001613

answers: Southern Africa

answers: NDQ_001614

answers: The average elevation of cratons

answers: NDQ_001618

answers: topographic unit

answers: NDQ_001619

answers: bathymetric survey

answers: NDQ_001620

answers: The African superswell

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: topographic unit

answers: NDQ_001623

answers: topographic anomaly

answers: NDQ_001624

answers: The African superswell

answers: NDQ_001625

answers: 500 m

text: The National Map is a significant contribution to the National Spatial Data Infrastructure (NSDI) and currently is being transformed to better serve the geospatial community by providing high quality, integrated geospatial data and improved products and services including new generation digital topographic maps. In addition, the National Map is foundational to implementation of the U.S. Department of the Interior (DOI) Geospatial Modernization Blueprint.

text: The National Map is a significant contribution to the

text: National Spatial Data Infrastructure

text: (NSDI) and currently is being transformed to better serve the

text: geospatial

text: community by providing high quality, integrated geospatial data and improved products and services including new generation digital

text: topographic map

text: s. In addition, the National Map is foundational to implementation of the

entity_name: United States Department of the Interior

text: U.S. Department of the Interior

text: (DOI) Geospatial Modernization Blueprint.

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answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: The National Map

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: National Map is a significant contribution

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: topographic

answers: NDQ_001592

answers: National Spatial Data Infrastructure (NSDI)

answers: NDQ_001593

answers: topographic maps

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: topographic maps

answers: NDQ_001598

answers: topographic maps

answers: NDQ_001600

answers: National Map

answers: NDQ_001603

answers: The National Map

answers: NDQ_001605

answers: The National Map

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic maps

answers: NDQ_001611

answers: topographic

answers: NDQ_001613

answers: The National Map

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: National Map

answers: NDQ_001619

answers: topographic

answers: NDQ_001620

answers: topographic

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: National Map

answers: NDQ_001623

answers: topographic

answers: NDQ_001624

answers: National Map

answers: NDQ_001625

answers: National Map

text: The Geographic Names Information System lists two sets of coordinates for the Swalley Canal. One is at   in the Bend quadrant of the United States Geological Survey topographic map. The other is at  in the Tumalo quadrant.

text: The

text: Geographic Names Information System

text: lists two sets of coordinates for the Swalley Canal. One is at   in the Bend quadrant of the

text: United States Geological Survey

text: topographic map. The other is at  in the Tumalo quadrant.

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text: As described above, topographic maps occur when spatial relationships are maintained between neuronal populations and their target fields in another tissue. This is a major feature of nervous system organization, particular in sensory systems. The neurobiologist Roger Sperry proposed a prescient model for topographic mapping mediated by what he called molecular "tags." The relative amounts of these tags would vary in gradients across both tissues. We now think of these tags as ligands (cues) and their axonal receptors. Perhaps the best understood class of tags are the Ephrin ligands and their receptors, the Ephs.

text: As described above, topographic maps occur when spatial relationships are maintained between neuronal populations and their target fields in another tissue. This is a major feature of nervous system organization, particular in sensory systems. The neurobiologist

text: Roger Sperry

text: proposed a prescient model for topographic mapping mediated by what he called molecular "tags." The relative amounts of these tags would vary in gradients across both tissues. We now think of these tags as ligands (cues) and their axonal receptors. Perhaps the best understood class of tags are the Ephrin ligands and their receptors, the Ephs.

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answers: NDQ_001611

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answers: NDQ_001613

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answers: NDQ_001614

answers: topographic maps

answers: NDQ_001618

answers: target fields

answers: NDQ_001619

answers: topographic

answers: NDQ_001620

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answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: target fields

answers: NDQ_001623

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answers: NDQ_001624

answers: target fields

answers: NDQ_001625

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text: , at each material point in the body at that time. However, numerical analysis and analytical methods allow only for the calculation of the stress tensor at a certain number of discrete material points. To graphically represent in two dimensions this partial picture of the stress field different sets of contour lines can be used:

text: , at each material point in the body at that time. However, numerical analysis and analytical methods allow only for the calculation of the stress tensor at a certain number of discrete material points. To graphically represent in two dimensions this partial picture of the stress field different sets of

text: contour lines

text: can be used:

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answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001592

answers: calculation of the stress tensor

answers: NDQ_001593

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answers: NDQ_001613

answers: To graphically represent in two dimensions this partial picture of the stress field

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text: The ship was contracted to conduct a bathymetric survey in the southern Indian Ocean during the search for Malaysia Airlines Flight 370. The survey was needed to produce a bathymetric map of the sea floor of the search area, which was previously poorly mapped and largely uncharted and mountainous, before a phase of the search using a towed side-scan sonar vehicle and autonomous underwater vehicles which need to operate close to the seafloor. In August, it was announced that Fugro had been awarded the contract for that phase of the search and that Fugro Equator and sister ship Fugro Discovery would conduct the search (with some assistance from Malaysian & Chinese naval vessels).

text: The ship was contracted to conduct a bathymetric survey in the southern Indian Ocean during the search for

text: Malaysia Airlines Flight 370

text: . The survey was needed to produce a bathymetric map of the sea floor of the search area, which was previously poorly mapped and largely uncharted and mountainous, before a phase of the search using a towed side-scan sonar vehicle and

text: autonomous underwater vehicle

text: s which need to operate close to the seafloor. In August, it was announced that Fugro had been awarded the contract for that phase of the search and that Fugro Equator and sister ship Fugro Discovery would conduct the search (with some assistance from Malaysian & Chinese naval vessels).

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answers: 4

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answers: NDQ_001624

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answers: NDQ_001625

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answers: NDQ_001586

answers: bathymetric

answers: NDQ_001587

answers: is needed to operate close to the seafloor

answers: NDQ_001588

answers: bathymetric

answers: NDQ_001589

answers: uncharted and mountainous

answers: NDQ_001590

answers: bathymetric

answers: NDQ_001591

answers: mountainous

answers: NDQ_001592

answers: operate close to the seafloor

answers: NDQ_001593

answers: mountainous

answers: NDQ_001594

answers: bathymetric map

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: bathymetric

answers: NDQ_001598

answers: mountainous

answers: NDQ_001600

answers: mountainous

answers: NDQ_001603

answers: uncharted

answers: NDQ_001605

answers: bathymetric

answers: NDQ_001606

answers: bathymetric

answers: NDQ_001608

answers: bathymetric map

answers: NDQ_001611

answers: mountainous

answers: NDQ_001613

answers: Fugro Equator

answers: NDQ_001614

answers: bathymetric

answers: NDQ_001618

answers: mountainous

answers: NDQ_001619

answers: bathymetric

answers: NDQ_001620

answers: bathymetric

answers: NDQ_001621

answers: bathymetric

answers: NDQ_001622

answers: mountainous

answers: NDQ_001623

answers: bathymetric

answers: NDQ_001624

answers: mountainous

answers: NDQ_001625

answers: bathymetric

text: By noting the corresponding compass vector, walking along the contour one can line up a hand held compass aligning the expected direction, and eye-balling the line of contour's estimated level, move up or down along the bearing faster— to closely locate a desired point (planned point) along the hillside. Pragmatically, this can be 'good enough' for rough project landscaping, such as timber clear cutting the work site of a structure like a bridge abutment or connecting ramps. The approximation can then be refined by transit and other surveyor tools to construct on target.

text: By noting the corresponding compass vector, walking along the contour one can line up a hand held compass aligning the expected direction, and eye-balling the line of contour's estimated level, move up or down along the bearing faster— to closely locate a desired point (planned point) along the hillside. Pragmatically, this can be 'good enough' for rough project landscaping, such as timber clear cutting the work site of a structure like a

text: bridge

text: abutment

text: or connecting ramps. The approximation can then be refined by transit and other surveyor tools to construct on target.

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answers: NDQ_001624

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answers: NDQ_001625

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answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: can be refined by transit

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: one can line up a hand held compass aligning the expected direction

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: expected direction

answers: NDQ_001592

answers: locate a desired point

answers: NDQ_001593

answers: hillside

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: direction

answers: NDQ_001598

answers: contour

answers: NDQ_001600

answers: hillside

answers: NDQ_001603

answers: Pragmatically

answers: NDQ_001605

answers: contour

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: By noting the corresponding compass vector

answers: NDQ_001611

answers: contour

answers: NDQ_001613

answers: contour

answers: NDQ_001614

answers: vertical

answers: NDQ_001618

answers: hillside

answers: NDQ_001619

answers: contour

answers: NDQ_001620

answers: bearing

answers: NDQ_001621

answers: contour

answers: NDQ_001622

answers: hillside

answers: NDQ_001623

answers: contour

answers: NDQ_001624

answers: hillside

answers: NDQ_001625

answers: hillside

text: Obsolete maps, especially of the 19th century, are often named Topographic Atlases, because their small-sized sheets were also bound into atlases.  An example of such a map series is the Topographic Atlas of the Kingdom of Hanover and the Duchy of Brunswick.

text: Obsolete maps, especially of the 19th century, are often named Topographic Atlases, because their small-sized sheets were also bound into atlases.  An example of such a map series is the

text: Topographic Atlas of the Kingdom of Hanover and the Duchy of Brunswick

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text: The fringes in the image above are out-of-plane fringes. The plate has been rotated about a vertical axis and the fringes represent contours of constant displacement.  The contour interval is about 0.3μm since a He-Ne laser was used in the system. As with many interferometric techniques, it is not possible to identify the zero-order fringe without additional information from the system.

text: The fringes in the image above are out-of-plane fringes. The plate has been rotated about a vertical axis and the fringes represent contours of constant displacement.  The contour interval is about 0.3μm since a

text: He-Ne laser

text: was used in the system. As with many interferometric techniques, it is not possible to identify the zero-order fringe without additional information from the system.

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text: While High Peak is not among the highest Catskill peaks, because of its distance from other major peaks it ranks fourth in topographic prominence, after Slide Mountain, Hunter Mountain and Black Dome. High Peak's summit rises 1,775 feet (541 m) from the lowest elevation contour line that encircles it.

text: While High Peak is not among the highest Catskill peaks, because of its distance from other major peaks it ranks fourth in

text: topographic prominence

text: , after

entity_name: Slide Mountain (Ulster County, New York)

text: Slide Mountain

text: Hunter Mountain

text: and

text: Black Dome

text: . High Peak's summit rises 1,775 feet (541 m) from the lowest elevation

text: contour line

text: that encircles it.

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text: The disastrous flood of the Fraser River in 1948 nearly changed the Clearwater River and Wells Gray Park forever. In November 1947, the Federal Minister of Public Works proposed the creation of a joint federal-provincial committee to study the Fraser’s water resources. The flood made this project all the more urgent and, in late 1948, the Dominion-Provincial Board, Fraser River Basin was established to report on power generation, fisheries, flood control, water supply and recreation. Between 1949 and 1954, the committee of ten collected basic data and filled in the gaps in other government studies. No report was produced, but, in 1953, 12 detailed maps of the Clearwater River between Hemp Creek and the North Thompson River were published. These had a scale of 1 inch = 500 feet and a contour interval of 20 feet. Over 50 years later, these sheets are still the most detailed and accurate topographic maps available of the lower Clearwater, although they are out-of-date regarding human developments.

text: The disastrous

text: flood

text: of the

text: Fraser River

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answers: 12 detailed maps of the Clearwater River

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text: The biological and geochemical manifestations of seepage leads to distinct bathymetrical features including positive relief mounds, pinnacles, mud volcanoes and negative relief pockmarks. These features can be detected by multibeam sonar and then sampled by navigated piston coring. Spec and proprietary multibeam seep mapping and core geochemistry by Texas A&M University’s Geochemical & Environmental Research Group and later TDI Brooks demonstrated thermogenic charge in deepwater Angola and deepwater Nigeria leading to an aggressive exploration program by a number of oil companies and subsequent discoveries. The emphasis on, and marketplace acceptance of, multibeam mapping combined with navigated coring as an improvement over grid-based approaches to geochemical exploration is attributed to AOA Geophysics Inc.

text: The biological and geochemical manifestations of seepage leads to distinct bathymetrical features including positive relief mounds, pinnacles,

text: mud volcano

text: es and negative relief

text: pockmark

text: s. These features can be detected by multibeam sonar and then sampled by navigated piston coring. Spec and proprietary multibeam

text: seep

text: mapping and core geochemistry by Texas A&M University’s Geochemical & Environmental Research Group and later TDI Brooks demonstrated thermogenic charge in deepwater

text: Angola

text: and deepwater

text: Nigeria

text: leading to an aggressive exploration program by a number of oil companies and subsequent discoveries. The emphasis on, and marketplace acceptance of, multibeam mapping combined with navigated coring as an improvement over grid-based approaches to geochemical exploration is attributed to AOA Geophysics Inc.

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answers: NDQ_001587

answers: negative relief pockmarks

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: grid-based approaches

answers: NDQ_001590

answers: relief

answers: NDQ_001591

answers: mud volcanoes

answers: NDQ_001592

answers: navigated piston coring

answers: NDQ_001593

answers: relief

answers: NDQ_001594

answers: bathymetrical features

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001598

answers: relief

answers: NDQ_001600

answers: relief pockmarks

answers: NDQ_001603

answers: marketplace acceptance

answers: NDQ_001605

answers: relief pockmarks

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

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answers: NDQ_001611

answers: pinnacles

answers: NDQ_001613

answers: relief pockmarks

answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

answers: bathymetric

answers: NDQ_001620

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answers: NDQ_001621

answers: relief

answers: NDQ_001622

answers: positive relief mounds

answers: NDQ_001623

answers: relief

answers: NDQ_001624

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answers: NDQ_001625

answers: positive relief mounds

text: where the contour must not enclose any of the points

text: where the contour must not enclose any of the points

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answers: NDQ_001586

answers: contour must not enclose any of the points

answers: NDQ_001587

answers: does not enclose any points

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: contour must not enclose any of the points

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: enclose any of the points

answers: NDQ_001592

answers: enclose any of the points

answers: NDQ_001593

answers: the slope of the land

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: enclose any of the points

answers: NDQ_001598

answers: contour

answers: NDQ_001600

answers: a plain or plateau

answers: NDQ_001603

answers: not enclose any of the points

answers: NDQ_001605

answers: color of the rocks

answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

answers: the contour must not enclose any of the points

answers: NDQ_001611

answers: the contour must not enclose any of the points

answers: NDQ_001613

answers: on the side of the circle with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: contour

answers: NDQ_001619

answers: contour

answers: NDQ_001620

answers: contour lines

answers: NDQ_001621

answers: contour

answers: NDQ_001622

answers: contour

answers: NDQ_001623

answers: contour

answers: NDQ_001624

answers: contour

answers: NDQ_001625

answers: the contour must not enclose

text: A topographical map of Auckland which Kinder drew is now held in the Hocken Library in Dunedin.

text: A topographical map of Auckland which Kinder drew is now held in the

text: Hocken Library

text: in

text: Dunedin

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text: By the 17th century, private map collections were often the basis for public map collections. As early as 1571, for example, the Court Library in Munich, Bavaria, (now the Bavarian State Library) became the owner of the Fugger collection.  In 1823, the British Museum in London acquired the King's Library, which had been inherited and greatly enlarged by George III of the United Kingdom, and donated to the Museum by his heir, George IV of the United Kingdom.  The King's Library included a collection of approximately 50,000 maps, plans and views, which are now housed at the British Library and known as the King's Topographical Collection.

text: By the 17th century,

text: private

text: map collections were often the basis for public map collections. As early as 1571, for example, the Court Library in

text: Munich

text: Bavaria

text: , (now the

text: Bavarian State Library

text: ) became the owner of the

text: Fugger

text: collection.  In 1823, the

text: British Museum

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text: London

text: acquired the

text: King's Library

text: , which had been inherited and greatly enlarged by

text: George III of the United Kingdom

text: , and donated to the Museum by his heir,

text: George IV of the United Kingdom

text: .  The King's Library included a collection of approximately 50,000 maps, plans and views, which are now housed at the

text: British Library

text: and known as the King's Topographical Collection.

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answers: approximately 50,000

text: Some high end keyboards such as the Kinesis Advantage contoured keyboard allow users total flexibility to reprogram keyboard mappings at the hardware level.

text: Some high end keyboards such as the

text: Kinesis Advantage contoured keyboard

text: allow users total flexibility to reprogram keyboard mappings at the hardware level.

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text: Wilson Ridge () is a prominent razorback ridge 6 nautical miles (11 km) north of Mount Harding in the Grove Mountains. Mapped by ANARE (Australian National Antarctic Research Expeditions) from air photos, 1956-60. Named by Antarctic Names Committee of Australia (ANCA) for R.R. Wilson, topographic draftsman, Division of National Mapping, Australian Dept. of National Development, who has contributed substantially to the compilation of Antarctic maps.

text: Wilson Ridge () is a prominent razorback ridge 6 nautical miles (11 km) north of

text: Mount Harding

text: in the

text: Grove Mountains

text: . Mapped by ANARE (

entity_name: Australian National Antarctic Research Expeditions

text: Australian National Antarctic Research Expeditions

text: ) from air photos, 1956-60. Named by

entity_name: Australian Antarctic Names and Medals Committee

text: Antarctic Names Committee of Australia

text: (ANCA) for

text: R.R. Wilson

text: , topographic draftsman, Division of

text: National Mapping

text: Australian Dept

text: . of

text: National Development

text: , who has contributed substantially to the compilation of Antarctic maps.

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answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: Wilson Ridge

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Antarctic names Committee of Australia

answers: NDQ_001590

answers: nautical miles

answers: NDQ_001591

answers: razorback ridge

answers: NDQ_001592

answers: Named

answers: NDQ_001593

answers: razorback ridge

answers: NDQ_001594

answers: nautical miles

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: 6 nautical miles

answers: NDQ_001598

answers: razorback ridge

answers: NDQ_001600

answers: razorback ridge

answers: NDQ_001603

answers: no

answers: NDQ_001605

answers: Mapping

answers: NDQ_001606

answers: 6 nautical miles

answers: NDQ_001608

answers: topographic

answers: NDQ_001611

answers: razorback ridge

answers: NDQ_001613

answers: razorback ridge

answers: NDQ_001614

answers: nautical miles

answers: NDQ_001618

answers: razorback ridge

answers: NDQ_001619

answers: nautical miles

answers: NDQ_001620

answers: razorback

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: razorback ridge

answers: NDQ_001623

answers: ridge

answers: NDQ_001624

answers: razorback ridge

answers: NDQ_001625

answers: 11 km

text: Let Δh be the uniform interval of altitude between contours on the contour map, and let Δx be the distance between two contours.  Then

text: Let Δh be the uniform interval of altitude between contours on the contour map, and let Δx be the distance between two contours.  Then

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answers: 4

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answers: 4

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answers: NDQ_001593

answers: 4

answers: NDQ_001594

answers: 4

answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 0

answers: NDQ_001598

answers: 0

answers: NDQ_001600

answers: 0

answers: NDQ_001603

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answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 4

answers: NDQ_001608

answers: 4

answers: NDQ_001611

answers: 0

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 4

answers: NDQ_001618

answers: 0

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 0

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: h is the uniform interval of altitude between contours

answers: NDQ_001587

answers: h is the uniform interval of altitude between contours

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: x is the distance between two contours

answers: NDQ_001590

answers: h = altitude

answers: NDQ_001591

answers: altitude

answers: NDQ_001592

answers: x be the distance between two contours

answers: NDQ_001593

answers: h is the slope of the land.

answers: NDQ_001594

answers: h is the uniform interval of altitude

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: x is the distance between two contours.

answers: NDQ_001598

answers: h is the uniform interval of altitude.

answers: NDQ_001600

answers: h represents a plain or plateau.

answers: NDQ_001603

answers: Contour maps are used by geologists.

answers: NDQ_001605

answers: h is the uniform interval of altitude.

answers: NDQ_001606

answers: x is the distance between two contours.

answers: NDQ_001608

answers: h is the uniform interval of altitude between contours.

answers: NDQ_001611

answers: h is the uniform interval of altitude between contours

answers: NDQ_001613

answers: The hatch marks are drawn on the side with the higher elevation.

answers: NDQ_001614

answers: Topographic maps cannot show horizontal distances.

answers: NDQ_001618

answers: contour map

answers: NDQ_001619

answers: contour map

answers: NDQ_001620

answers: x

answers: NDQ_001621

answers: contour map

answers: NDQ_001622

answers: contour map

answers: NDQ_001623

answers: contours

answers: NDQ_001624

answers: contours

answers: NDQ_001625

answers: h

text: The National Wetlands Inventory (NWI) was established by the United States Fish and Wildlife Service (FWS) to conduct a nationwide inventory of U.S. wetlands to provide biologists and others with information on the distribution and type of wetlands to aid in conservation efforts. To do this, the NWI developed a wetland classification system (Cowardin et al. 1979) that is now the official FWS wetland classification system and the Federal standard for wetland classification (adopted by the Federal Geographic Data Committee on July 29, 1996: 61 Federal Register 39465). The NWI also developed techniques for mapping and recording the inventory findings. The NWI relies on trained image analysts to identify and classify wetlands and deepwater habitats from aerial imagery. NWI started mapping wetlands at a small scale (1:250,000 map which covers an area the size of 128-1:24,000 USGS topographic maps or approximately 7,400 square miles). Eventually, large-scale (1:24K scale) maps became the standard product delivered by NWI. As computerized mapping and geospatial technology evolved,  NWI discontinued production of paper maps in favor of distributing  data via online "mapping tools" where information can be viewed and downloaded. Today, FWS serves its data  via an on-line data discovery "Wetlands Mapper". GIS users can access wetlands data through an online wetland mapping service or download data for various applications (maps, data analyses, and reports). The techniques used by  NWI have recently been adopted by the Federal Geographic Data Committee as the federal wetland mapping standard (FGDC Wetlands Subcommittee 2009). This standard applies to all federal grants involving wetland mapping to insure the data  can be added to the Wetlands Layer of the National Spatial Data Infrastructure. NWI also produces national wetlands status and trends reports required by the United States Congress.

text: The National Wetlands Inventory (NWI) was established by the

text: United States Fish and Wildlife Service

text: (FWS) to conduct a nationwide inventory of U.S. wetlands to provide biologists and others with information on the distribution and type of wetlands to aid in conservation efforts. To do this, the NWI developed a wetland classification system (Cowardin et al. 1979) that is now the official FWS wetland classification system and the Federal standard for wetland classification (adopted by the

text: Federal Geographic Data Committee

text: United States Congress

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answers: the data can be added to the Wetlands Layer of the National Spatial Data Infrastructure

answers: NDQ_001590

answers: 1:24,000

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answers: deepwater habitats

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text: Generally contour plots of 2D spectra are oriented with rising axes from left to right and top to down. Other orientations are possible, but interpretation has to be adapted accordingly.

text: Generally contour plots of 2D spectra are oriented with rising axes from left to right and top to down. Other orientations are possible, but interpretation has to be adapted accordingly.

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answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001594

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answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001608

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001620

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text: In 1910, the Map Reproduction Plant was given warehouse space at Ft. McNair, to accommodate the map reproduction unit of the Corps of Engineers. Ultimately named the Central Map Reproduction unit, it incorporated a lithographic school and 18 assigned military personnel. After World War I, this would be renamed the Engineer Reproduction Plant. The ERP was noted for experimentation on cartographic and photolithographic processes and media. They also experimentation in aerial photogrammetry.A number of US Geological Survey employees were assigned to the US Army Corps of Engineers 29th Engineers, a map organization, during World War I. Major G.S. Smith commanded part of the 29th Engineers, a map making and topographical unit, with 53 officers and 146 men transferred from the US Geological Survey. Thirteen additional USGS topographers were assigned to the Coast Artillery of the US Army as "orienteur officers." When the 2nd Brigade of Coast Artillery was formed, the military made a similar request for more USGS personnel, but the order was denied as these men were needed for the US Army Corps of Engineers.

text: In 1910, the

text: Map Reproduction Plant

text: was given warehouse space at

text: Ft. McNair

text: , to accommodate the map reproduction unit of the Corps of Engineers. Ultimately named the

text: Central Map Reproduction

text: unit, it incorporated a

text: lithographic

text: school and 18 assigned military personnel. After World War I, this would be renamed the

text: Engineer Reproduction Plant

text: . The ERP was noted for experimentation on cartographic and

text: photolithographic processes

text: and media. They also experimentation in aerial

text: photogrammetry

text: .A number of

text: US Geological Survey

text: employees were assigned to the US

text: Army Corps of Engineers

text: 29th Engineers, a map organization, during World War I. Major

text: G.S. Smith

text: commanded part of the 29th Engineers, a map making and topographical unit, with 53 officers and 146 men transferred from the US Geological Survey. Thirteen additional USGS

text: topographers

text: were assigned to the

text: Coast Artillery of the US Army

text: as "orienteur officers." When the

text: 2nd Brigade of Coast Artillery

text: was formed, the military made a similar request for more USGS personnel, but the order was denied as these men were needed for the US Army Corps of Engineers.

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answers: NDQ_001587

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answers: NDQ_001588

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answers: NDQ_001589

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answers: NDQ_001590

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answers: NDQ_001591

answers: Engineers

answers: NDQ_001592

answers: orienteur officers

answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

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answers: NDQ_001605

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answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

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answers: NDQ_001611

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

answers: elevation

answers: NDQ_001621

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answers: NDQ_001622

answers: topography

answers: NDQ_001623

answers: Aerial

answers: NDQ_001624

answers: orienteur

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text: The South Burying Ground occupies a roughly rectangular  on the west side of Winchester Street, a short way south of Massachusetts Route 9 in Newton Highlands.  The cemetery's primary topographical features are two knolls, which flank the main entrance.  The street-facing front and parts of the sides of the cemetery are lined by a stone wall that is probably of 19th century origin.  A chain link fence is mounted on the wall, and encircles the rest of the property.  The main entrance is secured by a chain-link gate.  The cemetery has no paved lanes, although early 20th century maps show a rectilinear grid of them.

text: The South Burying Ground occupies a roughly rectangular  on the west side of Winchester Street, a short way south of

text: Massachusetts Route 9

text: in Newton Highlands.  The cemetery's primary topographical features are two knolls, which flank the main entrance.  The street-facing front and parts of the sides of the cemetery are lined by a stone wall that is probably of 19th century origin.  A chain link fence is mounted on the wall, and encircles the rest of the property.  The main entrance is secured by a chain-link gate.  The cemetery has no paved lanes, although early 20th century maps show a rectilinear grid of them.

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answers: knolls

answers: NDQ_001587

answers: The cemetery's primary topographical features are two knolls

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: The cemetery has no paved lanes

answers: NDQ_001590

answers: a rectilinear grid

answers: NDQ_001591

answers: a rectilinear grid

answers: NDQ_001592

answers: paved lanes

answers: NDQ_001593

answers: a rectilinear grid

answers: NDQ_001594

answers: a rectilinear grid

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: west

answers: NDQ_001598

answers: knolls

answers: NDQ_001600

answers: knolls

answers: NDQ_001603

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answers: NDQ_001605

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answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001611

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answers: NDQ_001613

answers: knolls

answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

answers: knolls

answers: NDQ_001621

answers: topographical

answers: NDQ_001622

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answers: NDQ_001623

answers: rectilinear

answers: NDQ_001624

answers: a rectilinear grid

answers: NDQ_001625

answers: a short way

text: Charles Logasa was born in Davenport, Iowa, United States, on  July 14, 1883 to Sephardic Jewish parents and Ukrainian immigrants. His father was Seth Moses Logasa. He had two sisters, Jeanie Deana Bogen née Logasa, and Hannah Logasa He came with his parents to Omaha, Nebraska between the ages of three and five years old.   As a boy he became a pupil of J. Laurie Wallace who was a pupil of Thomas Eakins. As a young man he studied drafting and engineering and around 1905 was employed as a draftsman for the City of Omaha in the Engineer's Office drawing maps.  At the age of 22 he turned to oil painting. About 1910 or 1911 he left Omaha. He entered the service of the United States Geological Survey as a topographic draftsman in Washington D. C.  Logasa continued his art education with Messer and Brooke as a part-time student at the Corcoran College of Art and Design. In 1913 he took a year's leave of absence from his duties as topographic draftsman for the United States Geological Survey and went to Paris where he entered the Acadamie Julien studying under Paul Laurens.

text: Charles Logasa was born in Davenport, Iowa, United States, on  July 14, 1883 to

text: Sephardic

text: Jewish parents and Ukrainian immigrants. His father was Seth Moses Logasa. He had two sisters, Jeanie Deana Bogen née Logasa, and

text: Hannah Logasa

text: He came with his parents to Omaha, Nebraska between the ages of three and five years old.   As a boy he became a pupil of

text: J. Laurie Wallace

text: who was a pupil of

text: Thomas Eakins

text: . As a young man he studied drafting and engineering and around 1905 was employed as a draftsman for the City of Omaha in the Engineer's Office drawing maps.  At the age of 22 he turned to oil painting. About 1910 or 1911 he left Omaha. He entered the service of the United States Geological Survey as a topographic draftsman in Washington D. C.  Logasa continued his art education with Messer and Brooke as a part-time student at the

text: Corcoran College of Art and Design

text: . In 1913 he took a year's leave of absence from his duties as topographic draftsman for the United States Geological Survey and went to Paris where he entered the

text: Acadamie Julien

text: studying under

text: Paul Laurens

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text: The first phase of the programme was set up in 2006, with an initial grant of £7.2 million from the Department for Environment, Food and Rural Affairs (DEFRA). The funding was split into two with £4.1 million used by Teignbridge to deliver, Bathymetric and Topographic, Hydrographic surveys and £3.1 million managed by the Environment Agency to deliver Aerial photography, LiDAR and Ecological mapping. Phase 2 of the programme commenced in 2011 with 100% DEFRA funding, and will run until 2016. Phase 2 of the Programme is solely managed by Teignbridge District Council.

text: The first phase of the programme was set up in 2006, with an initial grant of £7.2 million from the

entity_name: Department for Environment, Food and Rural Affairs

text: Department for Environment, Food and Rural Affairs

text: (DEFRA). The funding was split into two with £4.1 million used by

text: Teignbridge

text: to deliver,

text: Bathymetric

text: and

text: Topographic

text: Hydrographic surveys

text: and £3.1 million managed by the

text: Environment Agency

text: to deliver

text: Aerial photography

text: LiDAR

text: and Ecological mapping. Phase 2 of the programme commenced in 2011 with 100% DEFRA funding, and will run until 2016. Phase 2 of the Programme is solely managed by Teignbridge District Council.

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answers: NDQ_001624

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answers: NDQ_001625

answers: LiDAR

text: A contour line (also isoline, isopleth, or isarithm) of a function of two variables is a  curve along which the function has a constant value. It is a cross-section of the three-dimensional graph of the function f(x, y) parallel to the x, y plane. In cartography, a contour line (often just called a "contour") joins points of equal elevation (height) above a given level, such as mean sea level. A contour map is a map illustrated with contour lines, for example a topographic map, which thus shows valleys and hills, and the steepness of slopes. The contour interval of a contour map is the difference in elevation between successive contour lines.

text: A contour line (also isoline, isopleth, or isarithm) of a

text: function

text: of two variables is a

text: curve

text: along which the function has a constant value. It is a

text: cross-section

text: of the

text: three-dimensional graph

text: of the function f(x, y) parallel to the x, y plane. In

text: cartography

text: , a contour line (often just called a "contour") joins points of equal

text: elevation

text: (height) above a given level, such as

text: mean sea level

text: . A contour map is a

text: map

text: illustrated with contour lines, for example a

text: topographic map

text: , which thus shows valleys and hills, and the steepness of slopes. The contour interval of a contour map is the difference in elevation between successive contour lines.

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answers: NDQ_001624

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answers: NDQ_001625

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answers: NDQ_001586

answers: The contour interval

answers: NDQ_001587

answers: isoline

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: shows valleys and hills, and the steepness of slopes

answers: NDQ_001590

answers: difference in elevation

answers: NDQ_001591

answers: valleys and hills

answers: NDQ_001592

answers: the steepness of slopes

answers: NDQ_001593

answers: A contour map

answers: NDQ_001594

answers: mean sea level

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: valleys and hills

answers: NDQ_001598

answers: slopes

answers: NDQ_001600

answers: valleys

answers: NDQ_001603

answers: In cartography

answers: NDQ_001605

answers: contour lines

answers: NDQ_001606

answers: The contour interval

answers: NDQ_001608

answers: f(x, y) parallel to the x, y plane

answers: NDQ_001611

answers: contour map

answers: NDQ_001613

answers: contour lines

answers: NDQ_001614

answers: hills

answers: NDQ_001618

answers: valleys and hills

answers: NDQ_001619

answers: sea level

answers: NDQ_001620

answers: The contour interval

answers: NDQ_001621

answers: topographic map

answers: NDQ_001622

answers: valleys

answers: NDQ_001623

answers: contour

answers: NDQ_001624

answers: valleys

answers: NDQ_001625

answers: difference in elevation

text: From 1870, a map series in the 1:25,000 scale of the original Dufour Map images was published under the official name Topographic Atlas of Switzerland (German: Topographischer Atlas der Schweiz), and also known as the Siegfried Atlas or Siegfried Map (German: Siegfriedkarte; French: Carte Siegfried).

text: From 1870, a map series in the 1:25,000 scale of the original Dufour Map images was published under the official name

text: Topographic Atlas of Switzerland

text: (German: Topographischer Atlas der Schweiz), and also known as the Siegfried Atlas or

text: Siegfried Map

text: (German: Siegfriedkarte; French: Carte Siegfried).

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answers: 1:25,000 scale

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answers: NDQ_001586

answers: Topographic Atlas

answers: NDQ_001587

answers: 1:25,000 scale

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: 1:25,000 scale

answers: NDQ_001590

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answers: NDQ_001591

answers: Topographic

answers: NDQ_001592

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answers: 1:25,000 scale

answers: NDQ_001598

answers: 1:25,000 scale

answers: NDQ_001600

answers: Topographic Atlas

answers: NDQ_001603

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answers: NDQ_001605

answers: Topographic Atlas

answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

answers: Topographic

answers: NDQ_001611

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answers: NDQ_001613

answers: Topographic Atlas of Switzerland

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answers: NDQ_001621

answers: 1:25,000 scale

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answers: Topographic

answers: NDQ_001623

answers: 1:25,000 scale

answers: NDQ_001624

answers: Topographic

answers: NDQ_001625

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text: Finally, many height indications on these maps are from quite old measurements, while glacier and firn melt has decreased the height of both peaks and key cols, sometimes quite dramatically. For example, in 1930, glacier-capped Cima Tosa was the highest mountain of the Brenta Dolomites at 3,173 m, but now is around 3,140 m high and some 10 m lower than its rocky neighbor Cima Brenta (3,151 m). Most maps and guides still report Cima Tosa's old height. On the other hand, in the 1930s, when the current Italian 1:25.000 topographic map of the region was created, the Passo del Vannino, northwest of the Ofenhorn, was covered by the Lebendun glacier and was measured to be 2,754 m, while the much more recent Swisstopo map shows it to be bare and 2,717 m high. This is the key col for Corno di Ban (3,028 m), which, thanks to the retreat of the glacier, now appears on the list with a prominence of 311 m.

text: Finally, many height indications on these maps are from quite old measurements, while glacier and

text: firn

text: melt has decreased the height of both peaks and key cols, sometimes quite dramatically. For example, in 1930, glacier-capped

text: Cima Tosa

text: was the highest mountain of the

text: Brenta Dolomites

text: at 3,173 m, but now is around 3,140 m high and some 10 m lower than its rocky neighbor

text: Cima Brenta

text: (3,151 m). Most maps and guides still report Cima Tosa's old height. On the other hand, in the 1930s, when the current Italian 1:25.000 topographic map of the region was created, the Passo del Vannino, northwest of the

text: Ofenhorn

text: , was covered by the Lebendun glacier and was measured to be 2,754 m, while the much more recent Swisstopo map shows it to be bare and 2,717 m high. This is the key col for

text: Corno di Ban

text: (3,028 m), which, thanks to the retreat of the glacier, now appears on the list with a prominence of 311 m.

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answers: many height indications on these maps are from quite old measurements

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answers: height indications

answers: NDQ_001587

answers: Passo del Vannino

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: Most maps and guides still report Cima Tosa's old height

answers: NDQ_001590

answers: Swisstopo

answers: NDQ_001591

answers: old measurements

answers: NDQ_001592

answers: report Cima Tosa's old height

answers: NDQ_001593

answers: Swisstopo map

answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001603

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answers: Swisstopo

answers: NDQ_001606

answers: The difference between two contour lines

answers: NDQ_001608

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answers: 1:25.000

text: For 113 years of colonisation after the arrival of the First Fleet, much of the mapping of Australia, mainly for exploration, settlement and development, was supervised and conducted by naval and military officers. These officers included the well known explorers and surveyors: Captain Matthew Flinders, Royal Navy; Lieutenant William Dawes (Royal Marines officer), (New South Wales); Lieutenant Philip Parker King, Royal Navy (mainly Tasmania, Western Australia and Northern Territory), Lieutenant John Oxley, Royal Navy, (New South Wales); Lieutenant Colonel Sir Thomas Mitchell (New South Wales, Victoria and Queensland); Captain Charles Sturt (New South Wales and South Australia); Lieutenant John Septimus Roe, Royal Navy (Western Australia), and Colonel William Light (South Australia). After 100 years of settlement some topographic maps had been produced for both public and private use but only a few maps were of any real military utility. The colonial part-time Defence Forces prepared small-area training manoeuvre maps and some colonies had produced small systematic topographic surveys for defence of the main ports of trade and commerce in the 1880s and 1890s. That is not to say that the need for topographic mapping was not a government and public concern but there were only minor attempts to allocate appropriate public resources.

text: For 113 years of colonisation after the arrival of the First Fleet, much of the mapping of Australia, mainly for exploration, settlement and development, was supervised and conducted by naval and military officers. These officers included the well known explorers and surveyors: Captain

text: Matthew Flinders

text: , Royal Navy; Lieutenant

text: William Dawes (Royal Marines officer)

text: , (New South Wales); Lieutenant

text: Philip Parker King

text: , Royal Navy (mainly Tasmania, Western Australia and Northern Territory), Lieutenant

text: John Oxley

text: , Royal Navy, (New South Wales); Lieutenant Colonel Sir

text: Thomas Mitchell

text: (New South Wales, Victoria and Queensland); Captain

text: Charles Sturt

text: (New South Wales and South Australia); Lieutenant

text: John Septimus Roe

text: , Royal Navy (Western Australia), and Colonel

text: William Light

text: (South Australia). After 100 years of settlement some topographic maps had been produced for both public and private use but only a few maps were of any real military utility. The colonial part-time Defence Forces prepared small-area training manoeuvre maps and some colonies had produced small systematic topographic surveys for defence of the main ports of trade and commerce in the 1880s and 1890s. That is not to say that the need for topographic mapping was not a government and public concern but there were only minor attempts to allocate appropriate public resources.

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answers: mainly Tasmania, Western Australia and Northern Territory

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: was supervised and conducted by naval and military officers

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

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answers: NDQ_001592

answers: allocate appropriate public resources

answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: no

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answers: NDQ_001606

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answers: NDQ_001624

answers: Tasmania

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answers: small-area

text: Switzerland has had its current boundaries since 1815, but maps of the Old Swiss Confederacy were drawn since the 16th century. The first topographical survey on a federal level began in 1809, resulting in the Topographic Map of Switzerland (German: Topographische Karte der Schweiz) or Dufour Map (German: Dufourkarte; French: Carte Dufour). From 1869 to 1901, this map was replaced by the Topographic Atlas of Switzerland (German: Topographischer Atlas der Schweiz) or Siegfried Map (German: Siegfriedkarte; French: Carte Siegfried).

text: Switzerland

text: has had its current boundaries since 1815, but maps of the

text: Old Swiss Confederacy

text: were drawn since the 16th century. The first topographical survey on a federal level began in 1809, resulting in the

text: Topographic Map of Switzerland

text: German

text: : Topographische Karte der Schweiz) or

text: Dufour Map

text: (German: Dufourkarte;

text: French

text: : Carte Dufour). From 1869 to 1901, this map was replaced by the

text: Topographic Atlas of Switzerland

text: (German: Topographischer Atlas der Schweiz) or

text: Siegfried Map

text: (German: Siegfriedkarte; French: Carte Siegfried).

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answers: NDQ_001587

answers: From 1869 to 1901

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Topographic Survey on a federal level began in 1809

answers: NDQ_001590

answers: Topographic Map of Switzerland

answers: NDQ_001591

answers: the Old Swiss Confederacy

answers: NDQ_001592

answers: its current boundaries

answers: NDQ_001593

answers: Topographic Atlas of Switzerland

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: From 1869 to 1901

answers: NDQ_001598

answers: Topographic Atlas of Switzerland

answers: NDQ_001600

answers: Topographic Atlas of Switzerland

answers: NDQ_001603

answers: It is not possible to tell

answers: NDQ_001605

answers: Topographic Map of Switzerland

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: Topographic Map

answers: NDQ_001611

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answers: Siegfried Map

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answers: Topographic Map

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answers: Topographic Atlas

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answers: Topographic

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answers: Dufour

answers: NDQ_001623

answers: Topographic

answers: NDQ_001624

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answers: NDQ_001625

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text: inside the contour

text: inside the contour

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answers: NDQ_001586

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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_001600

answers: 0

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answers: 0

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answers: 0

answers: NDQ_001606

answers: 0

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answers: 0

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answers: 0

answers: NDQ_001613

answers: 0

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answers: 0

answers: NDQ_001618

answers: 0

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 0

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: is a way of describing the shape of an object

answers: NDQ_001588

answers: intersects

answers: NDQ_001589

answers: contour lines are drawn on a map

answers: NDQ_001590

answers: contour interval

answers: NDQ_001591

answers: inside the contour

answers: NDQ_001592

answers: inside the contour

answers: NDQ_001593

answers: slope of the land

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: direction of flow

answers: NDQ_001598

answers: contour lines

answers: NDQ_001600

answers: a plain

answers: NDQ_001603

answers: None of the above choices .

answers: NDQ_001605

answers: contours are used to represent different types of rocks

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: contour lines

answers: NDQ_001611

answers: contour lines that are very far apart show a high, steep hill.

answers: NDQ_001613

answers: hatch marks are drawn on the side with the higher elevation.

answers: NDQ_001614

answers: horizontal distances

answers: NDQ_001618

answers: contour lines

answers: NDQ_001619

answers: contour

answers: NDQ_001620

answers: contour lines

answers: NDQ_001621

answers: contour

answers: NDQ_001622

answers: contour lines

answers: NDQ_001623

answers: contour

answers: NDQ_001624

answers: contour lines

answers: NDQ_001625

answers: inside the contour

text: Dutch Topographic map of Boxtel (place), March 2014.

text: Dutch Topographic map of Boxtel (place), March 2014.

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

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answers: NDQ_001619

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answers: NDQ_001620

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answers: NDQ_001621

answers: 5

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: Changes in elevation

answers: NDQ_001587

answers: Boxtel is a place

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: A bathymetric map is not a topographic map.

answers: NDQ_001590

answers: The contour interval is the horizontal distance between contour lines.

answers: NDQ_001591

answers: Boxtel

answers: NDQ_001592

answers: map of Boxtel

answers: NDQ_001593

answers: The Dutch Topographic map of Boxtel (place), March 2014.

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: The direction that rivers and streams flow

answers: NDQ_001598

answers: The steepest side of a mountain

answers: NDQ_001600

answers: If contour lines are so close together that they almost touch

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Different colors are used to represent different types of rocks

answers: NDQ_001606

answers: The difference between two contour lines

answers: NDQ_001608

answers: contour lines help us to see the three-dimensional shape

answers: NDQ_001611

answers: Boxtel (place), March 2014

answers: NDQ_001613

answers: The side of the circle with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Boxtel

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic map

answers: NDQ_001622

answers: Boxtel

answers: NDQ_001623

answers: isobath

answers: NDQ_001624

answers: Boxtel

answers: NDQ_001625

answers: 1 km

text: Topographic maps have multiple uses in the present day: any type of geographic planning or large-scale architecture; earth sciences and many other geographic disciplines; mining and other earth-based endeavours; civil engineering and recreational uses such as hiking and orienteering.

text: Topographic maps have multiple uses in the present day: any type of geographic

text: planning

text: or large-scale

text: architecture

text: earth sciences

text: and many other

text: geographic

text: disciplines;

text: mining

text: and other earth-based endeavours;

text: civil engineering

text: and recreational uses such as

text: hiking

text: and

text: orienteering

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answers: Topographic maps

answers: NDQ_001587

answers: large-scale architecture

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: hiking and orienteering

answers: NDQ_001590

answers: Topographic maps

answers: NDQ_001591

answers: large-scale

answers: NDQ_001592

answers: large-scale architecture

answers: NDQ_001593

answers: large-scale architecture

answers: NDQ_001594

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: Multiple uses

answers: NDQ_001605

answers: Topographic

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: Topographic maps

answers: NDQ_001611

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answers: NDQ_001613

answers: orienteering

answers: NDQ_001614

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answers: NDQ_001618

answers: scale

answers: NDQ_001619

answers: Topographic

answers: NDQ_001620

answers: Topographic maps

answers: NDQ_001621

answers: Topographic

answers: NDQ_001622

answers: scale

answers: NDQ_001623

answers: isobath

answers: NDQ_001624

answers: large-scale

answers: NDQ_001625

answers: large-scale

text: Of course, to determine differences in elevation between two points, the contour interval, or distance in altitude between two adjacent contour lines, must be known, and this is given at the bottom of the map. Usually contour intervals are consistent throughout a map, but there are exceptions. Sometimes intermediate contours are present in flatter areas; these can be dashed or dotted lines at half the noted contour interval. When contours are used with hypsometric tints on a small-scale map that includes mountains and flatter low-lying areas, it is common to have smaller intervals at lower elevations so that detail is shown in all areas. Conversely, for an island which consists of a plateau surrounded by steep cliffs, it is possible to use smaller intervals as the height increases.

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answers: NDQ_001587

answers: is used with hypsometric tints

answers: NDQ_001588

answers: adjacent

answers: NDQ_001589

answers: contours are used with hypsometric tints

answers: NDQ_001590

answers: altitude

answers: NDQ_001591

answers: differences in elevation

answers: NDQ_001592

answers: determine differences in elevation between two points

answers: NDQ_001593

answers: differences in elevation

answers: NDQ_001594

answers: altitude

answers: NDQ_001595

answers: half

answers: NDQ_001597

answers: contour lines

answers: NDQ_001598

answers: contour lines

answers: NDQ_001600

answers: contour interval

answers: NDQ_001603

answers: It is possible to use smaller intervals as the height increases

answers: NDQ_001605

answers: hypsometric

answers: NDQ_001606

answers: distance in altitude

answers: NDQ_001608

answers: to determine differences in elevation between two points

answers: NDQ_001611

answers: contour lines

answers: NDQ_001613

answers: It is possible to use smaller intervals as the height increases

answers: NDQ_001614

answers: contour lines

answers: NDQ_001618

answers: mountains

answers: NDQ_001619

answers: contours

answers: NDQ_001620

answers: contour interval

answers: NDQ_001621

answers: contour lines

answers: NDQ_001622

answers: mountains

answers: NDQ_001623

answers: contour lines

answers: NDQ_001624

answers: mountains

answers: NDQ_001625

answers: half the noted contour interval

text: TopoQuest is a free web mapping service built on open source software that provides internet-based topographic maps for most of the United States.

text: TopoQuest is a free

text: web mapping

text: service built on

text: open source

text: software that provides internet-based

text: topographic maps

text: for most of the

text: United States

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text: The Kloppstert is a hill, roughly 553 metres high, in the southwestern Harz in Lower Saxony, Germany. In the topographical map printed in 1978 it can only be made out with difficulty that the third letter is an o and the penultimate one an r. Unfortunately a contour line runs over the letter r so that it looks like a p. In the digitalised  1:25,000 topographic map, the hill is wrongly named as the Klappstept.

text: The Kloppstert is a hill, roughly 553 metres high, in the southwestern

text: Harz

text: in

text: Lower Saxony

text: Germany

text: . In the topographical map printed in 1978 it can only be made out with difficulty that the third letter is an o and the penultimate one an r. Unfortunately a contour line runs over the letter r so that it looks like a p. In the digitalised  1:25,000 topographic map, the hill is wrongly named as the Klappstept.

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answers: NDQ_001591

answers: runs over the letter r

answers: NDQ_001592

answers: Kloppstert

answers: NDQ_001593

answers: topographic map

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: contour line

answers: NDQ_001598

answers: contour line

answers: NDQ_001600

answers: hill

answers: NDQ_001603

answers: topographic map

answers: NDQ_001605

answers: contour line

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: contour lines

answers: NDQ_001611

answers: hill

answers: NDQ_001613

answers: contour line

answers: NDQ_001614

answers: topographic map

answers: NDQ_001618

answers: hill

answers: NDQ_001619

answers: contour line

answers: NDQ_001620

answers: 553 metres

answers: NDQ_001621

answers: topographic map

answers: NDQ_001622

answers: hill

answers: NDQ_001623

answers: contour line

answers: NDQ_001624

answers: letter r

answers: NDQ_001625

answers: 1:25,000

text: Dutch Topographic map of Dronten (town), March 2014.

text: Dutch Topographic map of Dronten (town), March 2014.

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

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answers: NDQ_001589

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answers: NDQ_001590

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answers: 5

answers: NDQ_001622

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answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: The contour lines that are numbered represent changes in elevation

answers: NDQ_001587

answers: Dronten is a town in the Netherlands

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: A bathymetric map is not a topographic map.

answers: NDQ_001590

answers: The contour interval is the horizontal distance between contour lines

answers: NDQ_001591

answers: town

answers: NDQ_001592

answers: change direction

answers: NDQ_001593

answers: Dronten (town) is located in the Netherlands.

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Dronten (town), March 2014

answers: NDQ_001598

answers: Dronten (town)

answers: NDQ_001600

answers: If contour lines are so close together that they almost touch

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Different colors are used to represent different types of rocks

answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: contour lines help us to see the three-dimensional shape

answers: NDQ_001611

answers: Concentric lines that are very far apart show a high, steep hill

answers: NDQ_001613

answers: The side of the circle with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Topographic map

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic map

answers: NDQ_001622

answers: Topographic map

answers: NDQ_001623

answers: isobath

answers: NDQ_001624

answers: V-shaped contour lines

answers: NDQ_001625

answers: 1 km

text: U.S. Forest Service maps, Bureau of Land Management maps, and U.S. Geological Survey (USGS) 1-24,000 scale topographic hard copy maps or topographic software such as National Geographic TOPO! are recommended for planning and on-trail use. A trail map is available for digital download in seventy-six separate PDF files at the Idaho Parks and Recreation Department Web site (see links section below). The link below does not lead to the PDF files but they can be found by searching the Idaho Parks and Recreation Web site.

text: U.S. Forest Service maps, Bureau of Land Management maps, and U.S. Geological Survey (USGS) 1-24,000 scale topographic hard copy maps or topographic software such as National Geographic TOPO! are recommended for planning and on-trail use. A trail map is available for digital download in seventy-six separate PDF files at the Idaho Parks and Recreation Department Web site (see links section below). The link below does not lead to the PDF files but they can be found by searching the Idaho Parks and Recreation Web site.

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text: Based on the survey, some 150 geographical features were mapped for the first time and a new 1:100000 topographic map of the two islands was published in 2005.  Data from the topographic survey Tangra 2004/05 was used also in the 2008 Bulgarian map of Livingston, Greenwich, Robert, Snow, and Smith Islands.

text: Based on the survey, some 150 geographical features were mapped for the first time and a new 1:100000

text: topographic map

text: of the two islands was published in 2005.  Data from the topographic survey Tangra 2004/05 was used also in the 2008 Bulgarian map of Livingston, Greenwich,

text: Robert

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text: , and

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text: Islands.

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text: Björn Gunnlaugsson (25 September 1788 – 17 March 1876) was an Icelandic mathematician and cartographer. For the Icelandic Literary Society, he surveyed the country from 1831 to 1843. The results of his work were published in a topographic map of Iceland at a scale of 1:480,000 on four sheets. It was the first complete map of Iceland and, although generally dated to 1844, was not completed until 1848. It was published under the direction of Olaf Nikolas Olsen in Copenhagen. In 1849, a smaller edition on one sheet at a scale of 1:960,000 appeared. For his survey work, Björn received the Order of the Dannebrog in 1846 and the French Légion d'honneur in 1859.

text: Björn Gunnlaugsson (25 September 1788 – 17 March 1876) was an

text: Iceland

text: ic

text: mathematician

text: and

text: cartographer

text: . For the

text: Icelandic Literary Society

text: , he surveyed the country from 1831 to 1843. The results of his work were published in a

text: topographic

text: map of Iceland at a scale of 1:480,000 on four sheets. It was the first complete map of Iceland and, although generally dated to 1844, was not completed until 1848. It was published under the direction of

text: Olaf Nikolas Olsen

text: in

text: Copenhagen

text: . In 1849, a smaller edition on one sheet at a scale of 1:960,000 appeared. For his survey work, Björn received the

text: Order of the Dannebrog

text: in 1846 and the French

text: Légion d'honneur

text: in 1859.

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text: Topographic maps for Taiwan had long been kept as confidential information due to security concerns. It has only been recently made available to public from the National Land Surveying and Mapping Center, the government agency responsible for surveying and publishing various maps. Topographic maps of up to 1:25,000 is now available in digital and printed format.

text: Topographic maps for Taiwan had long been kept as confidential information due to security concerns. It has only been recently made available to public from the National Land Surveying and Mapping Center, the government agency responsible for surveying and publishing various maps. Topographic maps of up to 1:25,000 is now available in digital and printed format.

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text: The Wei (220–265) and Jin Dynasty (265–420) cartographer and official Pei Xiu (224–271) was the first in China to describe in full the geometric grid reference for maps that allowed for precise measurements using a graduated scale, as well as topographical elevation. However, map-making in China had existed since at least the 4th century BC with the Qin state maps found in Gansu in 1986. Pinpointed accuracy of the winding courses of rivers and familiarity with scaled distance had been known since the Qin and Han Dynasty, respectively, as evidenced by their existing maps, while the use of a rectangular grid had been known in China since the Han as well. Historian Howard Nelson states that, although the accounts of Zhang Heng's work in cartography are somewhat vague and sketchy, there is ample written evidence that Pei Xiu derived the use of the rectangular grid reference from the maps of Zhang Heng. Rafe de Crespigny asserts that it was Zhang who established the rectangular grid system in Chinese cartography. Needham points out that the title of his book Flying Bird Calendar may have been a mistake, and that the book is more accurately entitled Bird's Eye Map. Historian Florian C. Reiter notes that Zhang's narrative "Guitian fu" contains a phrase about applauding the maps and documents of Confucius of the Zhou Dynasty, which Reiter suggests places maps (tu) on a same level of importance with documents (shu). It is documented that a physical geography map was first presented by Zhang Heng in 116 AD, called a Ti Hsing Thu.

text: The

text: Wei

text: (220–265) and

text: Jin Dynasty

text: cartographer

text: and official

text: Pei Xiu

text: (224–271) was the first in China to describe in full the geometric

text: grid reference

text: for maps that allowed for precise measurements

text: using a graduated scale

text: , as well as topographical

text: elevation

text: . However, map-making in China had existed since at least the 4th century BC with the

text: Qin state

text: maps found in

text: Gansu

text: in 1986. Pinpointed accuracy of the winding courses of rivers and familiarity with scaled distance had been known since the

text: Qin

text: and Han Dynasty, respectively, as evidenced by their existing maps, while the use of a rectangular

text: grid

text: Confucius

text: of the Zhou Dynasty, which Reiter suggests places maps (tu) on a same level of importance with documents (shu). It is documented that a physical geography map was first presented by Zhang Heng in 116 AD, called a Ti Hsing Thu.

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answers: NDQ_001587

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answers: NDQ_001588

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answers: NDQ_001589

answers: Pinpointed accuracy of the winding courses of rivers

answers: NDQ_001590

answers: topographical elevation

answers: NDQ_001591

answers: winding courses of rivers

answers: NDQ_001592

answers: precise measurements using a graduated scale

answers: NDQ_001593

answers: elevation

answers: NDQ_001594

answers: bathymetric map

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Pinpointed accuracy

answers: NDQ_001598

answers: elevation

answers: NDQ_001600

answers: Bird's Eye Map

answers: NDQ_001603

answers: it was Zhang who established the rectangular grid system in Chinese cartography

answers: NDQ_001605

answers: Pei Xiu

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographical elevation

answers: NDQ_001611

answers: topographical elevation

answers: NDQ_001613

answers: the use of a rectangular grid

answers: NDQ_001614

answers: Topographic elevation

answers: NDQ_001618

answers: elevation

answers: NDQ_001619

answers: graduated scale

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: topographical

answers: NDQ_001622

answers: elevation

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answers: graduated scale

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answers: elevation

answers: NDQ_001625

answers: 220–265)

text: The first officer appointed to the position Lieutenant Survey Section RAE (Permanent) was Lieutenant William Lawrence Whitham, a licensed surveyor from South Australia, having been highly recommended by the Surveyor-General South Australia. He assumed his appointment on 1 July 1910 at which time there were seven members of the Section. All men were professional surveyors and draftsman. CMF officers of the AIC in the Military District Headquarters supervised the work of the Section. In 1912 the Queensland, New South Wales, Victoria and South Australia State Governments each agreed to loan a Lands Department Survey Officer to the Survey Section RAE for two years to supervise the work of the Section in each State. Each Survey Officer was a militia officer in the AIC. The Section was divided into two sub-sections and employed in New South Wales, Victoria, South Australia and Western Australia producing scale 1 inch to 1 mile military maps ('1 mile' map) mainly of areas around cities and key infrastructure. By mid-1913 the Section had completed topographic field sheets by plane-tabling for eight maps around Newcastle, Melbourne and Canberra. The initial method of using parish plans to position the topographic detail was soon found to be inadequate and a geodetic subsection was established in 1914 to provide surveys by geodetic triangulation as spatial frameworks for the field sheets produced by the topographers. The triangulation work started at Werribee south-west of Melbourne and proceeded west along the coast to Warrnambool. This work included the 1860 Geodetic Survey of Victoria where appropriate – much of which was produced by Royal Engineer officers. The AIC was disbanded in 1914 but the work of the Survey Section continued under the supervision and control of the Intelligence Section of the General Staff under the general direction of the Chief of the General Staff (CGS).

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answers: 0: The answer is not relevant or complete at all.

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answers: NDQ_001625

answers: 1 mile

answers: NDQ_001586

answers: scale 1 inch to 1 mile

answers: NDQ_001587

answers: The Section was divided into two sub-sections

answers: NDQ_001588

answers: by plane-tabling

answers: NDQ_001589

answers: scale 1 inch to 1 mile military maps

answers: NDQ_001590

answers: 1 inch to 1 mile

answers: NDQ_001591

answers: triangulation

answers: NDQ_001592

answers: position the topographic detail

answers: NDQ_001593

answers: by plane-tabling

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: by geodetic triangulation

answers: NDQ_001598

answers: triangulation

answers: NDQ_001600

answers: 1 inch to 1 mile

answers: NDQ_001603

answers: surveyors and draftsman

answers: NDQ_001605

answers: '1 mile' map

answers: NDQ_001606

answers: 1 inch

answers: NDQ_001608

answers: triangulation

answers: NDQ_001611

answers: triangulation

answers: NDQ_001613

answers: triangulation

answers: NDQ_001614

answers: By mid-1913

answers: NDQ_001618

answers: 1 mile

answers: NDQ_001619

answers: 1 mile

answers: NDQ_001620

answers: 1 mile

answers: NDQ_001621

answers: 1 mile map

answers: NDQ_001622

answers: 1 mile

answers: NDQ_001623

answers: triangulation

answers: NDQ_001624

answers: 1 mile

answers: NDQ_001625

answers: 1 mile

text: CARLA was a customized software program conceived by Beverly Willis and written in house by a Harvard Graduate School of Design student, Jochen Eigen, designed to analyze prospective land parcels for their development potential as large-scale multi-unit complexes. Jochen Eigen wrote the programming scripts that directed CARLA as the managing software to interface a variety of planning unit concepts with a mapping program that could then process a variety of planning proposals against the site’s fixed fields of relevant data. The data was extracted from traditional analog topographical maps soil analysis, and marketing information.

text: CARLA was a customized software program conceived by

text: Beverly Willis

text: and written in house by a

text: Harvard Graduate School of Design

text: student, Jochen Eigen, designed to analyze prospective land parcels for their development potential as large-scale multi-unit complexes. Jochen Eigen wrote the programming scripts that directed CARLA as the managing software to interface a variety of planning unit concepts with a mapping program that could then process a variety of planning proposals against the site’s fixed fields of relevant data. The data was extracted from traditional analog topographical maps soil analysis, and marketing information.

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answers: NDQ_001588

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answers: NDQ_001589

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answers: NDQ_001590

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answers: NDQ_001591

answers: multi-unit complexes

answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: traditional analog topographical maps

answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

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answers: NDQ_001606

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answers: NDQ_001613

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answers: NDQ_001621

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answers: NDQ_001622

answers: soil

answers: NDQ_001623

answers: topographic

answers: NDQ_001624

answers: soil

answers: NDQ_001625

answers: 12 mile

text: Cartographers use a projection to project the curved surface of the earth onto a flat surface. This generates a grid that is used as a base for national topographic mapping. The projection introduces a distortion so that grid north differs from true north; magnetic north is a natural feature that differs from both. As an example: at 52° 35' N 1° 10' E (approx 7 km west of Norwich, England) true north is 2° 33' west of grid north, and magnetic north is about 7° west of grid north. Magnetic north varies continually and in this example (1986) was reducing by about ½° in four years. Orienteering maps are printed using magnetic north and this requires an adjustment to be made to the base map.

text: Cartographers use a

text: projection

text: to project the curved surface of the earth onto a flat surface. This generates a grid that is used as a base for national topographic mapping. The projection introduces a distortion so that grid north differs from true north; magnetic north is a natural feature that differs from both. As an example: at 52° 35' N 1° 10' E (approx 7 km west of Norwich, England) true north is 2° 33' west of grid north, and magnetic north is about 7° west of grid north. Magnetic north varies continually and in this example (1986) was reducing by about ½° in four years. Orienteering maps are printed using magnetic north and this requires an adjustment to be made to the base map.

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answers: 4

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answers: NDQ_001624

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answers: NDQ_001625

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answers: NDQ_001586

answers: contour lines that are numbered represent changes in elevation

answers: NDQ_001587

answers: project the curved surface of the earth onto a flat surface

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: true north is about 7° west of grid north

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: magnetic north

answers: NDQ_001592

answers: magnetic north

answers: NDQ_001593

answers: This generates a grid

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: magnetic north

answers: NDQ_001598

answers: magnetic north

answers: NDQ_001600

answers: flat surface

answers: NDQ_001603

answers: Orienteering

answers: NDQ_001605

answers: Cartographers use a projection

answers: NDQ_001606

answers: true north is about 7° west of grid north

answers: NDQ_001608

answers: topographic mapping

answers: NDQ_001611

answers: magnetic north

answers: NDQ_001613

answers: Orienteering

answers: NDQ_001614

answers: magnetic north

answers: NDQ_001618

answers: true north

answers: NDQ_001619

answers: water depth map

answers: NDQ_001620

answers: true north

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: true north

answers: NDQ_001623

answers: grid

answers: NDQ_001624

answers: true north

answers: NDQ_001625

answers: 1 2°

text: The topographic map revealed in the olfactory system differs in quality from the orderly representation inherent in the retinotopic, tonotopic, or somatotopic sensory maps.  Olfactory neurons differ from one another by the nature of the receptor that they possess. However, the olfactory sensory neurons to which olfactory bulb neurons are connected are also distributed across the receptor sheet (the olfactory epithelium) depending on their chemical preferences. Locations on the olfactory epithelium and the olfactory bulb are correlated  so, as with other sensory systems, the topographic map in the brain is linked to the structure of the peripheral organ. This principle is called rhinotopy.

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answers: 4

answers: NDQ_001589

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answers: 4

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 0

answers: NDQ_001597

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answers: 0

answers: NDQ_001600

answers: 0

answers: NDQ_001603

answers: 0

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answers: NDQ_001606

answers: 4

answers: NDQ_001608

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answers: NDQ_001611

answers: 0

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 4

answers: NDQ_001618

answers: 0

answers: NDQ_001619

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answers: NDQ_001620

answers: 0

answers: NDQ_001621

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answers: NDQ_001622

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answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: topographic map

answers: NDQ_001587

answers: the olfactory epithelium

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: topographic map revealed in the olfactory system

answers: NDQ_001590

answers: topographic map

answers: NDQ_001591

answers: the topographic map

answers: NDQ_001592

answers: orderly representation

answers: NDQ_001593

answers: topographic map

answers: NDQ_001594

answers: topographic map

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: This principle is called rhinotopy

answers: NDQ_001598

answers: topographic map

answers: NDQ_001600

answers: topographic map

answers: NDQ_001603

answers: no

answers: NDQ_001605

answers: topographic map

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic map

answers: NDQ_001611

answers: topographic map

answers: NDQ_001613

answers: This principle is called rhinotopy

answers: NDQ_001614

answers: topographic map

answers: NDQ_001618

answers: tonotopic

answers: NDQ_001619

answers: tonotopic

answers: NDQ_001620

answers: tonotopic

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: retinotopic

answers: NDQ_001623

answers: tonotopic

answers: NDQ_001624

answers: tonotopic

answers: NDQ_001625

answers: the topographic map revealed in the olfactory system

text: The GNIS database consistently reports the peak elevation lower than the referenced USGS and/or USFS topographic maps. The topographic maps also report lower elevations than selected GPS measurements conducted by personnel of the Juneau Icefield Research Program, but not to the degree of the GNIS Database.

text: The

text: GNIS

text: database consistently reports the peak elevation lower than the referenced

text: USGS

text: and/or

text: USFS

text: topographic maps. The topographic maps also report lower elevations than selected

text: GPS

text: measurements conducted by personnel of the

text: Juneau Icefield Research Program

text: , but not to the degree of the

text: GNIS

text: Database.

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text: RADARSAT-2 is a follow-on to RADARSAT-1 which mission terminated in April 2013. It has the same orbit (798 km altitude sun-synchronous orbit with 6 p.m. ascending node and 6 a.m. descending node). Some of the orbit characteristics are 24 days repeat cycle (=343 orbits), 14.29 orbits per day, each orbit being 100.75 minutes duration. It is filling a wide variety of application, including sea ice mapping and ship routing, iceberg detection, agricultural crop monitoring, marine surveillance for ship and pollution detection, terrestrial defence surveillance and target identification, geological mapping, mine monitoring, land use mapping, wetlands mapping, topographic mapping.

text: RADARSAT-2 is a follow-on to

text: which mission terminated in April 2013. It has the same orbit (798 km altitude

text: sun-synchronous orbit

text: with 6 p.m. ascending node and 6 a.m. descending node). Some of the orbit characteristics are 24 days repeat cycle (=343 orbits), 14.29 orbits per day, each orbit being 100.75 minutes duration. It is filling a wide variety of application, including sea ice mapping and ship routing, iceberg detection, agricultural crop monitoring, marine surveillance for ship and pollution detection, terrestrial defence surveillance and target identification, geological mapping, mine monitoring, land use mapping, wetlands mapping, topographic mapping.

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text: The work of the Commission is supported by geographical information and mapping resulting from topographic surveys in Antarctica, such as the 1995/96 survey in Livingston Island, and the topographic survey Tangra 2004/05. Field work carried out during the latter survey has been noted by Discovery Channel as a timeline event in Antarctic exploration.

text: The work of the Commission is supported by

text: geographical information

text: and

text: mapping

text: resulting from

text: topographic

text: surveys

text: in Antarctica, such as the 1995/96 survey in

text: Livingston Island

text: , and the topographic survey

text: Tangra 2004/05

text: . Field work carried out during the latter survey has been noted by

text: Discovery Channel

text: as a timeline event in Antarctic exploration.

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answers: NDQ_001586

answers: topographic surveys

answers: NDQ_001587

answers: survey in Livingston Island

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: topographic surveys in Antarctica

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: topographic surveys

answers: NDQ_001592

answers: timeline event in Antarctic exploration

answers: NDQ_001593

answers: topographic surveys

answers: NDQ_001594

answers: topographic surveys

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: topographic surveys

answers: NDQ_001598

answers: topographic surveys

answers: NDQ_001600

answers: Tangra

answers: NDQ_001603

answers: no

answers: NDQ_001605

answers: Tangra

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic

answers: NDQ_001611

answers: Tangra

answers: NDQ_001613

answers: Tangra

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Livingston Island

answers: NDQ_001619

answers: topographic

answers: NDQ_001620

answers: topographic surveys

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: Antarctica

answers: NDQ_001623

answers: topographic

answers: NDQ_001624

answers: Tangra

answers: NDQ_001625

answers: 2004/05

text: Belt is located just to the west of the village of Hippolytushoef. It is named after the small hill ("bult") that it lies on. It is not named on recent topographical maps, where it is considered to be a part of Hippolytushoef.

text: Belt is located just to the west of the village of

text: Hippolytushoef

text: . It is named after the small hill ("bult") that it lies on. It is not named on recent topographical maps, where it is considered to be a part of Hippolytushoef.

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answers: NDQ_001587

answers: is not named on recent topographical maps

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: it is not named on recent topographical maps

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: hill ("bult") that it lies on

answers: NDQ_001592

answers: name

answers: NDQ_001593

answers: hill ("bult")

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: west

answers: NDQ_001598

answers: west

answers: NDQ_001600

answers: hill ("bult")

answers: NDQ_001603

answers: It is not named on recent topographical maps

answers: NDQ_001605

answers: Bult

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographical maps

answers: NDQ_001611

answers: hill ("bult")

answers: NDQ_001613

answers: "bult"

answers: NDQ_001614

answers: topographical maps

answers: NDQ_001618

answers: topographical maps

answers: NDQ_001619

answers: topographical maps

answers: NDQ_001620

answers: hill ("bult")

answers: NDQ_001621

answers: topographical

answers: NDQ_001622

answers: not named

answers: NDQ_001623

answers: hill

answers: NDQ_001624

answers: recent topographical maps

answers: NDQ_001625

answers: 8 kilometres

text: is the angle which the side makes with North or South directions (the instruments used in traversing include Total Station or Theodolite with stand, Compass with stand, ranging rods and measuring tape). Then in next step RL (reduced level) of each station is determined with reference to permanent benchmark (the instruments used to determine reduced level include Auto Level with stand and Levelling Staff). Then RL of different points keeping specified spacing between them with reference to each station is determined. The points having same RL are joined to form contour lines and thus a topographic map of an area is prepared using AutoCAD or with the help of plane table survey.

text: is the angle which the side makes with North or South directions (the instruments used in traversing include Total Station or Theodolite with stand, Compass with stand, ranging rods and measuring tape). Then in next step

text: RL

text: (reduced level) of each station is determined with reference to permanent

text: benchmark

text: (the instruments used to determine reduced level include Auto Level with stand and Levelling Staff). Then RL of different points keeping specified spacing between them with reference to each station is determined. The points having same RL are joined to form

text: contour lines

text: and thus a topographic map of an area is prepared using AutoCAD or with the help of plane table survey.

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answers: NDQ_001586

answers: points having same RL

answers: NDQ_001587

answers: is the angle which the side makes

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: is the angle which the side makes with North or South directions

answers: NDQ_001590

answers: RL

answers: NDQ_001591

answers: angle

answers: NDQ_001592

answers: Levelling Staff

answers: NDQ_001593

answers: The angles which the side makes with North or South directions

answers: NDQ_001594

answers: RL

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: North or South

answers: NDQ_001598

answers: angle which the side makes with North or South directions

answers: NDQ_001600

answers: RL

answers: NDQ_001603

answers: unanswerable

answers: NDQ_001605

answers: contour lines

answers: NDQ_001606

answers: RL

answers: NDQ_001608

answers: topographic map

answers: NDQ_001611

answers: points having same RL are joined to form contour lines

answers: NDQ_001613

answers: Theodolite with stand

answers: NDQ_001614

answers: RL

answers: NDQ_001618

answers: area

answers: NDQ_001619

answers: contour lines

answers: NDQ_001620

answers: spacing

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: area

answers: NDQ_001623

answers: contour lines

answers: NDQ_001624

answers: area

answers: NDQ_001625

answers: spacing between them

text: The traditional set of Vicmap Topographic maps consist of approximately 850 1:25000 and 1:50000 hardcopy topographic map sheets printed and made available for sale to the general public. These map sheets cover 80% of Victoria. Most of the mapsheets are single format at a scale of 1:25000. Less inhabited areas of the state are covered by double format 1:25000 and 1:50000 mapsheets. All of these maps were produced using traditional cartographic methods, with the majority being last updated in the 1970s and 1980s.

text: The traditional set of Vicmap Topographic maps consist of approximately 850 1:25000 and 1:50000 hardcopy topographic map sheets printed and made available for sale to the general public. These map sheets cover 80% of Victoria. Most of the mapsheets are single format at a scale of 1:25000. Less inhabited areas of the state are covered by double format 1:25000 and 1:50000 mapsheets. All of these maps were produced using traditional cartographic methods, with the majority being last updated in the 1970s and 1980s.

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answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: These map sheets cover 80% of Victoria

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: the majority being last updated in the 1970s and 1980s

answers: NDQ_001590

answers: 1:25000

answers: NDQ_001591

answers: Less inhabited areas

answers: NDQ_001592

answers: cover 80% of Victoria

answers: NDQ_001593

answers: 1:25000

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: 1:25000

answers: NDQ_001598

answers: 1:25000

answers: NDQ_001600

answers: 1:25000

answers: NDQ_001603

answers: general public

answers: NDQ_001605

answers: 1:25000

answers: NDQ_001606

answers: 1:25000

answers: NDQ_001608

answers: 1:25000

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answers: 1:25000

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answers: 1:25000

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answers: 1:25000

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answers: 1:25000

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answers: 1:25000

answers: NDQ_001620

answers: 1:25000

answers: NDQ_001621

answers: 1:25000

answers: NDQ_001622

answers: Less inhabited areas

answers: NDQ_001623

answers: 1:25000

answers: NDQ_001624

answers: 1:25000

answers: NDQ_001625

answers: 1:25000

text: The contour of the interpolant on an individual triangle is a line segment (it is an interval on the intersection of two planes). The equation for the line can be found, however the points where the line crosses the edges of the triangle are the endpoints of the line segment.

text: The contour of the interpolant on an individual triangle is a line segment (it is an interval on the intersection of two planes). The equation for the line can be found, however the points where the line crosses the edges of the triangle are the endpoints of the line segment.

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answers: an interval on the intersection of two planes

text: The computer graphic information reports were represented either in the form of topographical site perspectives, contour maps or as a sequence of numeric values organized within a template matrix that allowed the architect to identify the optimal relationships and planning concept. This work then became the basis for presentation materials that were used to introduce the client/developer to the proposed designs.

text: The computer graphic information reports were represented either in the form of topographical site perspectives, contour maps or as a sequence of numeric values organized within a template matrix that allowed the architect to identify the optimal relationships and planning concept. This work then became the basis for presentation materials that were used to introduce the client/developer to the proposed designs.

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answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001619

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text: Official references are the NOAA Coastal pilot, NOAA nautical charts, and USGS topographic maps.<ref name="usgs_topo">USGS topographic maps, 1:24,000 scale, listed from west to east (in a row), then north to south:

text: Official references are the

text: NOAA

text: Coastal pilot, NOAA

text: nautical chart

text: s, and

text: USGS

text: topographic maps.<ref name="usgs_topo">USGS topographic maps, 1:24,000 scale, listed from west to east (in a row), then north to south:

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answers: NDQ_001591

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answers: NDQ_001593

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answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: from west to east (in a row), then north to south

answers: NDQ_001598

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answers: NDQ_001600

answers: Plain or plateau

answers: NDQ_001603

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answers: Coastal pilot

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answers: Coastal pilot

answers: NDQ_001625

answers: 1:24,000

text: Because the M tidal constituent dominates in most locations, the stage or phase of a tide, denoted by the time in hours after high water, is a useful concept. Tidal stage is also measured in degrees, with 360° per tidal cycle. Lines of constant tidal phase are called cotidal lines, which are analogous to contour lines of constant altitude on topographical maps. High water is reached simultaneously along the cotidal lines extending from the coast out into the ocean, and cotidal lines (and hence tidal phases) advance along the coast. Semi-diurnal and long phase constituents are measured from high water, diurnal from maximum flood tide. This and the discussion that follows is precisely true only for a single tidal constituent.

text: Because the M tidal constituent dominates in most locations, the stage or phase of a tide, denoted by the time in hours after high water, is a useful concept. Tidal stage is also measured in degrees, with 360° per tidal cycle. Lines of constant tidal phase are called cotidal lines, which are analogous to

text: contour lines

text: of constant altitude on

text: topographical maps

text: . High water is reached simultaneously along the cotidal lines extending from the coast out into the ocean, and cotidal lines (and hence tidal phases) advance along the coast. Semi-diurnal and long phase constituents are measured from high water, diurnal from maximum flood tide. This and the discussion that follows is precisely true only for a single tidal constituent.

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answers: NDQ_001586

answers: contour lines of constant altitude

answers: NDQ_001587

answers: is analogous to contour lines of constant altitude on topographical maps

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: contour lines of constant altitude

answers: NDQ_001590

answers: constant altitude

answers: NDQ_001591

answers: constant altitude

answers: NDQ_001592

answers: Tidal stage

answers: NDQ_001593

answers: contour lines of constant altitude

answers: NDQ_001594

answers: cotidal lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: cotidal lines

answers: NDQ_001598

answers: contour lines of constant altitude

answers: NDQ_001600

answers: contour lines of constant altitude

answers: NDQ_001603

answers: unanswerable

answers: NDQ_001605

answers: contour lines

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographical maps

answers: NDQ_001611

answers: contour lines of constant altitude

answers: NDQ_001613

answers: contour lines of constant altitude

answers: NDQ_001614

answers: cotidal lines

answers: NDQ_001618

answers: constant altitude

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text: The landmark scientific expedition (December 1872 – May 1876) of the British Royal Navy survey ship HMS Challenger yielded a tremendous amount of bathymetric data, much of which has been confirmed by subsequent researchers. Bathymetric data obtained during the course of the Challenger expedition enabled scientists to draw maps, which provided a rough outline of certain major submarine terrain features, such as the edge of the continental shelves and the Mid-Atlantic Ridge. This discontinuous set of data points was obtained by the simple technique of taking soundings by lowering long lines from the ship to the seabed.

text: The landmark scientific

text: expedition

text: (December 1872 – May 1876) of the British

text: Royal Navy

text: survey ship

text: HMS Challenger

text: yielded a tremendous amount of

text: bathymetric

text: data, much of which has been confirmed by subsequent researchers. Bathymetric data obtained during the course of the Challenger expedition enabled scientists to draw maps, which provided a rough outline of certain major submarine terrain features, such as the edge of the

text: continental shelves

text: and the

text: Mid-Atlantic Ridge

text: . This discontinuous set of data points was obtained by the simple technique of taking

text: soundings

text: by lowering long lines from the ship to the seabed.

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answers: NDQ_001588

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answers: provided a rough outline of certain major submarine terrain features

answers: NDQ_001590

answers: long lines

answers: NDQ_001591

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answers: NDQ_001592

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answers: NDQ_001593

answers: Bathymetric

answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

answers: Mid-Atlantic Ridge

answers: NDQ_001603

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answers: NDQ_001625

answers: discontinuous set of data points

text: Contour lines are also used to display non-geographic information in economics. Indifference curves (as shown at left) are used to show bundles of goods to which a person would assign equal utility. An isoquant (in the image at right) is a curve of equal production quantity for alternative combinations of input usages, and an isocost curve (also in the image at right) shows alternative usages having equal production costs.

text: Contour lines are also used to display non-geographic information in economics.

text: Indifference curves

text: (as shown at left) are used to show bundles of goods to which a person would assign equal utility. An

text: isoquant

text: (in the image at right) is a curve of equal production quantity for alternative combinations of

text: input usages

text: , and an

text: isocost curve

text: (also in the image at right) shows alternative usages having equal production costs.

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answers: Contour lines

answers: NDQ_001587

answers: shows alternative usages having equal production costs

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Indifference curves

answers: NDQ_001590

answers: Contour lines

answers: NDQ_001591

answers: non-geographic information

answers: NDQ_001592

answers: Indifference curves

answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001598

answers: contour lines

answers: NDQ_001600

answers: isoquant

answers: NDQ_001603

answers: non-geographic

answers: NDQ_001605

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answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: Contour lines are used to display non-geographic information

answers: NDQ_001611

answers: Contour lines

answers: NDQ_001613

answers: Contour lines are used to display non-geographic information in economics

answers: NDQ_001614

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answers: NDQ_001618

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answers: isoquant

answers: NDQ_001623

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answers: NDQ_001624

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answers: equal

text: along the contour

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answers: changes in elevation

answers: NDQ_001587

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answers: NDQ_001588

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answers: NDQ_001589

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answers: NDQ_001597

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answers: contour is a type of rock

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answers: the difference between two contour lines

answers: NDQ_001608

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answers: contour lines that are very far apart show a high, steep hill.

answers: NDQ_001613

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answers: NDQ_001614

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text: Contour lines (or isohypses) are isolines showing equal elevation. This is the most common way of numerically showing elevation, and is familiar from topographic maps.

text: Contour lines (or isohypses) are isolines showing equal elevation. This is the most common way of numerically showing elevation, and is familiar from

text: topographic map

text: s.

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text: This map is derived from GTOPO30 data that describes the elevation of Earth's terrain at intervals of 30 arcseconds (approximately 1 km).  It uses color and shading instead of contour lines to indicate elevation.

text: This map is derived from

text: data that describes the elevation of Earth's terrain at intervals of 30 arcseconds (approximately 1 km).  It uses color and shading instead of contour lines to indicate elevation.

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answers: 30 arc seconds

text: The composition ψφ is an order-preserving map from the interval [a ∧ b, b] to itself which also satisfies the inequality ψ(φ(x)) = (x ∨ a) ∧ b ≥ x. The example shows that this inequality can be strict in general. In a modular lattice, however, equality holds. Since the dual of a modular lattice is again modular, φψ is also the identity on [a, a ∨ b], and therefore the two maps φ and ψ are isomorphisms between these two intervals. This result is sometimes called the diamond isomorphism theorem for modular lattices. A lattice is modular if and only if the diamond isomorphism theorem holds for every pair of elements.

text: The composition ψφ is an order-preserving map from the interval [a ∧ b, b] to itself which also satisfies the inequality ψ(φ(x)) = (x ∨ a) ∧ b ≥ x. The example shows that this inequality can be strict in general. In a modular lattice, however, equality holds. Since the dual of a modular lattice is again modular, φψ is also the identity on [a, a ∨ b], and therefore the two maps φ and ψ are isomorphisms between these two intervals. This result is sometimes called the diamond isomorphism theorem for modular lattices. A lattice is modular if and only if the diamond isomorphism theorem holds for every pair of elements.

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answers: NDQ_001598

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text: When the AIF members returned to Australia in 1919 they were discharged and most were re-appointed to the Survey Section RAE (Permanent) or the Australian Survey Corps (Permanent). Military reorganisation after World War I, and the general reduction in military capability, saw the numbers reduced to fourteen all ranks. In 1920 the Corps was suspended and reverted, in title, to the Survey Section, RAE (Permanent). Mapping continued, mainly the '1 mile' maps, albeit at a reduced rate consistent with the allocated resources, with priority given to areas around Brisbane, Sydney and Melbourne. By 1929 the Section had produced fifty-four '1 mile' maps including five revised maps. Technical developments provided for improved efficiencies. These included use of single photographs and strips of air photographs to supplement ground surveys by plane-table for topographic detail. The first military map produced with a significant component of aerial photography flown by the Royal Australian Air Force was the Albury '1 mile' map published in 1933. Compilation of this map highlighted inconsistencies in State triangulation systems and once again demonstrated the need for a national geodetic survey which had been identified by colonial survey officers in the 1890s.

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text: On a user pays basis it produces geospatial products such as topographic maps and satellite imagery. It is also a major contributor to the Australian Government's free, open data collections such as data.gov.au.

text: On a

text: user pays

text: basis it produces geospatial products such as

text: topographic maps

text: and

text: satellite imagery

text: . It is also a major contributor to the Australian Government's free, open data collections such as data.gov.au.

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text: Selecting a model for a shape of the Earth involves choosing between the advantages and disadvantages of a sphere versus an ellipsoid. Spherical models are useful for small-scale maps such as world atlases and globes, since the error at that scale is not usually noticeable or important enough to justify using the more complicated ellipsoid. The ellipsoidal model is commonly used to construct topographic maps and for other large- and medium-scale maps that need to accurately depict the land surface. Auxiliary latitudes are often employed in projecting the ellipsoid.

text: Selecting a model for a shape of the Earth involves choosing between the advantages and disadvantages of a sphere versus an ellipsoid. Spherical models are useful for small-scale maps such as world atlases and globes, since the error at that scale is not usually noticeable or important enough to justify using the more complicated ellipsoid. The ellipsoidal model is commonly used to construct

text: topographic map

text: s and for other large- and medium-scale maps that need to accurately depict the land surface.

text: Auxiliary latitudes

text: are often employed in projecting the ellipsoid.

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answers: Auxiliary latitudes

text: Snow cover is frequently shown as a contour-line map.

text: Snow

text: cover is frequently shown as a contour-line map.

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text: Petermann was responsible for drawing most of the maps in the first few years of the journal. His strength was in the analysis and evaluation of all sources available. As such one can say that the indication ‘Originalkarte’ (original map) in many titles was well earned, for few slavishly copied what explorers or other experts had sketched. German geographers, like Hermann Wagner (1840–1929), claimed that in other geographical journals explorer's maps were just copied instead of having them evaluated by cartographers first. Maps based on recent exploration reports were always, when possible, complemented with route maps from previous expeditions. He did not like to infer or extrapolate from the sources, for that might give inaccurate measurements, so many of his maps show large blank spaces. How right he was in this respect was demonstrated in 1911 when Julien Thoulet drafted bathymetric maps for the territory of France. In these four maps he draws hypothetical isobaths, which are based on respectively 15, 31, 154, and 308 altitude measurements per  for France and the adjacent territories. (A reasonable amount of measuring points for precipitation and temperature maps would be 1,500 and 600 per 100,000 km² respectively to create acceptable isoline maps for these phenomena). These give schematic negative relief maps, which hardly even approximate the true relief of the territory. Thoulet wanted to show that the few bathymetric measurements available for the vast oceans would only vaguely approximate the true relief of the ocean floors. Petermann must have had the same idea intuitively for his exploratory maps. He was keen, however, to introduce spot heights and spot depths in the maps he drafted in order that others could benefit from them.

text: Petermann was responsible for drawing most of the maps in the first few years of the journal. His strength was in the analysis and evaluation of all sources available. As such one can say that the indication ‘Originalkarte’ (original map) in many titles was well earned, for few slavishly copied what explorers or other experts had sketched. German geographers, like

text: Hermann Wagner

text: (1840–1929), claimed that in other geographical journals explorer's maps were just copied instead of having them evaluated by cartographers first. Maps based on recent exploration reports were always, when possible, complemented with route maps from previous expeditions. He did not like to infer or extrapolate from the sources, for that might give inaccurate measurements, so many of his maps show large blank spaces. How right he was in this respect was demonstrated in 1911 when

text: Julien Thoulet

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answers: 1500

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answers: These give schematic negative relief maps, which hardly even approximate the true relief of the territory

answers: NDQ_001605

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text: is the "contour length" or

text: is the "contour length" or

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text: Fort Sumner was razed in 1953. There are a few visible remains of Battery Bailey in Westmoreland Hills Park, which can be seen from the adjacent Capital Crescent Trail. Part of the site was acquired by the Army Map Service (AMS) early in World War II and renamed Fort Sumner. The AMS was renamed US Army Topographic Command in 1968 and merged into the Defense Mapping Agency in 1972, at which time the site was renamed Defense Mapping Agency Topographic Center. The Defense Mapping Agency and its successors, the National Imagery and Mapping Agency and the National Geospatial-Intelligence Agency, occupied the site until the early 2010s. The residential area that was built over Fort Sumner has a plaque about the fort at Sangamore Road and West Path Way, and portions of it are named "Fort Sumner Hills" and "Sumner Village".

text: Fort Sumner was razed in 1953. There are a few visible remains of Battery Bailey in Westmoreland Hills Park, which can be seen from the adjacent

text: Capital Crescent Trail

text: . Part of the site was acquired by the

text: Army Map Service

text: (AMS) early in

text: World War II

text: and renamed Fort Sumner. The AMS was renamed US Army Topographic Command in 1968 and merged into the

text: Defense Mapping Agency

text: in 1972, at which time the site was renamed Defense Mapping Agency Topographic Center. The

text: Defense Mapping Agency

text: and its successors, the

text: National Imagery and Mapping Agency

text: and the

text: National Geospatial-Intelligence Agency

text: , occupied the site until the early 2010s. The residential area that was built over Fort Sumner has a plaque about the fort at Sangamore Road and West Path Way, and portions of it are named "Fort Sumner Hills" and "Sumner Village".

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answers: NDQ_001587

answers: Westmoreland Hills Park

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Fort Sumner was razed in 1953

answers: NDQ_001590

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answers: NDQ_001592

answers: renamed Fort Sumner

answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: National Geospatial-Intelligence

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answers: Topographic Center

answers: NDQ_001623

answers: Capital Crescent Trail

answers: NDQ_001624

answers: Topographic Center

answers: NDQ_001625

answers: 135 feet

text: Flintstone is included in the Fort Oglethorpe Quad of topographical maps published by the United States Geological Services.

text: Flintstone is included in the Fort Oglethorpe Quad of topographical maps published by the United States Geological Services.

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answers: intersect

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answers: Flintstone is included

answers: NDQ_001590

answers: Fort Oglethorpe Quad

answers: NDQ_001591

answers: topographical

answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: It's impossible to say

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answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

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answers: NDQ_001613

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answers: NDQ_001618

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answers: NDQ_001619

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answers: Quad

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answers: NDQ_001624

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answers: NDQ_001625

answers: Quad

text: The peak is located at  which is 940 m north of Maystora Peak,  1.22 km northeast of Razgrad Peak, 1.18 km east by north of Terter Peak, 2.87 km east of the highest point of Oborishte Ridge, 4.1 km south of Ferrer Point, 590 m west of Momchil Peak, 2 km west-northwest of the summit of Viskyar Ridge and 3.32 km northwest of Sartorius Point.  British mapping in 1968, Bulgarian topographic survey Tangra 2004/05 and mapping in 2009.

text: The peak is located at  which is 940 m north of

text: Maystora Peak

text: ,  1.22 km northeast of

text: Razgrad Peak

text: , 1.18 km east by north of

text: Terter Peak

text: , 2.87 km east of the highest point of

text: Oborishte Ridge

text: , 4.1 km south of

text: Ferrer Point

text: , 590 m west of

text: Momchil Peak

text: , 2 km west-northwest of the summit of

text: Viskyar Ridge

text: and 3.32 km northwest of

text: Sartorius Point

text: .  British mapping in 1968, Bulgarian topographic survey

text: Tangra 2004/05

text: and mapping in 2009.

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answers: British mapping in 1968

answers: NDQ_001587

answers: The peak is located at which is 940 m north of Maystora Peak

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: The peak is located at which is 940 m north of Maystora Peak

answers: NDQ_001590

answers: 1.18 km

answers: NDQ_001591

answers: summit of Viskyar Ridge

answers: NDQ_001592

answers: 4.1 km south of Ferrer Point

answers: NDQ_001593

answers: 1.18 km east by north of Terter Peak

answers: NDQ_001594

answers: Contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: northwest

answers: NDQ_001598

answers: east

answers: NDQ_001600

answers: Oborishte Ridge

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Terter Peak

answers: NDQ_001606

answers: 1.18 km east by north

answers: NDQ_001608

answers: Contour lines help us to see the three-dimensional shape of the land

answers: NDQ_001611

answers: Razgrad Peak

answers: NDQ_001613

answers: Ferrer Point

answers: NDQ_001614

answers: 1.22 km northeast of Razgrad Peak

answers: NDQ_001618

answers: Maystora Peak

answers: NDQ_001619

answers: Point

answers: NDQ_001620

answers: 940 m

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: Maystora Peak

answers: NDQ_001623

answers: Maystora Peak

answers: NDQ_001624

answers: Maystora Peak

answers: NDQ_001625

answers: 1.18 km

text: From the 16th and 17th centuries, several examples survive of maps focused on cultural information. Gridlines are not used on either Yu Shi's Gujin xingsheng zhi tu (1555) or Zhang Huang's Tushu bian (1613); instead, illustrations and annotations show mythical places, exotic foreign peoples, administrative changes and the deeds of historic and legendary heroes. Also in the 17th century, an edition of a possible Tang Dynasty map shows clear topographical contour lines. Although topographic features were part of maps in China for centuries, a Fujian county official Ye Chunji (1532–1595) was the first to base county maps using on-site topographical surveying and observations.

text: From the 16th and 17th centuries, several examples survive of maps focused on cultural information. Gridlines are not used on either

text: Yu Shi

text: 's

text: Gujin xingsheng zhi tu

text: (1555) or

text: Zhang Huang

text: 's

text: Tushu bian

text: (1613); instead, illustrations and annotations show mythical places, exotic foreign peoples, administrative changes and the deeds of historic and legendary heroes. Also in the 17th century, an edition of a possible Tang Dynasty map shows clear topographical

text: contour lines

text: . Although

text: topographic

text: features were part of maps in China for centuries, a

text: Fujian

text: county official

text: Ye Chunji

text: (1532–1595) was the first to base county maps using on-site topographical

text: surveying

text: and observations.

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answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: topographical contour lines

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: Gridlines are not used

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: topographic features

answers: NDQ_001592

answers: cultural information

answers: NDQ_001593

answers: contour lines

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: topographical contour lines

answers: NDQ_001598

answers: contour lines

answers: NDQ_001600

answers: clear topographical contour lines

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Gridlines are not used

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: contour lines

answers: NDQ_001611

answers: contour lines

answers: NDQ_001613

answers: contour lines

answers: NDQ_001614

answers: Gridlines

answers: NDQ_001618

answers: topographical

answers: NDQ_001619

answers: contour lines

answers: NDQ_001620

answers: contour lines

answers: NDQ_001621

answers: topographic contour lines

answers: NDQ_001622

answers: topographical

answers: NDQ_001623

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answers: NDQ_001624

answers: topographical

answers: NDQ_001625

answers: 17th century

text: [[File:Lake Superior bathymetry map.png|thumb|240px|Lake Superior bathymetric map. The deepest point, roughly off its southeastern shore, is marked with "×". The deep trenches in its eastern part may have originated from tunnel valleys.]]

text: [[File:Lake Superior bathymetry map.png|thumb|240px|Lake Superior

text: bathymetric map

text: . The deepest point, roughly off its southeastern shore, is marked with "×". The deep trenches in its eastern part may have originated from

text: tunnel valley

text: s.]]

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text: Line weight is simply the darkness or thickness of the line used.  This choice is made based upon the least intrusive form of contours that enable the reader to decipher the background information in the map itself.  If there is little or no content on the base map, the contour lines may be drawn with relatively heavy thickness.  Also, for many forms of contours such as topographic maps, it is common to vary the line weight and/or color, so that a different line characteristic occurs for certain numerical values. For example, in the topographic map above, the even hundred foot elevations are shown in a different weight from the twenty foot intervals.

text: Line weight is simply the darkness or thickness of the line used.  This choice is made based upon the least intrusive form of contours that enable the reader to decipher the background information in the map itself.  If there is little or no content on the base map, the contour lines may be drawn with relatively heavy thickness.  Also, for many forms of contours such as topographic maps, it is common to vary the line weight and/or color, so that a different line characteristic occurs for certain numerical values. For example, in the

text: topographic

text: map above, the even hundred foot elevations are shown in a different weight from the twenty foot intervals.

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text: TopoZone was one of the first topographic mapping site on the web, providing visitors with free viewing and printing of the full set of United States Geological Survey topographic maps covering the entire United States. The maps are produced by the USGS, which encourages the distribution of their maps through business partners.  TopoZone offered aerial photographs from the USGS and street maps from the United States Census Bureau.  In 2007 complete coverage of Canada was added, using the topographic map series produced by Natural Resources Canada.

text: TopoZone was one of the first topographic mapping site on the web, providing visitors with free viewing and printing of the full set of

text: United States Geological Survey

text: topographic maps

text: covering the entire

text: United States

text: . The maps are produced by the

text: USGS

text: , which encourages the distribution of their maps through business partners.  TopoZone offered aerial photographs from the

text: USGS

text: and street maps from the

text: United States Census Bureau

text: .  In 2007 complete coverage of

text: Canada

text: was added, using the topographic map series produced by

text: Natural Resources Canada

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answers: NDQ_001587

answers: TopoZone offered aerial photographs from the USGS

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: TopoZone offered aerial photographs

answers: NDQ_001590

answers: TopoZone

answers: NDQ_001591

answers: the entire United States

answers: NDQ_001592

answers: street maps

answers: NDQ_001593

answers: topographic maps

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: TopoZone

answers: NDQ_001598

answers: topographic maps

answers: NDQ_001600

answers: Plain

answers: NDQ_001603

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answers: NDQ_001605

answers: Geological Survey topographic maps

answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001611

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answers: United States Geological Survey topographic maps

answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

answers: topographic

answers: NDQ_001620

answers: Topographic mapping

answers: NDQ_001621

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answers: NDQ_001622

answers: topographic

answers: NDQ_001623

answers: Topographic zone

answers: NDQ_001624

answers: United States Geological Survey

answers: NDQ_001625

answers: 100 m

text: He was a native of Guangdong province and served as a county official of Huian County in Fujian province. Although topographic features were part of maps in China for centuries, Ye was the first to base county maps on on-site topographical surveying and observations. His career was sidelined for seventeen years after he became a victim of political vengeance. He came up with a model of county commerce with goods of greatest, great, and lesser importance—the latter being non-subsistence surplus goods that could be traded out of the county for commercial profit.

text: He was a native of

text: Guangdong

text: province and served as a county official of Huian County in

text: Fujian

text: province. Although

text: topographic

text: features were part of

text: maps in China for centuries

text: , Ye was the first to base county maps on on-site topographical

text: surveying

text: and observations. His career was sidelined for seventeen years after he became a victim of political vengeance. He came up with a model of county commerce with goods of greatest, great, and lesser importance—the latter being non-subsistence surplus goods that could be traded out of the county for commercial profit.

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answers: 0

answers: NDQ_001586

answers: topographic features

answers: NDQ_001587

answers: Guangdong province

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: topographic features were part of maps

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: non-subsistence surplus goods

answers: NDQ_001592

answers: trade out of the county

answers: NDQ_001593

answers: topographic features

answers: NDQ_001594

answers: topographic features

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: on-site topographical surveying

answers: NDQ_001598

answers: topographic

answers: NDQ_001600

answers: topographic features

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: topographic features

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic features

answers: NDQ_001611

answers: topographic features

answers: NDQ_001613

answers: topographic features

answers: NDQ_001614

answers: topographic features

answers: NDQ_001618

answers: topographic

answers: NDQ_001619

answers: topographic

answers: NDQ_001620

answers: topographic features

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: topographic

answers: NDQ_001623

answers: greatest

answers: NDQ_001624

answers: topographic features

answers: NDQ_001625

answers: lesser importance

text: AMS was redesignated the U.S. Army Topographic Command (USATC) on September 1, 1968 and continued as an independent organization until 1972, when it was merged into the new Defense Mapping Agency (DMA) and redesignated as the DMA Topographic Center (DMATC).

text: AMS was redesignated the U.S.

text: Army Topographic Command

text: (USATC) on September 1, 1968 and continued as an independent organization until 1972, when it was merged into the new

text: Defense Mapping Agency

text: (DMA) and redesignated as the DMA Topographic Center (DMATC).

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text: There are also eight township roads in Poyntelle. Three of them are entirely located within the village: Czapnik Road (designated Township Road 571, or T571), which connects to both Cribbs and South Preston; Poyntelle Road (T722), which connects to Crosstown, Cribbs, and South Preston; and Lake Lorain Road (T729; referred to as "Lorain Road" on the United States Geological Survey (USGS)  Orson Quadrangle topographic map, which includes Poyntelle), which connects to just Crosstown. The other five cross into other villages: Paluch Road (T567; the USGS map says "Poluch Road"), which connects to Cribbs; Clark Road (T579), which connects to Crosstown; Dix Road (T594; referred to as "North Road" on the PennDOT General Highway Map for Wayne County), which connects to Paluch; Spruce Lake Road (T688), which connects to Crosstown and Clark; and O & W Road (T727; the USGS map says "Old State Road"), which connects to Cribbs and Poyntelle. Like many township roads in the state, Paluch, Czapnik, Clark, Dix, Spruce Lake, Poyntelle, O & W, and Lake Lorain are all unpaved.

text: There are also eight

text: township roads

text: in Poyntelle. Three of them are entirely located within the village: Czapnik Road (designated Township Road 571, or T571), which connects to both Cribbs and South Preston; Poyntelle Road (T722), which connects to Crosstown, Cribbs, and South Preston; and Lake Lorain Road (T729; referred to as "Lorain Road" on the

text: United States Geological Survey (USGS)

text: Orson

text: Quadrangle

text: topographic

text: map, which includes Poyntelle), which connects to just Crosstown. The other five cross into other villages: Paluch Road (T567; the USGS map says "Poluch Road"), which connects to Cribbs; Clark Road (T579), which connects to Crosstown; Dix Road (T594; referred to as "North Road" on the PennDOT General Highway Map for Wayne County), which connects to Paluch; Spruce Lake Road (T688), which connects to Crosstown and Clark; and O & W Road (T727; the USGS map says "Old State Road"), which connects to Cribbs and Poyntelle. Like many township roads in the state, Paluch, Czapnik, Clark, Dix, Spruce Lake, Poyntelle, O & W, and Lake Lorain are all

text: unpaved

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answers: T567

text: Given a set of intervals I = {I, I, ... , I}, let OPT(I) be any optimal solution of the interval scheduling problem, and let EFT(I) be the solution of the earliest finishing time algorithm. For any interval J ∈ OPT(I), define h(J) as the interval J' ∈ EFT(I) that intersects J with the earliest finishing time amongst all intervals in EFT(I) intersecting J.  To show that the earliest finish time algorithm is optimal using the charging argument, h must be shown to be a one-to-one function mapping intervals in OPT(I) to those in EFT(I). Suppose J is an arbitrary interval in OPT(I).

text: Given a set of intervals I = {I, I, ... , I}, let OPT(I) be any optimal solution of the interval scheduling problem, and let EFT(I) be the solution of the earliest finishing time algorithm. For any interval J ∈ OPT(I), define h(J) as the interval J' ∈ EFT(I) that intersects J with the earliest finishing time amongst all intervals in EFT(I) intersecting J.  To show that the earliest finish time algorithm is optimal using the charging argument, h must be shown to be a one-to-one function mapping intervals in OPT(I) to those in EFT(I). Suppose J is an arbitrary interval in OPT(I).

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answers: contour lines that are numbered represent changes in elevation

answers: NDQ_001587

answers: To show that the earliest finish time algorithm is optimal using the charging argument, h must be shown to be a one-to-one function mapping intervals in OPT(I) to those in EFT(I).

answers: NDQ_001588

answers: intersects

answers: NDQ_001589

answers: one-to-one function mapping intervals in OPT(I) to those in EFT(I)

answers: NDQ_001590

answers: The contour interval of a topographic map represents the horizontal distance between contour lines

answers: NDQ_001591

answers: earliest finishing time

answers: NDQ_001592

answers: intersects J

answers: NDQ_001593

answers: For any interval J  OPT(I), define h(J) as the interval J'  EFT(I)

answers: NDQ_001594

answers: contour lines represent the distance to the bottom of the water

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: For any interval J  OPT(I)

answers: NDQ_001598

answers: For any interval J  OPT(I)

answers: NDQ_001600

answers: Plain or plateau

answers: NDQ_001603

answers: Not all intervals can be shown to be a one-to-one function mapping intervals in OPT(I) to those in EFT(I).

answers: NDQ_001605

answers: For any interval J  OPT(I)

answers: NDQ_001606

answers: For any interval J  OPT(I)

answers: NDQ_001608

answers: Contour lines help us to see the three-dimensional shape of the land

answers: NDQ_001611

answers: For any interval J  OPT(I)

answers: NDQ_001613

answers: For any interval J  OPT(I), define h(J) as the interval J'  EFT(I) that intersects J with the earliest finishing time amongst all intervals in EFT(I) intersecting J.

answers: NDQ_001614

answers: Topographic maps cannot show horizontal distances.

answers: NDQ_001618

answers: intervals

answers: NDQ_001619

answers: h(J)

answers: NDQ_001620

answers: h(J)

answers: NDQ_001621

answers: EFT(I)

answers: NDQ_001622

answers: h(J)

answers: NDQ_001623

answers: h(J)

answers: NDQ_001624

answers: intervals

answers: NDQ_001625

answers: J'  EFT(I)

text: The database is part of a system that includes topographic map names and bibliographic references. The names of books and historic maps that confirm the feature or place name are cited. Variant names, alternatives to official federal names for a feature, are also recorded. Each feature receives a permanent, unique feature record identifier, sometimes called the GNIS identifier. The database never removes an entry, "except in cases of obvious duplication."

text: The database is part of a system that includes topographic map names and bibliographic references. The names of books and historic maps that confirm the feature or place name are cited. Variant names, alternatives to official federal names for a feature, are also recorded. Each feature receives a permanent, unique feature record identifier, sometimes called the GNIS identifier. The database never removes an entry, "except in cases of obvious duplication."

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text: Numerical marking is the manner of denoting the arithmetical values of contour lines.  This can be done by placing numbers along some of the contour lines, typically using interpolation for intervening lines. Alternatively a map key can be produced associating the contours with their values.

text: Numerical marking is the manner of denoting the

text: arithmetic

text: al values of contour lines.  This can be done by placing numbers along some of the contour lines, typically using

text: interpolation

text: for intervening lines. Alternatively a map key can be produced associating the contours with their values.

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text: Older relief maps often show heights above the old reference planes. Current maps by the federal survey authorities are based on NHN. At the beginning of 2013 most of the federal states (except Berlin, Thuringia and Saxony-Anhalt) had complete coverage by the new digital topographic mapping at 1:25,000 scale (DTK). Not all the maps have appeared in print yet. On the DTK25 maps, NHN is used for elevations, however, on the DTK25-V scanned topographic maps Höhennull (HN) and Normalnull (NN) are still being used.

text: Older

text: relief map

text: s often show heights above the old reference planes. Current maps by the federal survey authorities are based on NHN. At the beginning of 2013 most of the federal states (except Berlin, Thuringia and Saxony-Anhalt) had complete coverage by the new digital topographic mapping at 1:25,000 scale (DTK). Not all the maps have appeared in print yet. On the DTK25 maps, NHN is used for elevations, however, on the DTK25-V scanned topographic maps

text: Höhennull

text: (HN) and

text: Normalnull

text: (NN) are still being used.

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text: The USGS produces several national series of topographic maps which vary in scale and extent, with some wide gaps in coverage, notably the complete absence of 1:50,000 scale topographic maps or their equivalent. The largest (both in terms of scale and quantity) and best-known topographic series is the 7.5-minute, 1:24,000 scale, quadrangle, a non-metric scale virtually unique to the United States. Each of these maps covers an area bounded by two lines of latitude and two lines of longitude spaced 7.5 minutes apart. Nearly 57,000 individual maps in this series cover the 48 contiguous states, Hawaii, U.S. territories, and areas of Alaska near Anchorage, Fairbanks, and Prudhoe Bay. The area covered by each map varies with the latitude of its represented location due to convergence of the meridians. At lower latitudes, near 30° north, a 7.5-minute quadrangle contains an area of about . At 49° north latitude,  are contained within a quadrangle of that size. As a unique non-metric map scale, the 1:24,000 scale naturally requires a separate and specialized romer scale for plotting map positions. In recent years, budget constraints have forced the USGS to rely on donations of time by civilian volunteers in an attempt to update its 7.5-minute topographic map series, and USGS stated outright in 2000 that the program was to be phased out in favor of The National Map (not to be confused with the National Atlas of the United States produced by the Department of the Interior, one of whose bureaus is USGS).

text: The USGS produces several national series of

text: topographic maps

text: which vary in

text: scale

text: and extent, with some wide gaps in coverage, notably the complete absence of 1:50,000 scale topographic maps or their equivalent. The largest (both in terms of scale and quantity) and best-known topographic series is the 7.5-minute, 1:24,000 scale,

text: quadrangle

text: , a non-metric scale virtually unique to the United States. Each of these maps covers an area bounded by two lines of

text: latitude

text: and two lines of

text: longitude

text: spaced 7.5

text: minutes

text: apart. Nearly 57,000 individual maps in this series cover the

text: 48 contiguous states

text: Hawaii

text: U.S. territories

text: , and areas of

text: Alaska

text: near Anchorage, Fairbanks, and Prudhoe Bay. The area covered by each map varies with the latitude of its represented location due to convergence of the meridians. At lower latitudes, near 30° north, a 7.5-minute quadrangle contains an area of about . At 49° north latitude,  are contained within a quadrangle of that size. As a unique non-metric map scale, the 1:24,000 scale naturally requires a separate and specialized

text: romer

text: scale for plotting map positions. In recent years, budget constraints have forced the USGS to rely on donations of time by civilian volunteers in an attempt to update its 7.5-minute topographic map series, and USGS stated outright in 2000 that the program was to be phased out in favor of

text: The National Map

text: (not to be confused with the

text: National Atlas of the United States

text: produced by the

text: Department of the Interior

text: , one of whose bureaus is USGS).

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answers: latitude and two lines of longitude

answers: NDQ_001587

answers: The area covered by each map varies with the latitude of its represented location

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: 1:50,000 scale topographic maps or their equivalent

answers: NDQ_001590

answers: 7.5 minutes

answers: NDQ_001591

answers: latitude

answers: NDQ_001592

answers: 1:50,000

answers: NDQ_001593

answers: latitude of its represented location

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 7.5 minutes

answers: NDQ_001597

answers: latitude of its represented location due to convergence of the meridians

answers: NDQ_001598

answers: The area covered by each map varies with the latitude

answers: NDQ_001600

answers: quadrangle

answers: NDQ_001603

answers: It does not state that the program was to be phased out

answers: NDQ_001605

answers: The USGS produces several national series

answers: NDQ_001606

answers: 7.5 minutes

answers: NDQ_001608

answers: latitude and two lines of longitude

answers: NDQ_001611

answers: spaced 7.5 minutes apart

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answers: latitude of its represented location due to convergence of the meridians

answers: NDQ_001614

answers: latitude

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answers: Prudhoe Bay

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answers: 7.5 minutes

text: Stratigraphic contour lines may be used to illustrate the surface of a selected stratum illustrating the subsurface topographic trends of the strata. Isopach maps detail the variations in thickness of stratigraphic units. It is not always possible to properly show this when the strata are extremely fractured, mixed, in some discontinuities, or where they are otherwise disturbed.

text: Stratigraphic

text: contour line

text: s may be used to illustrate the surface of a selected

text: stratum

text: illustrating the subsurface

text: topographic

text: trends of the strata.

text: Isopach map

text: s detail the variations in thickness of stratigraphic units. It is not always possible to properly show this when the strata are extremely fractured, mixed, in some discontinuities, or where they are otherwise disturbed.

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answers: 0

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answers: 4

answers: NDQ_001587

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answers: NDQ_001588

answers: 4

answers: NDQ_001589

answers: 0

answers: NDQ_001590

answers: 4

answers: NDQ_001591

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answers: NDQ_001608

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answers: 4

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answers: NDQ_001622

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answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: Stratigraphic contour lines

answers: NDQ_001587

answers: isopach maps detail the variations in thickness of stratigraphic units

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: the variations in thickness of stratigraphic units

answers: NDQ_001590

answers: Isopach

answers: NDQ_001591

answers: variations in thickness of stratigraphic units

answers: NDQ_001592

answers: the variations in thickness of stratigraphic units

answers: NDQ_001593

answers: topographic trends

answers: NDQ_001594

answers: subsurface topographic trends

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: topographic trends

answers: NDQ_001598

answers: Stratigraphic contour lines

answers: NDQ_001600

answers: Isopach

answers: NDQ_001603

answers: It is not always possible to properly show this when the strata are extremely fractured

answers: NDQ_001605

answers: Isopach

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic

answers: NDQ_001611

answers: Stratigraphic contour lines

answers: NDQ_001613

answers: Isopach

answers: NDQ_001614

answers: Stratigraphic contour lines

answers: NDQ_001618

answers: Isopach maps

answers: NDQ_001619

answers: Isopach

answers: NDQ_001620

answers: variations in thickness

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: Isopach

answers: NDQ_001623

answers: contour lines

answers: NDQ_001624

answers: Isopach

answers: NDQ_001625

answers: variations in thickness of stratigraphic units

text: The United States Geological Survey (USGS), a civilian federal agency, produces several national series of topographic maps which vary in scale and extent, with some wide gaps in coverage, notably the complete absence of 1:50,000 scale topographic maps or their equivalent. The largest (both in terms of scale and quantity) and best-known topographic series is the 7.5-minute or 1:24,000 quadrangle. This scale is unique to the United States, where nearly every other developed nation has introduced a metric 1:25,000 or 1:50,000 large scale topo map.  The USGS also publishes 1:100,000 maps covering 30 minutes latitude by one degree longitude, 1:250,000 covering one by two degrees, and state maps at 1:500,000 with California, Michigan and Montana needing two sheets while Texas has four. Alaska is mapped on a single sheet, at scales ranging from 1:1,584,000 to 1:12,000,000.

text: The

text: United States Geological Survey

text: (USGS), a civilian federal agency, produces several national series of topographic maps which vary in scale and extent, with some wide gaps in coverage, notably the complete absence of 1:50,000 scale topographic maps or their equivalent. The largest (both in terms of scale and quantity) and best-known topographic series is the 7.5-minute or 1:24,000

text: quadrangle

text: . This scale is unique to the United States, where nearly every other developed nation has introduced a metric 1:25,000 or 1:50,000 large scale topo map.  The USGS also publishes 1:100,000 maps covering 30 minutes latitude by one degree longitude, 1:250,000 covering one by two degrees, and state maps at 1:500,000 with

text: California

text: Michigan

text: and

text: Montana

text: needing two sheets while

text: Texas

text: has four.

text: Alaska

text: is mapped on a single sheet, at scales ranging from 1:1,584,000 to 1:12,000,000.

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answers: 0

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answers: 0

answers: tqa2:L_0039/T_0395/e1278a8201ddf520d5b19846047bf656

answers: 0

answers: NDQ_001586

answers: 0

answers: NDQ_001587

answers: 0

answers: NDQ_001588

answers: 4

answers: NDQ_001589

answers: 0

answers: NDQ_001590

answers: 4

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 0

answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 0

answers: NDQ_001598

answers: 0

answers: NDQ_001600

answers: 0

answers: NDQ_001603

answers: 0

answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 4

answers: NDQ_001608

answers: 0

answers: NDQ_001611

answers: 0

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 0

answers: NDQ_001618

answers: 0

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 5

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 1

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: contour lines that are numbered

answers: NDQ_001587

answers: 1:24,000 quadrangle

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Alaska is mapped on a single sheet

answers: NDQ_001590

answers: 1:24,000

answers: NDQ_001591

answers: quadrangle

answers: NDQ_001592

answers: 1:50,000 scale topographic maps

answers: NDQ_001593

answers: 1:24,000 quadrangle

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: latitude by one degree longitude

answers: NDQ_001598

answers: 1:24,000 quadrangle

answers: NDQ_001600

answers: 1:250,000

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: It does not say.

answers: NDQ_001606

answers: 1:50,000

answers: NDQ_001608

answers: 1:24,000 quadrangle

answers: NDQ_001611

answers: 1:24,000 quadrangle

answers: NDQ_001613

answers: 1:24,000 quadrangle

answers: NDQ_001614

answers: latitude and longitude

answers: NDQ_001618

answers: latitude

answers: NDQ_001619

answers: 1:250,000

answers: NDQ_001620

answers: 1:24,000

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: 1:24,000 quadrangle

answers: NDQ_001623

answers: latitude

answers: NDQ_001624

answers: 1:24,000 quadrangle

answers: NDQ_001625

answers: 7.5-minute

text: In the earliest days, contoured electron density maps were hand drawn on large plastic sheets.  Sometimes, bingo chips were placed on the plastic sheets where atoms were interpreted to be.

text: In the earliest days, contoured electron density maps were hand drawn on large plastic sheets.  Sometimes,

text: bingo chip

text: s were placed on the plastic sheets where atoms were interpreted to be.

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answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

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answers: NDQ_001623

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answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: contoured electron density maps

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: bingo chips were placed on the plastic sheets

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: atoms

answers: NDQ_001592

answers: contoured

answers: NDQ_001593

answers: contoured

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: contour

answers: NDQ_001598

answers: contour

answers: NDQ_001600

answers: contoured

answers: NDQ_001603

answers: contoured

answers: NDQ_001605

answers: bingo chips

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: contour lines

answers: NDQ_001611

answers: contoured

answers: NDQ_001613

answers: contouring

answers: NDQ_001614

answers: bingo chips

answers: NDQ_001618

answers: electron density

answers: NDQ_001619

answers: contouring

answers: NDQ_001620

answers: contour

answers: NDQ_001621

answers: contoured

answers: NDQ_001622

answers: contoured

answers: NDQ_001623

answers: contour

answers: NDQ_001624

answers: electron density maps

answers: NDQ_001625

answers: contoured

text: To maximize readability of contour maps, there are several design choices available to the map creator, principally line weight, line color, line type and method of numerical marking.

text: To maximize readability of contour maps, there are several design choices available to the map creator, principally line weight, line

text: color

text: , line type and method of numerical marking.

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answers: NDQ_001586

answers: numerical marking

answers: NDQ_001587

answers: contour maps

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: numerical marking

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: numerical marking

answers: NDQ_001592

answers: numerical marking

answers: NDQ_001593

answers: contour maps

answers: NDQ_001594

answers: contour maps

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: contour maps

answers: NDQ_001598

answers: contour maps

answers: NDQ_001600

answers: line weight

answers: NDQ_001603

answers: readability of contour maps

answers: NDQ_001605

answers: line color

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: contour maps

answers: NDQ_001611

answers: line type

answers: NDQ_001613

answers: method of numerical marking

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: contour maps

answers: NDQ_001619

answers: contour maps

answers: NDQ_001620

answers: contour

answers: NDQ_001621

answers: contour maps

answers: NDQ_001622

answers: contour maps

answers: NDQ_001623

answers: contour

answers: NDQ_001624

answers: contour maps

answers: NDQ_001625

answers: numerical marking

text: In the early days of orienteering, competitors used whatever maps were available; these were typically topographic maps from the national mapping agency. While national mapping agencies update their topographic maps on a regular basis, they are usually not sufficiently up to date for orienteering purposes. Gradually, specially drawn maps have been provided to meet the specific requirements of orienteering.

text: In the early days of orienteering, competitors used whatever maps were available; these were typically topographic maps from the national mapping agency. While national mapping agencies update their topographic maps on a regular basis, they are usually not sufficiently up to date for orienteering purposes. Gradually, specially drawn maps have been provided to meet the specific requirements of orienteering.

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answers: NDQ_001624

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answers: NDQ_001625

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answers: NDQ_001586

answers: topographic maps

answers: NDQ_001587

answers: specially drawn maps

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: they are usually not sufficiently up to date for orienteering purposes

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: topographic

answers: NDQ_001592

answers: orienteering

answers: NDQ_001593

answers: topographic maps

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: orienteering

answers: NDQ_001598

answers: topographic maps

answers: NDQ_001600

answers: topographic maps

answers: NDQ_001603

answers: not sufficiently up to date for orienteering purposes

answers: NDQ_001605

answers: topographic maps

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic maps

answers: NDQ_001611

answers: orienteering

answers: NDQ_001613

answers: orienteering

answers: NDQ_001614

answers: topographic maps

answers: NDQ_001618

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answers: NDQ_001619

answers: topographic

answers: NDQ_001620

answers: topographic

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: topographic

answers: NDQ_001623

answers: topographic map

answers: NDQ_001624

answers: contour lines

answers: NDQ_001625

answers: sufficiently up to date

text: Since 1991, the peninsula has been investigated by the team of ETH Zürich geologically and cartographically.  From this, a topographical map of the entire peninsula at a scale of 1:25,000 was made.  An interactive 3D map was created and is on the World Wide Web. Also a rich photographic archive with about 10.000 color slides has been produced (see links below).

text: Since 1991, the peninsula has been investigated by the team of

text: ETH Zürich

text: geologically and cartographically.  From this, a topographical map of the entire peninsula at a scale of 1:25,000 was made.  An interactive 3D map was created and is on the World Wide Web. Also a rich photographic archive with about 10.000 color slides has been produced (see links below).

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answers: 1: The answer is not relevant or complete at all.

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text: The United States Geological Survey's (USGS) most recent topographic maps identify the tip of the peninsula that contains Fort McNair as "Greenleaf Point". The USGS maps also identify a lesser point to the northeast of Greenleaf Point as "Buzzard Point". (James Creek, which was excavated in the 19th century to become a branch of the [now defunct] Washington City Canal, once separated these two points. Its name persists in the present day James Creek Marina, located between the two named points. In early days, James Creek was also known as St. James Creek.)

text: The

text: United States Geological Survey

text: 's (USGS) most recent topographic maps identify the tip of the peninsula that contains Fort McNair as "Greenleaf Point". The USGS maps also identify a lesser point to the northeast of Greenleaf Point as "Buzzard Point". (James Creek, which was excavated in the 19th century to become a branch of the [now defunct]

text: Washington City Canal

text: , once separated these two points. Its name persists in the present day

text: James Creek Marina

text: , located between the two named points. In early days, James Creek was also known as St. James Creek.)

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text: Many of the features will be shown by straight, curved, dashed, or solid lines. They may also be colored to represent different classes of information. The typical color standard for topographic maps depicts contours in brown, bodies of water in blue, boundaries in black, and grids and roads in red. Topographic maps may use different colors to represent area features. Most topographic maps will use green for vegetation or national parks and wildlife management areas. They will also use blue for rivers, lakes, or other bodies of water. Red may also be used to represent areas of significant importance.

text: Many of the features will be shown by straight, curved, dashed, or solid lines. They may also be colored to represent different classes of information. The typical color standard for topographic maps depicts contours in brown, bodies of water in blue, boundaries in black, and grids and roads in red. Topographic maps may use different colors to represent

text: area features

text: . Most topographic maps will use green for vegetation or national parks and wildlife management areas. They will also use blue for rivers, lakes, or other bodies of water. Red may also be used to represent areas of significant importance.

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text: When maps with contour lines became common, the idea spread to other applications. Perhaps the latest to develop are air quality and noise pollution contour maps, which first appeared in the US, in approximately 1970, largely as a result of national legislation requiring spatial delineation of these parameters. In 2007, Pictometry International was the first to allow users to dynamically generate elevation contour lines to be laid over oblique images.

text: When maps with contour lines became common, the idea spread to other applications. Perhaps the latest to develop are

text: air quality

text: and

text: noise pollution

text: contour maps, which first appeared in the

text: US

text: , in approximately 1970, largely as a result of national legislation requiring spatial delineation of these parameters. In 2007,

text: Pictometry International

text: was the first to allow users to dynamically generate elevation contour lines to be laid over oblique images.

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answers: dynamically generate elevation contour lines

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answers: 1000 feet

answers: NDQ_001597

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text: In many locations within the brain, adjacent neurons have receptive fields that include slightly different, but overlapping portions of the visual field. The position of the center of these receptive fields forms an orderly sampling mosaic that covers a portion of the visual field. Because of this orderly arrangement, which emerges from the spatial specificity of connections between neurons in different parts of the visual system, cells in each structure can be seen as contributing to a map of the visual field (also called a retinotopic map, or a visuotopic map). Retinotopic maps are a particular case of topographic organization. Many brain structures that are responsive to visual input, including much of the visual cortex and visual nuclei of the brain stem (such as the superior colliculus) and thalamus (such as the lateral geniculate nucleus and the pulvinar), are organized into retinotopic maps, also called visual field maps.

text: In many locations within the brain, adjacent

text: neuron

text: s have

text: receptive fields

text: that include slightly different, but overlapping portions of the

text: visual field

text: . The position of the center of these receptive fields forms an orderly sampling mosaic that covers a portion of the visual field. Because of this orderly arrangement, which emerges from the spatial specificity of connections between neurons in different parts of the visual system, cells in each structure can be seen as contributing to a map of the visual field (also called a retinotopic map, or a visuotopic map). Retinotopic maps are a particular case of

text: topographic

text: organization. Many brain structures that are responsive to visual input, including much of the

text: visual cortex

text: and visual

text: nuclei

text: of the

text: brain stem

text: (such as the

text: superior colliculus

text: ) and

text: thalamus

text: (such as the

text: lateral geniculate nucleus

text: and the

text: pulvinar

text: ), are organized into retinotopic maps, also called visual field maps.

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answers: cells in each structure can be seen as contributing

answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001598

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answers: NDQ_001603

answers: No

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answers: NDQ_001619

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answers: NDQ_001620

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text: These large-scale maps are the basis for maps at smaller scales.  Maps at scales 1:4,000,000 or smaller are exported by  Cartographic Publishing House, Beijing while larger-scale maps are restricted as state secrets, and prohibited from publishing by legislation, all except Hong Kong and Macau.  China's topographic maps follow the international system of subdivision with 1:100,000 maps spanning 30 minutes longitude by 20 minutes latitude.

text: These large-scale maps are the basis for maps at smaller scales.  Maps at scales 1:4,000,000 or smaller are exported by  Cartographic Publishing House, Beijing while larger-scale maps are restricted as state secrets, and prohibited from publishing by legislation, all except Hong Kong and Macau.  China's topographic maps follow the

text: international system of subdivision

text: with 1:100,000 maps spanning 30 minutes longitude by 20 minutes latitude.

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answers: NDQ_001591

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

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answers: NDQ_001605

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answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001611

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

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answers: NDQ_001623

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answers: NDQ_001625

answers: 20 minutes

text: This route can be traced on topographical maps overprinted with the ancient route, in G. Castellve, J.-B. Compsa, J. Kotarba and A. Pezin, eds. Voies romaines du Rhône à l'Èbre: Via Domitia et Via Augusta (DAF 61) Paris 1997.

text: This route can be traced on topographical maps overprinted with the ancient route, in G. Castellve, J.-B. Compsa, J. Kotarba and A. Pezin, eds. Voies romaines du Rhône à l'Èbre: Via Domitia et Via Augusta (DAF 61) Paris 1997.

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answers: This route can be traced on topographical maps

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001597

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answers: NDQ_001600

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answers: NDQ_001603

answers: Voies romaines du Rhône

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answers: NDQ_001611

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001622

answers: overprinted

answers: NDQ_001623

answers: Via Augusta

answers: NDQ_001624

answers: overprinted

answers: NDQ_001625

answers: DAF

text: Topographic maps are based on the Ordnance Survey Oxford Cartographers. The most commonly used Map projection is that of Eckert (the Pseudo-cylindrical projection). The show also uses satellite imagery from Google Earth and the first use was in the episode named: "Nigeria, rich state poor country."

text: Topographic maps are based on the Ordnance Survey Oxford Cartographers. The most commonly used

text: Map projection

text: is that of Eckert (the

text: Pseudo-cylindrical projection

text: ). The show also uses satellite imagery from

text: Google Earth

text: and the first use was in the episode named: "

text: Nigeria

text: , rich state poor country."

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answers: Topographic maps

answers: NDQ_001587

answers: the Pseudo-cylindrical projection

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: The most commonly used Map projection is that of Eckert

answers: NDQ_001590

answers: Topographic maps

answers: NDQ_001591

answers: rich state poor country

answers: NDQ_001592

answers: Nigeria, rich state poor country

answers: NDQ_001593

answers: Topographic maps

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Map projection is that of Eckert

answers: NDQ_001598

answers: the Pseudo-cylindrical projection

answers: NDQ_001600

answers: Pseudo-cylindrical projection

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Ordnance Survey Oxford Cartographers

answers: NDQ_001606

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answers: NDQ_001611

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answers: NDQ_001613

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answers: NDQ_001614

answers: Topographic maps

answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic

answers: NDQ_001622

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answers: NDQ_001623

answers: cylindrical projection

answers: NDQ_001624

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answers: NDQ_001625

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text: A topographic profile is a cross sectional view along a line drawn through a portion of a topographic map.  In other words, if you could slice through a portion of the earth, pull away one portion, and  look at it from the side, the surface would be a topographic profile.

text: A topographic profile is a

text: cross sectional

text: view along a line drawn through a portion of a

text: topographic map

text: .  In other words, if you could slice through a portion of the earth, pull away one portion, and  look at it from the side, the surface would be a topographic profile.

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answers: NDQ_001593

answers: In other words, if you could slice through a portion of the earth

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answers: a topographic profile

text: A number of people mapped and commented on the region before the loss of the terraces. Dr Ferdinand von Hochstetter carried out a topographic and geological survey of the Lake Rotomahana area in 1859, producing his Geographic and Geological survey. This gave enough data to form the first map of the area and to suggest how the terraces had been formed.

text: A number of people mapped and commented on the region before the loss of the terraces. Dr Ferdinand von Hochstetter carried out a topographic and geological survey of the Lake Rotomahana area in 1859, producing his Geographic and Geological survey. This gave enough data to form the first map of the area and to suggest how the terraces had been formed.

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answers: NDQ_001588

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answers: NDQ_001589

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answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: The terraces had been formed

answers: NDQ_001598

answers: topographic

answers: NDQ_001600

answers: terraces

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Geological maps

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic

answers: NDQ_001611

answers: topographic

answers: NDQ_001613

answers: how the terraces had been formed

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: terraces

answers: NDQ_001619

answers: topographic

answers: NDQ_001620

answers: topographic

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: terraces

answers: NDQ_001623

answers: topographic

answers: NDQ_001624

answers: terraces

answers: NDQ_001625

answers: 1 km

text: About half of the region was beyond the terminator during the three Mariner 10 encounters and hence not visible. The entire mapped area was covered by near-vertical photography from the second encounter, and the eastern part, from longitude 15° to about 110°, was covered by oblique photography from the first encounter. No third-encounter images were acquired. The entire visible area may be viewed stereoscopically by combining images from the first and second encounters taken at different viewing angles or by combining second-encounter images of the same area taken at different viewing angles. These combinations provided excellent qualitative control of topographic relief and a good quantitative photogrammetric base. However, sun-elevation angles of the images are limited to less than 25°, and image resolutions are no higher than about 0.5 km per picture element. Therefore, the south polar geologic map reflects mostly large-scale processes and topographic information, whereas other mercurian quadrangle maps benefit from greater albedo discrimination and, in some cases, higher resolution.

text: About half of the region was beyond the

text: terminator

text: during the three

text: Mariner 10

text: encounters and hence not visible. The entire mapped area was covered by near-vertical photography from the second encounter, and the eastern part, from longitude 15° to about 110°, was covered by oblique photography from the first encounter. No third-encounter images were acquired. The entire visible area may be viewed

text: stereoscopically

text: by combining images from the first and second encounters taken at different viewing angles or by combining second-encounter images of the same area taken at different viewing angles. These combinations provided excellent qualitative control of topographic relief and a good quantitative photogrammetric base. However, sun-elevation angles of the images are limited to less than 25°, and image resolutions are no higher than about 0.5 km per picture element. Therefore, the south polar

text: geologic map

text: reflects mostly large-scale processes and topographic information, whereas other mercurian quadrangle maps benefit from greater

text: albedo

text: discrimination and, in some cases, higher resolution.

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answers: topographic relief

answers: NDQ_001587

answers: The entire visible area may be viewed stereoscopically

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: benefit from greater albedo discrimination and, in some cases, higher resolution

answers: NDQ_001590

answers: 0.5 km

answers: NDQ_001591

answers: topographic information

answers: NDQ_001592

answers: greater albedo discrimination

answers: NDQ_001593

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answers: NDQ_001594

answers: topographic relief

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: longitude

answers: NDQ_001598

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answers: NDQ_001600

answers: near-vertical

answers: NDQ_001603

answers: These combinations provided excellent qualitative control of topographic relief and a good quantitative photogrammetric base

answers: NDQ_001605

answers: albedo discrimination

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

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answers: NDQ_001611

answers: These combinations provided excellent qualitative control of topographic relief

answers: NDQ_001613

answers: sun-elevation angles

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text: Such maps are used in town planning, in the insurance industry, and by individuals who want to avoid moving into a home at risk of flooding or to know how to protect their property. FIRMs are used to set rates of insurance against risk of flood and whether buildings are insurable at all against flood.  It is similar to a topographic map, but is designed to show floodplains. Towns and municipalities use FIRMs to plan zoning areas.  Most places will not allow construction in a flood way.

text: Such maps are used in

text: town planning

text: , in the insurance industry, and by individuals who want to avoid moving into a home at risk of flooding or to know how to protect their property. FIRMs are used to set rates of insurance against risk of flood and whether buildings are insurable at all against flood.  It is similar to a

text: topographic

text: map, but is designed to show floodplains. Towns and municipalities use FIRMs to plan zoning areas.  Most places will not allow construction in a flood way.

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text: The name was noted by the United States Geological Survey on 1948 and 1962 topographical maps of the Juneau area, but it was removed prior to the latter edition's publication.  It later appeared on a 1997 USGS map.  It was entered into the Geographic Names Information System on March 31, 1981.

text: The name was noted by the

text: United States Geological Survey

text: on 1948 and 1962 topographical maps of the Juneau area, but it was removed prior to the latter edition's publication.  It later appeared on a 1997 USGS map.  It was entered into the

text: Geographic Names Information System

text: on March 31, 1981.

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text: An interval may overlap the center point of several nodes in the tree. Since each node stores the intervals that overlap it, with all intervals completely to the left of its center point in the left subtree, similarly for the right subtree, it follows that each interval is stored in the node closest to the root from the set of nodes whose center point it overlaps.

text: An interval may overlap the center point of several nodes in the tree. Since each node stores the intervals that overlap it, with all intervals completely to the left of its center point in the left subtree, similarly for the right subtree, it follows that each interval is stored in the node closest to the root from the set of nodes whose center point it overlaps.

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answers: nodes that overlap it

answers: NDQ_001587

answers: is a cross section

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: each node stores the intervals that overlap it

answers: NDQ_001590

answers: Each node stores the intervals that overlap it

answers: NDQ_001591

answers: center point

answers: NDQ_001592

answers: store the intervals that overlap it

answers: NDQ_001593

answers: node closest to the root

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: To the left

answers: NDQ_001598

answers: node closest to the root

answers: NDQ_001600

answers: Plain or plateau

answers: NDQ_001603

answers: nodes

answers: NDQ_001605

answers: node closest to the root

answers: NDQ_001606

answers: Each node stores the intervals that overlap it

answers: NDQ_001608

answers: The center point of several nodes in the tree

answers: NDQ_001611

answers: None

answers: NDQ_001613

answers: each node stores the intervals that overlap it

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: interval

answers: NDQ_001619

answers: interval

answers: NDQ_001620

answers: interval

answers: NDQ_001621

answers: interval

answers: NDQ_001622

answers: interval

answers: NDQ_001623

answers: interval

answers: NDQ_001624

answers: interval

answers: NDQ_001625

answers: completely to the left of its center point

text: Topographic map image of Arnhem (city), September 2014.

text: Topographic map image of Arnhem (city), September 2014.

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answers: 4: The answer is mostly relevant and complete but may have minor gaps or inaccuracies.

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answers: Topographic map image of Arnhem (city)

answers: NDQ_001587

answers: is a type of map

answers: NDQ_001588

answers: intersect each other

answers: NDQ_001589

answers: bathymetric map is a map of the ocean

answers: NDQ_001590

answers: The contour interval is the horizontal distance between contour lines.

answers: NDQ_001591

answers: Topographic map

answers: NDQ_001592

answers: Identify landmarks

answers: NDQ_001593

answers: The slope of the land can be determined using a topographic map.

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: A topographic map can be used to determine the direction that streams flow.

answers: NDQ_001598

answers: The steepest side of a mountain

answers: NDQ_001600

answers: If contour lines are so close together that they almost touch, they represent a plain

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Colors are used to represent different types of rocks.

answers: NDQ_001606

answers: The difference between two contour lines

answers: NDQ_001608

answers: Contour lines help us to see the three-dimensional shape

answers: NDQ_001611

answers: Concentric lines that are very close together show a low hill.

answers: NDQ_001613

answers: The side of the circle with the higher elevation

answers: NDQ_001614

answers: Topographic maps cannot show horizontal distances.

answers: NDQ_001618

answers: Topographic map

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic map

answers: NDQ_001622

answers: Topographic map

answers: NDQ_001623

answers: isosceles

answers: NDQ_001624

answers: Topographic map

answers: NDQ_001625

answers: 1 km

text: The geologic map of Georgia (a state within the United States) is a special-purpose map made to show geological features. Rock units or geologic strata are shown by colors or symbols to indicate where they are exposed at the surface. Structural features such as faults and shear zones are also shown. Since the first national geological map, in 1809, there have been numerous maps which included the geology of Georgia. The first Georgia specific geologic map was created in 1825. The most recent state-produced geologic map of Georgia, by the Georgia Department of Natural Resources is 1:500,000 scale, and was created in 1976 by the department's Georgia Geological Survey. It was generated from a base map produced by the United States Geological Survey. The state geologist and Director of the Geological Survey of Georgia was Sam M. Pickering, Jr. Since 1976, several geological maps of Georgia, featuring the state's five distinct geologic regions, have been produced by the federal government.

text: The geologic map of Georgia (a state within the United States) is a special-purpose

text: map

text: made to show

text: geological

text: features.

text: Rock

text: units or

text: geologic strata

text: are shown by colors or symbols to indicate where they are exposed at the surface. Structural features such as

text: faults

text: and

text: shear zones

text: are also shown. Since the first national geological map, in 1809, there have been numerous maps which included the geology of Georgia. The first Georgia specific geologic map was created in 1825. The most recent state-produced geologic map of Georgia, by the

text: Georgia Department of Natural Resources

text: is 1:500,000 scale, and was created in 1976 by the department's Georgia Geological Survey. It was generated from a base map produced by the

text: United States Geological Survey

text: . The state geologist and Director of the Geological Survey of Georgia was Sam M. Pickering, Jr. Since 1976, several geological maps of Georgia, featuring the state's five distinct geologic regions, have been produced by the federal government.

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answers: The most recent state-produced geologic map

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text: In addition to the seven maps on wooden blocks found at Tomb 1 of Fangmatan, a fragment of a paper map (5.6 × 2.6 cm) was found on the chest of the occupant of Tomb 5 of Fangmatan in 1986. This tomb is dated to the early Western Han dynasty, so the map dates to the early 2nd century BC. The map shows topographic features such as mountains, waterways and roads, and is believed to cover the Qin state of the Warring States period.

text: In addition to the seven maps on wooden blocks found at Tomb 1 of Fangmatan, a fragment of a paper map (5.6 × 2.6 cm) was found on the chest of the occupant of Tomb 5 of Fangmatan in 1986. This tomb is dated to the early

text: Western Han dynasty

text: , so the map dates to the early 2nd century BC. The map shows topographic features such as mountains, waterways and roads, and is believed to cover the

text: Qin state

text: of the Warring States period.

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text: This phenomenon is also inherent in calculating the sound levels from aircraft noise, so that an accurate determination of topographic features may be understood.  In that way one can produce sound level isopleths, or contour maps, which faithfully depict outcomes over variable terrain.

text: This phenomenon is also inherent in calculating the sound levels from

text: aircraft noise

text: , so that an accurate determination of topographic features may be understood.  In that way one can produce sound level

text: isopleth

text: s, or contour maps, which faithfully depict outcomes over variable terrain.

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text: High-resolution surface textures are available for most solar system bodies, including Virtual Textures with complete coverage up to 32768 pixels wide (1.25 km/pixel at the Earth's equator), with selected coverage at higher resolutions. This allows very close views of the Earth, Mars, and the Moon. Many 3D models of historical and existing spacecraft are available flying in reasonably accurate trajectories, from Sputnik 1 and Voyager 2 to the Hubble Space Telescope and International Space Station, as are extended data plots for stars (2 million with correct spatial coordinates). DSOs (nebulae, galaxies, open clusters, etc.), as well as catalogues of thousands of asteroids and comets, and more than 96,000 locations on the Earth can be drawn by the program. Add-ons also include extensive space objects such as red and blue supergiants, red and brown dwarfs, neutron stars, spinning pulsars, rotating black holes with accretion disks, protostars, star nursery nebula, supernova and planetary nebulae, galactic redshifts, geological planetary displays (e.g. 3D interiors, topographic and bathymetric maps, ice age simulations), planetary aurorae, rotating magnetic fields, animated solar flares and prominences, 3D craters and mountains, and historic collision events. All can be visited via the Celestia travel interface. All stages in the life cycle of stars are available, from protostar to black dwarf.

text: High-resolution surface textures are available for most solar system bodies, including Virtual Textures with complete coverage up to 32768 pixels wide (1.25 km/pixel at the Earth's equator), with selected coverage at higher resolutions. This allows very close views of the Earth, Mars, and the Moon. Many 3D models of historical and existing spacecraft are available flying in reasonably accurate trajectories, from

text: Sputnik 1

text: and

text: Voyager 2

text: to the

text: Hubble Space Telescope

text: and

text: International Space Station

text: , as are extended

text: data plot

text: s for stars (2 million with correct spatial coordinates).

text: DSO

text: s (nebulae, galaxies,

text: open cluster

text: s, etc.), as well as catalogues of thousands of asteroids and comets, and more than 96,000 locations on the Earth can be drawn by the program. Add-ons also include extensive space objects such as red and blue supergiants, red and brown dwarfs, neutron stars, spinning pulsars, rotating black holes with accretion disks, protostars, star nursery nebula, supernova and planetary nebulae, galactic redshifts, geological planetary displays (e.g. 3D interiors, topographic and

text: bathymetric

text: maps, ice age simulations),

text: planetary aurorae

text: , rotating magnetic fields, animated

text: solar flare

text: s and

text: prominence

text: s, 3D craters and mountains, and historic collision events. All can be visited via the Celestia travel interface. All stages in the life cycle of stars are available, from

text: protostar

text: to

text: black dwarf

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answers: NDQ_001603

answers: geological planetary displays

answers: NDQ_001605

answers: 3D craters and mountains

answers: NDQ_001606

answers: 1.25 km/pixel

answers: NDQ_001608

answers: topographic and bathymetric maps

answers: NDQ_001611

answers: mountains

answers: NDQ_001613

answers: 1.25 km/pixel

answers: NDQ_001614

answers: geological planetary displays

answers: NDQ_001618

answers: mountains

answers: NDQ_001619

answers: bathymetric

answers: NDQ_001620

answers: topographic

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: mountains

answers: NDQ_001623

answers: equator

answers: NDQ_001624

answers: mountains

answers: NDQ_001625

answers: 1.25 km/pixel

text: Topographic map of the municipality of Alphen-Chaam, Sept. 2014.

text: Topographic map of the municipality of Alphen-Chaam, Sept. 2014.

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answers: NDQ_001624

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answers: NDQ_001625

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answers: NDQ_001586

answers: Changes in elevation

answers: NDQ_001587

answers: Alphen-Chaam is a municipality in Germany

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Bathymetric maps do not use topographic data.

answers: NDQ_001590

answers: The contour interval is the horizontal distance between contour lines.

answers: NDQ_001591

answers: municipality

answers: NDQ_001592

answers: Identify the location of landmarks

answers: NDQ_001593

answers: The municipality of Alphen-Chaam, Sept. 2014.

answers: NDQ_001594

answers: contour lines represent the distance to the bottom of the water

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: The direction that rivers and streams flow

answers: NDQ_001598

answers: The steepest side of the mountain

answers: NDQ_001600

answers: If contour lines are so close together that they almost touch

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Different colors are used to represent different types of rocks.

answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: Contour lines help us to see the three-dimensional shape

answers: NDQ_001611

answers: Concentric lines that are very far apart show a high, steep hill

answers: NDQ_001613

answers: The side of the circle with the higher elevation

answers: NDQ_001614

answers: Topographic maps cannot show horizontal distances

answers: NDQ_001618

answers: Topographic map

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic map

answers: NDQ_001622

answers: Topographic map

answers: NDQ_001623

answers: Topographic map

answers: NDQ_001624

answers: Alphen-Chaam

answers: NDQ_001625

answers: 1 km

text: Today, topographic maps are prepared using photogrammetric interpretation of aerial photography, lidar and other Remote sensing techniques. Older topographic maps were prepared using traditional surveying instruments.

text: Today, topographic maps are prepared using

text: photogrammetric

text: interpretation of

text: aerial photography

text: lidar

text: and other

text: Remote sensing

text: techniques. Older topographic maps were prepared using traditional

text: surveying

text: instruments.

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text: The self-organizing map (SOM, also called Kohonen map) and its probabilistic variant generative topographic mapping (GTM) use a point representation in the embedded space to form a latent variable model based on a non-linear mapping from the embedded space to the high-dimensional space. These techniques are related to work on density networks, which also are based around the same probabilistic model.

text: The

text: self-organizing map

text: (SOM, also called Kohonen map) and its probabilistic variant

text: generative topographic mapping

text: (GTM) use a point representation in the embedded space to form a

text: latent variable model

text: based on a non-linear mapping from the embedded space to the high-dimensional space. These techniques are related to work on

text: density networks

text: , which also are based around the same probabilistic model.

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text: The Commission published the first Bulgarian topographic map of Livingston Island and Greenwich Island in 2005, and jointly with the Military Topographic Service of the Bulgarian Army, the first detailed topographic map of Smith Island in 2008.

text: The Commission published the first Bulgarian topographic map of

text: Livingston Island

text: and

text: Greenwich Island

text: in 2005, and jointly with the Military Topographic Service of the Bulgarian Army, the first detailed topographic map of

text: Smith Island

text: in 2008.

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answers: NDQ_001600

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answers: It's impossible to say

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answers: Livingston Island

answers: NDQ_001623

answers: topographic map

answers: NDQ_001624

answers: Livingston Island

answers: NDQ_001625

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text: His art career was interrupted when he entered into the United States Army in 1941. He did not paint again until he returned to New Mexico in 1945.  In the U.S. Army, he worked with topographic maps.

text: His art career was interrupted when he entered into the United States Army in 1941. He did not paint again until he returned to New Mexico in 1945.  In the U.S. Army, he worked with topographic maps.

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answers: NDQ_001587

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answers: NDQ_001589

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answers: NDQ_001590

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: No

answers: NDQ_001605

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

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answers: NDQ_001624

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answers: 45

text: All elevations use the North American Vertical Datum of 1988 (NAVD88), the currently accepted vertical control datum for United States, Canada and Mexico. Elevations are from the National Geodetic Survey when available. Others are from the United States Geological Survey topographic maps when available. Elevations followed by a plus sign (+) were interpolated using topographic map contour lines. The true elevation is between that shown and the elevation plus forty feet since the relevant topographic maps all use 40-foot contours.

text: All elevations use the

text: North American Vertical Datum of 1988

text: (NAVD88), the currently accepted vertical control datum for United States, Canada and Mexico. Elevations are from the

text: National Geodetic Survey

text: when available. Others are from the

text: United States Geological Survey

text: topographic maps

text: when available. Elevations followed by a plus sign (+) were interpolated using topographic map

text: contour lines

text: . The true elevation is between that shown and the elevation plus forty feet since the relevant topographic maps all use 40-foot contours.

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answers: NDQ_001586

answers: true elevation is between that shown and the elevation plus forty feet

answers: NDQ_001587

answers: is between that shown and the elevation plus forty feet

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: use 40-foot contours

answers: NDQ_001590

answers: 40-foot

answers: NDQ_001591

answers: vertical control datum

answers: NDQ_001592

answers: use 40-foot contours

answers: NDQ_001593

answers: contour lines

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 40-foot

answers: NDQ_001597

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answers: NDQ_001598

answers: contour lines

answers: NDQ_001600

answers: contour lines

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: None

answers: NDQ_001606

answers: 40-foot

answers: NDQ_001608

answers: contour lines

answers: NDQ_001611

answers: contour lines

answers: NDQ_001613

answers: (NAVD88)

answers: NDQ_001614

answers: topographic map contour lines

answers: NDQ_001618

answers: true elevation

answers: NDQ_001619

answers: contour lines

answers: NDQ_001620

answers: The true elevation

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: true elevation

answers: NDQ_001623

answers: contour lines

answers: NDQ_001624

answers: 40-foot contours

answers: NDQ_001625

answers: 40-foot

text: Sacca Sessola loosely translated as "Scoop Bag" (also not correctly named as "Isola delle Rose" or "Island of Roses" by the hotel which is located in that area, for unnecessary marketing reasons: it is not a name recognized by the Venetians, and on topographical maps) is an island in the Venetian Lagoon, northern Italy.

text: Sacca Sessola loosely translated as "Scoop Bag" (also not correctly named as "Isola delle Rose" or "Island of Roses" by the hotel which is located in that area, for unnecessary marketing reasons: it is not a name recognized by the Venetians, and on topographical maps) is an island in the

text: Venetian Lagoon

text: , northern

text: Italy

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answers: NDQ_001624

answers: 4

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: topographical maps

answers: NDQ_001587

answers: is an island in the Venetian Lagoon

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: it is not a name recognized

answers: NDQ_001590

answers: Isola delle Rose

answers: NDQ_001591

answers: island

answers: NDQ_001592

answers: correctly named

answers: NDQ_001593

answers: topographical maps

answers: NDQ_001594

answers: Lagoon

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Venetian Lagoon

answers: NDQ_001598

answers: topographical maps

answers: NDQ_001600

answers: Lagoon

answers: NDQ_001603

answers: not correctly named

answers: NDQ_001605

answers: topographical maps

answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

answers: topographical

answers: NDQ_001611

answers: topographical maps

answers: NDQ_001613

answers: Island of Roses

answers: NDQ_001614

answers: topographical

answers: NDQ_001618

answers: topographical

answers: NDQ_001619

answers: Lagoon

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: topographical

answers: NDQ_001622

answers: island

answers: NDQ_001623

answers: Lagoon

answers: NDQ_001624

answers: Lagoon

answers: NDQ_001625

answers: 1 km

text: On maps produced by Swisstopo, the color of the contour lines is used to indicate the type of ground: black for bare rock and scree, blue for ice and underwater contours, brown for earth-covered ground.

text: On maps produced by

text: Swisstopo

text: , the color of the contour lines is used to indicate the type of ground: black for bare rock and

text: scree

text: , blue for ice and underwater contours, brown for earth-covered ground.

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answers: contour lines are used to indicate the type of ground

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answers: NDQ_001590

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answers: NDQ_001606

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answers: NDQ_001621

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text: We fix the interpolation nodes x, ..., x and an interval [a, b] containing all the interpolation nodes. The process of interpolation maps the function f to a polynomial p. This defines a mapping X from the space C([a, b]) of all continuous functions on [a, b] to itself. The map X is linear and it is a projection on the subspace  of polynomials of degree  or less.

text: We fix the interpolation nodes x, ..., x and an

text: interval

text: [a, b] containing all the interpolation nodes. The process of interpolation maps the function f to a polynomial p. This defines a mapping X from the space C([a, b]) of all continuous functions on [a, b] to itself. The map X is linear and it is a

text: projection

text: on the subspace  of polynomials of degree  or less.

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answers: NDQ_001588

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answers: NDQ_001589

answers: It is a projection on the subspace of polynomials of degree or less

answers: NDQ_001590

answers: [a, b]

answers: NDQ_001591

answers: interpolation nodes

answers: NDQ_001592

answers: fix the interpolation nodes

answers: NDQ_001593

answers: It is a projection on the subspace of polynomials

answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

answers: It is a projection on the subspace of polynomials of degree or less

answers: NDQ_001598

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answers: NDQ_001603

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answers: NDQ_001611

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001623

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answers: NDQ_001624

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answers: NDQ_001625

answers: [a, b]

text: The Survey has provided orthoimagery and digital topographic data derived from lidar through the PAMAP program. The Survey provides oil and gas well information through PA*IRIS. BTGS participates in federally funded StateMap program to produce 1:24000 geological maps.

text: The Survey has provided orthoimagery and digital topographic data derived from lidar through the PAMAP program. The Survey provides oil and gas well information through PA*IRIS. BTGS participates in federally funded StateMap program to produce 1:24000 geological maps.

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answers: It uses different colors to represent different rocks.

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text: The spatial data used in the new maps is Vicmap Topographic data, which includes Vicmap Digital Framework Datasets along with other key government datasets. Vicmap data is the authoritative spatial data for the State of Victoria and is the foundation of Victoria's primary mapping and geographic information systems. The features depicted in Vicmap Topographic maps include both natural features, such as watercourses, contours, cliffs and tree cover, and constructed features, such as drains, gates, roads and shipwrecks. The traditional 1:25,000 printed topographic maps have been used as a benchmark for the new Vicmap Topographic products. Hence the new series replicates the features and associated symbology as depicted on the old maps.

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answers: NDQ_001588

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answers: NDQ_001589

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answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: The traditional 1:25,000 printed topographic maps have been used as a benchmark

answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001611

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text: Aerial photography is used in cartography (particularly in photogrammetric surveys, which are often the basis for topographic maps), land-use planning, archaeology, movie production, environmental studies, power line inspection, surveillance, commercial advertising, conveyancing, and artistic projects. An example of how aerial photography is used in the field of archaeology is the mapping project done at the site Angkor Borei in Cambodia from 1995-1996. Using aerial photography, archaeologists were able to identify archaeological features, including 112 water features (reservoirs, artificially constructed pools and natural ponds) within the walled site of Angkor Borei. In the United States, aerial photographs are used in many Phase I Environmental Site Assessments for property analysis.

text: Aerial photography is used in

text: cartography

text: (particularly in

text: photogrammetric

text: surveys

text: , which are often the basis for

text: topographic maps

text: ), land-use planning,

text: archaeology

text: movie production

text: environmental

text: studies,

text: power line

text: inspection,

text: surveillance

text: , commercial advertising,

text: conveyancing

text: , and artistic projects. An example of how aerial photography is used in the field of archaeology is the mapping project done at the site Angkor Borei in Cambodia from 1995-1996. Using aerial photography, archaeologists were able to identify archaeological features, including 112 water features (reservoirs, artificially constructed pools and natural ponds) within the walled site of Angkor Borei. In the United States, aerial photographs are used in many

text: Phase I Environmental Site Assessment

text: s for property analysis.

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text: Lyddan Island is an ice-covered island located at the southwestern extremity of the Riiser-Larsen Ice Shelf, separating it from the Brunt Ice Shelf, about  off the Princess Martha Coast of Antarctica. It is about  long and has three narrow arms in the form of a trefoil. It was discovered and plotted by W.R. MacDonald on November 5, 1967, in the course of a U.S. Navy Squadron VXE-6 reconnaissance flight over the coast in LC-130 aircraft, and was named by the Advisory Committee on Antarctic Names for Robert H. Lyddan, Chief Topographic Engineer of the United States Geological Survey, who had been active in the planning and supervision of Antarctic mapping operations since the 1950s.

text: Lyddan Island is an ice-covered island located at the southwestern extremity of the

text: Riiser-Larsen Ice Shelf

text: , separating it from the

text: Brunt Ice Shelf

text: , about  off the

text: Princess Martha Coast

text: of Antarctica. It is about  long and has three narrow arms in the form of a trefoil. It was discovered and plotted by

text: W.R. MacDonald

text: on November 5, 1967, in the course of a U.S. Navy Squadron

text: reconnaissance flight over the coast in

text: aircraft, and was named by the

text: Advisory Committee on Antarctic Names

text: for

text: Robert H. Lyddan

text: , Chief Topographic Engineer of the

text: United States Geological Survey

text: , who had been active in the planning and supervision of Antarctic mapping operations since the 1950s.

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answers: NDQ_001587

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answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Antarctic mapping operations since the 1950s

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: three narrow arms

answers: NDQ_001592

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answers: NDQ_001593

answers: Antarctica

answers: NDQ_001594

answers: Topographic Engineer

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: southwestern extremity

answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

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answers: NDQ_001605

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answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

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answers: NDQ_001611

answers: Lyddan Island

answers: NDQ_001613

answers: The Advisory Committee on Antarctic Names

answers: NDQ_001614

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answers: NDQ_001618

answers: Brunt Ice Shelf

answers: NDQ_001619

answers: Topographic

answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

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answers: NDQ_001623

answers: trefoil

answers: NDQ_001624

answers: Riiser-Larsen Ice Shelf

answers: NDQ_001625

answers: about

text: The earliest geologic map of the modern era is the 1771 "Map of Part of Auvergne, or figures of, The Current of Lava in which Prisms, Balls, Etc. are Made from Basalt.  To be used with Mr. Demarest's theories of this hard basalt.  Engraved by Messr. Pasumot and Daily, Geological Engineers of the King."  This map is based on Nicolas Desmarest's 1768 detailed study of the geology and eruptive history of the Auvergne volcanoes and a comparison with the columns of the Giant's Causeway of Ireland.  He identified both landmarks as features of extinct volcanoes.  The 1798 report was incorporated in the 1771 (French) Royal Academy of Science compendium.

text: The earliest geologic map of the modern era is the 1771 "Map of Part of Auvergne, or figures of, The Current of Lava in which Prisms, Balls, Etc. are Made from Basalt.  To be used with Mr. Demarest's theories of this hard basalt.  Engraved by Messr. Pasumot and Daily, Geological Engineers of the King."  This map is based on

text: Nicolas Desmarest

text: 's 1768 detailed study of the geology and eruptive history of the

text: Auvergne

text: volcanoes and a comparison with the columns of the

text: Giant's Causeway

text: of Ireland.  He identified both landmarks as features of extinct volcanoes.  The 1798 report was incorporated in the 1771 (French) Royal Academy of Science compendium.

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answers: NDQ_001587

answers: the columns of the Giant's Causeway of Ireland

answers: NDQ_001588

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answers: NDQ_001589

answers: The Current of Lava in which Prisms, Balls, Etc. are Made from Basalt

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: Prisms

answers: NDQ_001592

answers: identify both landmarks as features of extinct volcanoes

answers: NDQ_001593

answers: topographic map

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: The Current of Lava

answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

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answers: NDQ_001605

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answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001611

answers: Prisms, Balls, Etc

answers: NDQ_001613

answers: the side of the circle with the higher elevation

answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

answers: The Current

answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001623

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answers: NDQ_001624

answers: Prisms

answers: NDQ_001625

answers: 1771

text: Existing topographic survey maps, because of their comprehensive and encyclopedic coverage, form the basis for much derived topographic work. Digital Elevation Models, for example, have often been created not from new remote sensing data but from existing paper topographic maps. Many government and private publishers use the artwork (especially the contour lines) from existing topographic map sheets as the basis for their own specialized or updated topographic maps.

text: Existing topographic survey maps, because of their comprehensive and encyclopedic coverage, form the basis for much derived topographic work. Digital Elevation Models, for example, have often been created not from new remote sensing data but from existing paper topographic maps. Many government and private publishers use the artwork (especially the contour lines) from existing topographic map sheets as the basis for their own specialized or updated topographic maps.

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text: Labels are a critical component of elevation maps. A properly labeled contour map helps the reader to quickly interpret the shape of the terrain. If numbers are placed close to each other, it means that the terrain is steep. Labels should be placed along a slightly curved line "pointing" to the summit or nadir, from several directions if possible, making the visual identification of the summit or nadir easy. Contour labels can be oriented so a reader is facing uphill when reading the label.

text: Labels

text: are a critical component of elevation maps. A properly labeled contour map helps the reader to quickly interpret the shape of the terrain. If numbers are placed close to each other, it means that the terrain is steep. Labels should be placed along a slightly curved line "pointing" to the summit or nadir, from several directions if possible, making the visual identification of the summit or nadir easy. Contour labels can be oriented so a reader is facing uphill when reading the label.

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text: These maps are much more detailed than general-purpose topographic maps, and incorporate a standard symbology that is designed to be useful to anyone, regardless of native language. In addition to indicating the topography of the terrain with contour lines, orienteering maps also show forest density, water features, clearings, trails and roads, earthen banks and rock walls, ditches, wells and pits, fences and power lines, buildings, boulders, and other features of the terrain. Orienteering maps are 1:15 000 or 1:10 000 scale.

text: These maps are much more detailed than general-purpose topographic maps, and incorporate a standard symbology that is designed to be useful to anyone, regardless of native language. In addition to indicating the

text: topography

text: of the terrain with contour lines, orienteering maps also show forest density, water features, clearings, trails and roads, earthen banks and rock walls, ditches, wells and pits, fences and power lines, buildings, boulders, and other features of the terrain. Orienteering maps are 1:15 000 or 1:10 000

text: scale

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answers: NDQ_001587

answers: contour lines

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: wells and pits

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: topography

answers: NDQ_001592

answers: native language

answers: NDQ_001593

answers: contour lines

answers: NDQ_001594

answers: water features

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: water features

answers: NDQ_001598

answers: contour lines

answers: NDQ_001600

answers: clearings

answers: NDQ_001603

answers: general-purpose

answers: NDQ_001605

answers: boulders

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: contour lines

answers: NDQ_001611

answers: contour lines

answers: NDQ_001613

answers: contour lines

answers: NDQ_001614

answers: contour lines

answers: NDQ_001618

answers: topography

answers: NDQ_001619

answers: wells

answers: NDQ_001620

answers: contour lines

answers: NDQ_001621

answers: contour lines

answers: NDQ_001622

answers: topography

answers: NDQ_001623

answers: contour lines

answers: NDQ_001624

answers: topography

answers: NDQ_001625

answers: 1:15 000

text: Topographic map of the former municipality of Bergambacht, 2013.

text: Topographic map of the former municipality of Bergambacht, 2013.

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answers: contour lines that are numbered represent changes in elevation

answers: NDQ_001587

answers: Bergambacht is a municipality in the Netherlands

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: Bathymetric maps do not have topographic features

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: Bergambacht

answers: NDQ_001592

answers: map of the former municipality

answers: NDQ_001593

answers: The former municipality of Bergambacht, 2013.

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: The direction that rivers and streams flow

answers: NDQ_001598

answers: The steepest side of the mountain

answers: NDQ_001600

answers: The former municipality of Bergambacht

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Bergambacht is a municipality in the Netherlands.

answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: contour lines help us to see the three-dimensional shape of the land

answers: NDQ_001611

answers: Concentric lines that are very close together show a low hill

answers: NDQ_001613

answers: the side with the higher elevation

answers: NDQ_001614

answers: Horizontal distances

answers: NDQ_001618

answers: Topographic map

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic map

answers: NDQ_001622

answers: Bergambacht

answers: NDQ_001623

answers: Topographic map

answers: NDQ_001624

answers: Bergambacht

answers: NDQ_001625

answers: 3 m

text: The map sheets have been produced in several different versions: topographic maps, tourist maps, special maps (for aerospace, geology, etc.). They are now also available on electronic media.  The topographic maps have been published in the following scale series:

text: The map sheets have been produced in several different versions: topographic maps, tourist maps, special maps (for aerospace, geology, etc.). They are now also available on electronic media.  The topographic maps have been published in the following

text: scale series

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answers: NDQ_001587

answers: The topographic maps have been published

answers: NDQ_001588

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answers: NDQ_001589

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answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001592

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answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: The scale series

answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001611

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

answers: scale series

answers: NDQ_001623

answers: scale

answers: NDQ_001624

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answers: NDQ_001625

answers: 1  100

text: Topographical disorientation, also known as topographical agnosia and topographagnosia, is the inability to orient oneself in one's surroundings as a result of focal brain damage. This disability may result from the inability to make use of selective spatial information (e.g., environmental landmarks) or to orient by means of specific cognitive strategies such as the ability to form a mental representation of the environment, also known as a cognitive map.  It may be part of a syndrome known as visuospatial dysgnosia.

text: Topographical disorientation, also known as topographical agnosia and topographagnosia, is the inability to orient oneself in one's surroundings as a result of

text: focal brain damage

text: . This disability may result from the inability to make use of selective spatial information (e.g., environmental landmarks) or to orient by means of specific cognitive strategies such as the ability to form a mental representation of the environment, also known as a

text: cognitive map

text: .  It may be part of a syndrome known as

text: visuospatial dysgnosia

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answers: Topographical disorientation

answers: NDQ_001587

answers: may be part of a syndrome known as visuospatial dysgnosia

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: mental representation of the environment

answers: NDQ_001590

answers: Topographical disorientation

answers: NDQ_001591

answers: Topographical disorientation

answers: NDQ_001592

answers: make use of selective spatial information

answers: NDQ_001593

answers: topographic map

answers: NDQ_001594

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: The ability to form a mental representation of the environment, also known as a cognitive map

answers: NDQ_001598

answers: This disability may result from the inability to make use of selective spatial information

answers: NDQ_001600

answers: Topographical disorientation

answers: NDQ_001603

answers: None of the above choices.

answers: NDQ_001605

answers: Topographical disorientation

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: Topographical disorientation

answers: NDQ_001611

answers: Topographical disorientation

answers: NDQ_001613

answers: Topographical disorientation

answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

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answers: NDQ_001621

answers: Topographical

answers: NDQ_001622

answers: environmental landmarks

answers: NDQ_001623

answers: cognitive map

answers: NDQ_001624

answers: environmental landmarks

answers: NDQ_001625

answers: 1 km

text: Dutch Topographic map of the island of Schouwen-Duiveland, as per Sept. 2014.

text: Dutch Topographic map of the island of Schouwen-Duiveland, as per Sept. 2014.

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

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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: tqa2:L_0039/T_0395/e1278a8201ddf520d5b19846047bf656

answers: 0

answers: NDQ_001586

answers: 4

answers: NDQ_001587

answers: 0

answers: NDQ_001588

answers: 4

answers: NDQ_001589

answers: 0

answers: NDQ_001590

answers: 0

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 4

answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 4

answers: NDQ_001598

answers: 0

answers: NDQ_001600

answers: 4

answers: NDQ_001603

answers: 0

answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 4

answers: NDQ_001608

answers: 4

answers: NDQ_001611

answers: 3

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 0

answers: NDQ_001618

answers: 0

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 5

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: contour lines that are numbered represent changes in elevation

answers: NDQ_001587

answers: Schouwen-Duiveland

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Schouwen-Duiveland, as per Sept. 2014

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: Schouwen

answers: NDQ_001592

answers: name the island

answers: NDQ_001593

answers: Schouwen-Duiveland

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Schouwen-Duiveland

answers: NDQ_001598

answers: The steepest side of the mountain

answers: NDQ_001600

answers: Plains or plateaus

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Different colors represent different types of rocks.

answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: Contour lines help us to see the three-dimensional shape

answers: NDQ_001611

answers: Concentric lines that are very far apart show a high, steep hill

answers: NDQ_001613

answers: The side of the circle with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Schouwen

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic map

answers: NDQ_001622

answers: island

answers: NDQ_001623

answers: isobath

answers: NDQ_001624

answers: Schouwen

answers: NDQ_001625

answers: 9 km

text: The distribution of pyroclastic ash depends largely on the direction of wind at intermediate and high altitudes between approximately 4.5 – 13 km. The general trend of pyroclastic dispersal is shown using isopachs (which are analogous to topographic map contours though they illustrate lines of equal thickness rather than elevation) and show the dispersal as elongated with wind direction.

text: The distribution of pyroclastic ash depends largely on the direction of

text: wind

text: at intermediate and high altitudes between approximately 4.5 – 13 km. The general trend of pyroclastic dispersal is shown using

text: isopachs

text: (which are analogous to

text: topographic map

text: contours though they illustrate lines of equal thickness rather than elevation) and show the dispersal as elongated with wind direction.

answers: tqa2:L_0039/T_0389/3eb574e104aa97e246137e9e5232abcf

answers: equal thickness

answers: tqa2:L_0039/T_0389/597e2ff69da54b6e4c2b673fbb036c95

answers: 0

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answers: equal thickness

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answers: 0

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answers: 0

answers: tqa2:L_0039/T_0395/6aad7f1f8d291b5761a8b73d39008410

answers: 0

answers: tqa2:L_0039/T_0395/e4440cb133c19079cf1de06142182459

answers: 0

answers: tqa2:L_0039/T_0395/a1ad3c980328bce73604a21928ff7929

answers: 4

answers: tqa2:L_0039/T_0395/b3ed9fe004e17c5d260376b7dc97546c

answers: 0

answers: tqa2:L_0039/T_0395/617bb1adf869087f60ef513ffed01cc1

answers: 4

answers: tqa2:L_0039/T_0395/3a25e8f10326f778d0e4ce880cf48373

answers: 0

answers: tqa2:L_0039/T_0395/6e7058ba6ae907b02aadde87cadc8f56

answers: 0

answers: tqa2:L_0039/T_0395/3442c8987c1161ceca69ab5226dd316e

answers: 0

answers: tqa2:L_0039/T_0395/4c9d21d7c8934e2cf4b88c65d430fc09

answers: 0

answers: tqa2:L_0039/T_0395/e1278a8201ddf520d5b19846047bf656

answers: 0

answers: NDQ_001586

answers: 4

answers: NDQ_001587

answers: 0

answers: NDQ_001588

answers: 4

answers: NDQ_001589

answers: 0

answers: NDQ_001590

answers: 4

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 0

answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 3

answers: NDQ_001597

answers: 4

answers: NDQ_001598

answers: 4

answers: NDQ_001600

answers: 4

answers: NDQ_001603

answers: 2

answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 4

answers: NDQ_001608

answers: 4

answers: NDQ_001611

answers: 0

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 3

answers: NDQ_001618

answers: 4

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 0

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 4

answers: NDQ_001624

answers: 4

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: lines of equal thickness

answers: NDQ_001587

answers: isopachs

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: elevation

answers: NDQ_001590

answers: isopaches

answers: NDQ_001591

answers: equal thickness

answers: NDQ_001592

answers: elevation

answers: NDQ_001593

answers: contours

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 4.5–13 km

answers: NDQ_001597

answers: wind direction

answers: NDQ_001598

answers: contours

answers: NDQ_001600

answers: isopachs

answers: NDQ_001603

answers: isopachs

answers: NDQ_001605

answers: isopachs

answers: NDQ_001606

answers: isopachs

answers: NDQ_001608

answers: isopachs

answers: NDQ_001611

answers: isopach

answers: NDQ_001613

answers: isopachs

answers: NDQ_001614

answers: elevation

answers: NDQ_001618

answers: elevation

answers: NDQ_001619

answers: contours

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: elevation

answers: NDQ_001623

answers: contours

answers: NDQ_001624

answers: elevation

answers: NDQ_001625

answers: 4.5 – 13 km

text: Topographic mapping should not be confused with geologic mapping. The latter is concerned with underlying structures and processes to the surface, rather than with identifiable surface features.

text: Topographic mapping should not be confused with

text: geologic map

text: ping. The latter is concerned with underlying structures and processes to the surface, rather than with identifiable surface features.

answers: tqa2:L_0039/T_0389/3eb574e104aa97e246137e9e5232abcf

answers: 0

answers: tqa2:L_0039/T_0389/597e2ff69da54b6e4c2b673fbb036c95

answers: 0

answers: tqa2:L_0039/T_0389/da52047f037a81ec1147b44727e238d3

answers: 0

answers: tqa2:L_0039/T_0389/bba68f60f9ae0cf6d7b951e050bb5340

answers: 3

answers: tqa2:L_0039/T_0389/e77a5165d73f9d04072d23950a162b86

answers: 0

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text: Hydrography, mostly for reasons of safety, adopted a number of conventions that have affected its portrayal of the data on nautical charts. For example, hydrographic charts are designed to portray what is safe for navigation, and therefore will usually tend to maintain least depths and occasionally de-emphasize the actual submarine topography that would be portrayed on bathymetric charts. The former are the mariner's tools to avoid accident. The latter are best representations of the actual seabed, as in a topographic map, for scientific and other purposes. Trends in hydrographic practice since c. 2003–2005 have led to a narrowing of this difference, with many more hydrographic offices maintaining "best observed" databases, and then making navigationally "safe" products as required.  This has been coupled with a preference for multi-use surveys, so that the same data collected for nautical charting purposes can also be used for bathymetric portrayal.

text: Hydrography, mostly for reasons of safety, adopted a number of conventions that have affected its portrayal of the data on nautical charts. For example, hydrographic charts are designed to portray what is safe for navigation, and therefore will usually tend to maintain least

text: depth

text: s and occasionally de-emphasize the actual submarine

text: topography

text: that would be portrayed on

text: bathymetric chart

text: s. The former are the

text: mariner

text: 's tools to avoid accident. The latter are best representations of the actual seabed, as in a topographic map, for scientific and other purposes. Trends in hydrographic practice since c. 2003–2005 have led to a narrowing of this difference, with many more

entity_name: List of Members of the International Hydrographic Organization

text: hydrographic offices

text: maintaining "best observed" databases, and then making navigationally "safe" products as required.  This has been coupled with a preference for multi-use surveys, so that the same data collected for nautical charting purposes can also be used for bathymetric portrayal.

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answers: will usually tend to maintain least depths

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: hydrographic charts are designed to portray what is safe for navigation

answers: NDQ_001590

answers: bathymetric

answers: NDQ_001591

answers: submarine topography

answers: NDQ_001592

answers: maintain least depths

answers: NDQ_001593

answers: topography

answers: NDQ_001594

answers: bathymetric charts

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Bathymetric charts

answers: NDQ_001598

answers: topography

answers: NDQ_001600

answers: topography

answers: NDQ_001603

answers: for scientific and other purposes

answers: NDQ_001605

answers: topographic maps

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topography

answers: NDQ_001611

answers: Bathymetric charts

answers: NDQ_001613

answers: Bathymetric charts

answers: NDQ_001614

answers: bathymetric charts

answers: NDQ_001618

answers: actual seabed

answers: NDQ_001619

answers: bathymetric

answers: NDQ_001620

answers: bathymetric

answers: NDQ_001621

answers: topographic map

answers: NDQ_001622

answers: actual seabed

answers: NDQ_001623

answers: bathymetric

answers: NDQ_001624

answers: submarine topography

answers: NDQ_001625

answers: bathymetric

text: Dutch Topographic map of Zaltbommel (municipality), Sept. 2014

text: Dutch Topographic map of Zaltbommel (municipality), Sept. 2014

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answers: 4

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answers: 0

answers: NDQ_001590

answers: 0

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 4

answers: NDQ_001594

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answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 4

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answers: NDQ_001600

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answers: 4

answers: NDQ_001608

answers: 4

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answers: 3

answers: NDQ_001613

answers: 0

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answers: 4

answers: NDQ_001618

answers: 0

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 5

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: Zaltbommel

answers: NDQ_001587

answers: Zaltbommel (municipality)

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Topographic map of Zaltbommel (municipality)

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: V shape

answers: NDQ_001592

answers: Zaltbommel

answers: NDQ_001593

answers: Zaltbommel (municipality)

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: The direction that rivers and streams flow

answers: NDQ_001598

answers: The steepest side

answers: NDQ_001600

answers: Zaltbommel (municipality)

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Different colors represent different types of rocks.

answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: contour lines help us to see the three-dimensional shape

answers: NDQ_001611

answers: Zaltbommel

answers: NDQ_001613

answers: the side with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Zaltbommel

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic map

answers: NDQ_001622

answers: Zaltbommel

answers: NDQ_001623

answers: isobath

answers: NDQ_001624

answers: Zaltbommel

answers: NDQ_001625

answers: 1 km

text: Dutch Topographic map of the municipality of Sittard-Geleen, 2013.

text: Dutch Topographic map of the municipality of Sittard-Geleen, 2013.

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answers: contour lines that are numbered

answers: NDQ_001587

answers: A cross section is a cross section of a map.

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: Bathymetric maps do not have contour lines.

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: a V shape

answers: NDQ_001592

answers: location of landmarks

answers: NDQ_001593

answers: The slope of the land can be determined using a topographic map.

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: It can be used to determine the direction that rivers and streams flow

answers: NDQ_001598

answers: The steepest side of the mountain

answers: NDQ_001600

answers: Plains or plateaus

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Different colors represent different types of rocks.

answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: Contour lines help us to see the three-dimensional shape

answers: NDQ_001611

answers: Concentric lines that are very close together show a low hill

answers: NDQ_001613

answers: On the side of the circle with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Topographic map

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: The difference in elevation

answers: NDQ_001621

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answers: NDQ_001622

answers: Topographic map

answers: NDQ_001623

answers: isosceles

answers: NDQ_001624

answers: V-shaped contour lines

answers: NDQ_001625

answers: 3 m

text: Once Williams came to Murray to make his proposal in 1923, Murray and his partner, Henry Flood, Jr., pored over topographic maps of the region and worked on estimates. It looked as if they might be able to generate enormous power at very low cost. It was said that here, as Murray looked over a topographic map of the Saluda River Valley, his eyes glanced at the  contour line. He followed the line as it meandered through the valley and noticed that the contour did not touch a railroad, and its highest elevation was never less than 40 feet (12 m) below the divide separating the Saluda Valley from the neighboring Broad River Valley. After winding around the valley of the Saluda for nearly 300 miles (500 km), about 10 miles (15 km) west of Columbia its position the north side of the valley approached within 8,000 feet (2.4 km) of its position on the south side. Murray realized that a dam across such an expanse would be ideal for power development. He visited South Carolina to investigate.

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answers: NDQ_001588

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answers: NDQ_001590

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answers: NDQ_001592

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answers: Pored over topographic maps of the region and worked on estimates

answers: NDQ_001605

answers: topographic maps

answers: NDQ_001606

answers: the contour did not touch a railroad

answers: NDQ_001608

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answers: Saluda Valley

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answers: Saluda River Valley

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answers: 40 feet

text: Dutch topographic map of Veldhoven (town), Dec. 2013

text: Dutch topographic map of Veldhoven (town), Dec. 2013

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answers: Veldhoven (town), Dec. 2013

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answers: Concentric lines that are very close together show a valley

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text: Although virtually the entire terrestrial surface of Earth has been mapped at scale 1:1,000,000, medium and large-scale mapping has been accomplished intensively in some countries and much less in others. Nevertheless, national mapping programs listed below are only a partial selection. Several commercial vendors supply international topographic map series.

text: Although virtually the entire terrestrial surface of Earth has been mapped at scale 1:1,000,000, medium and large-scale mapping has been accomplished intensively in some countries and much less in others. Nevertheless, national mapping programs listed below are only a partial selection. Several commercial vendors supply international topographic map series.

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answers: NDQ_001605

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text: For neurons, it is metabolically costly to make long connections, and the trade-off of connection distance is time.  Thus, it is good design to group neurons together that are to be highly interconnected.  Multiple topographic maps is a feature that is advantageous because it allows maps of different sizes that would accommodate varying levels of acuity and details in signals.  A more detailed map has more neurons that would take up more area than a more global map, which would require fewer connections.

text: For

text: neurons

text: , it is metabolically costly to make long connections, and the trade-off of connection distance is time.  Thus, it is good design to group neurons together that are to be highly interconnected.  Multiple topographic maps is a feature that is advantageous because it allows maps of different sizes that would accommodate varying levels of acuity and details in signals.  A more detailed map has more neurons that would take up more area than a more global map, which would require fewer connections.

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answers: NDQ_001587

answers: A more detailed map has more neurons that would take up more area

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: it is metabolically costly to make long connections

answers: NDQ_001590

answers: Connection distance

answers: NDQ_001591

answers: neurons that are to be highly interconnected

answers: NDQ_001592

answers: make long connections

answers: NDQ_001593

answers: topographic maps

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001598

answers: The trade-off of connection distance is time

answers: NDQ_001600

answers: global map

answers: NDQ_001603

answers: no

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answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

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answers: NDQ_001611

answers: Connection distance is time

answers: NDQ_001613

answers: A more detailed map has more neurons that would take up more area

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: global map

answers: NDQ_001619

answers: topographic

answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001623

answers: connections

answers: NDQ_001624

answers: global map

answers: NDQ_001625

answers: global map

text: Mr. Gerald Fitzgerald, Chief of the Topographic Branch of the US Geological Survey, said, "Do you have a copy of USGS Bulletin 657? that your father wrote? You must obtain a copy! That bulletin laid the groundwork for the entire field of photogrammetric surveying and map-making!"

text: Mr. Gerald Fitzgerald, Chief of the Topographic Branch of the US Geological Survey, said, "Do you have a copy of USGS Bulletin 657? that your father wrote? You must obtain a copy! That bulletin laid the groundwork for the entire field of photogrammetric surveying and map-making!"

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answers: Topographic

answers: NDQ_001587

answers: photogrammetric surveying

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answers: intersect

answers: NDQ_001589

answers: photogrammetric

answers: NDQ_001590

answers: Topographic

answers: NDQ_001591

answers: Topographic

answers: NDQ_001592

answers: lay the groundwork

answers: NDQ_001593

answers: Topographic

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: USGS Bulletin

answers: NDQ_001598

answers: Topographic

answers: NDQ_001600

answers: Topographic

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answers: It's impossible to say

answers: NDQ_001605

answers: Topographic

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: Topographic

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answers: Topographic

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answers: Topographic

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answers: Topographic

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answers: Topographic

answers: NDQ_001623

answers: Topographic

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answers: Topographic

answers: NDQ_001625

answers: photogrammetric

text: 12 individual islets are named on detailed topographical maps:

text: 12 individual islets are named on detailed topographical maps:

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

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

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answers: NDQ_001587

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answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: 12 individual islets are named

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: islets

answers: NDQ_001592

answers: name individual islets

answers: NDQ_001593

answers: The slope of the land

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: The direction that rivers and streams flow

answers: NDQ_001598

answers: side of the mountain is steepest

answers: NDQ_001600

answers: islets

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Colors are used to represent rocks.

answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

answers: topographical maps

answers: NDQ_001611

answers: islets are named on detailed topographical maps

answers: NDQ_001613

answers: on the side of the circle with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: islets

answers: NDQ_001619

answers: topographical

answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

answers: islets

answers: NDQ_001623

answers: islets

answers: NDQ_001624

answers: islets

answers: NDQ_001625

answers: 12

text: However, in the vernacular and day to day world, the representation of relief (contours) is popularly held to define the genre, such that even small-scale maps showing relief are commonly (and erroneously, in the technical sense) called "topographic".

text: However, in the vernacular and day to day world, the representation of relief (contours) is popularly held to define the genre, such that even small-scale maps showing relief are commonly (and erroneously, in the technical sense) called "topographic".

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answers: NDQ_001586

answers: relief

answers: NDQ_001587

answers: Contours

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: "topographic"

answers: NDQ_001590

answers: relief

answers: NDQ_001591

answers: relief

answers: NDQ_001592

answers: representation of relief

answers: NDQ_001593

answers: relief

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Contours

answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: unanswerable

answers: NDQ_001605

answers: Contours

answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001611

answers: relief

answers: NDQ_001613

answers: relief

answers: NDQ_001614

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answers: NDQ_001618

answers: relief

answers: NDQ_001619

answers: Contours

answers: NDQ_001620

answers: relief

answers: NDQ_001621

answers: relief

answers: NDQ_001622

answers: relief

answers: NDQ_001623

answers: contours

answers: NDQ_001624

answers: relief

answers: NDQ_001625

answers: small-scale

text: Relevant topographic maps for the track are available from the NSW Department of Lands, maps Katoomba (8930-1S), Hampton (8930-4S) and Jenolan (8930-3N) cover the entirety of the track.  Or Download and print the full map set on the PDF from wildwalks

text: Relevant

text: topographic maps

text: for the track are available from the NSW Department of Lands, maps Katoomba (8930-1S), Hampton (8930-4S) and Jenolan (8930-3N) cover the entirety of the track.  Or Download and print the full map set on the PDF from wildwalks

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text: Mexican topographic maps and United States Geological Survey (USGS) maps of the region disagree on the name of an adjacent range lying to the southeast of the Tinajas Altas Mountains. In the United States this small range is referred to as the Sierra de la Lechuguilla, but in Mexico they are called the Sierra Tinajas Altas which would suggest that they are a longer extension of the Tinajas Altas Mountains into Mexico. The two ranges, however, share no surface connection so they are not the same. The Sierra de la Lechuguilla/Sierra Tinajas Altas range are instead on a parallel alignment to the southeast of the Tinajas Altas Mountains proper.

text: Mexican topographic maps and

text: United States Geological Survey

text: (USGS) maps of the region disagree on the name of an adjacent range lying to the southeast of the Tinajas Altas Mountains. In the United States this small range is referred to as the

text: Sierra de la Lechuguilla

text: , but in Mexico they are called the Sierra Tinajas Altas which would suggest that they are a longer extension of the Tinajas Altas Mountains into Mexico. The two ranges, however, share no surface connection so they are not the same. The Sierra de la Lechuguilla/Sierra Tinajas Altas range are instead on a parallel alignment to the southeast of the Tinajas Altas Mountains proper.

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answers: The two ranges, however, share no surface connection so they are not the same

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: USGS maps of the region disagree on the name of an adjacent range

answers: NDQ_001590

answers: (USGS)

answers: NDQ_001591

answers: longer extension

answers: NDQ_001592

answers: name of an adjacent range

answers: NDQ_001593

answers: topographic maps

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: to the southeast

answers: NDQ_001598

answers: The two ranges, however, share no surface connection

answers: NDQ_001600

answers: parallel alignment

answers: NDQ_001603

answers: USGS

answers: NDQ_001605

answers: Sierra de la Lechuguilla

answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

answers: topographic maps

answers: NDQ_001611

answers: Tinajas Altas Mountains

answers: NDQ_001613

answers: The two ranges, however, share no surface connection so they are not the same

answers: NDQ_001614

answers: parallel alignment

answers: NDQ_001618

answers: mountains

answers: NDQ_001619

answers: depth map

answers: NDQ_001620

answers: parallel alignment

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: The two ranges

answers: NDQ_001623

answers: parallel alignment

answers: NDQ_001624

answers: USGS

answers: NDQ_001625

answers: parallel alignment

text: In the 1670s, Cassini began work on a project to create a topographic map of France, using Gemma Frisius's technique of triangulation. The project was continued by his son Jacques Cassini and eventually finished by his grandson César-François Cassini de Thury and published as the Carte de Cassini in 1789 or 1793. It was the first topographic map of an entire country.

text: In the 1670s, Cassini began work on a project to create a

text: topographic

text: map of France, using

text: Gemma Frisius

text: 's technique of

text: triangulation

text: . The project was continued by his son

text: Jacques Cassini

text: and eventually finished by his grandson

text: César-François Cassini de Thury

text: and published as the Carte de Cassini in 1789 or 1793. It was the

text: first topographic map of an entire country

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text: In 1933 during the Sixteenth International Geological Congress, an excursion took attendees into the Grand Canyon.  The geologists afterwards signed their names to a panoramic view of the canyon and sent it to Matthes with the message "We have been using your maps and have marveled at them.  There are no other such topographic maps in all the world."

text: In 1933 during the Sixteenth

entity_name: International Union of Geological Sciences

text: International Geological Congress

text: , an excursion took attendees into the Grand Canyon.  The geologists afterwards signed their names to a

text: panoramic view

text: of the canyon and sent it to Matthes with the message "We have been using your maps and have marveled at them.  There are no other such topographic maps in all the world."

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answers: NDQ_001591

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answers: NDQ_001592

answers: panoramic view of the canyon

answers: NDQ_001593

answers: topographic maps

answers: NDQ_001594

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001603

answers: They are useful only to geologists

answers: NDQ_001605

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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text: Vicmap Topographic Map Series is a series of topographic maps covering the State of Victoria, Australia. Created and maintained by the State of Victoria, the map series is currently in a transition phase, with traditional Vicmap Topographic maps being gradually replaced with a new map series.

text: Vicmap Topographic Map Series is a

text: series of topographic maps

text: covering the State of

text: Victoria, Australia

text: . Created and maintained by the State of Victoria, the

text: map series

text: is currently in a transition phase, with traditional Vicmap Topographic maps being gradually replaced with a new map series.

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answers: NDQ_001597

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answers: NDQ_001624

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answers: 1 km

text: The words isoline and isarithm (ἀριθμός arithmos "number") are general terms covering all types of contour line.  The word isogram (γράμμα gramma "writing or drawing") was proposed by Francis Galton in 1889 as a convenient generic designation for lines indicating equality of some physical condition or quantity; but it commonly refers to a word without a repeated letter.

text: The words isoline and isarithm (ἀριθμός arithmos "number") are general terms covering all types of contour line.  The word isogram (γράμμα gramma "writing or drawing") was proposed by

text: Francis Galton

text: in 1889 as a convenient generic designation for lines indicating equality of some physical condition or quantity; but it commonly refers to a

text: word without a repeated letter

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text: The first "decent" map of California and Oregon were drawn by Captain John C. Frémont of the U.S. Army's Corps of Topographical Engineers, and his topographers and cartographers in about 1848. Fremont and his men, led by his guide and former trapper Kit Carson, made extensive expeditions starting in 1844 over parts of California and Oregon including the important Humboldt River and Old Spanish Trail routes. They made numerous topographical measurements of longitude, latitude and elevation as well as cartographic sketches of the observable surroundings. His map, although in error in minor ways, was the best map available in 1848.  John C. Frémont gave the Great Salt Lake, Humboldt River, Pyramid Lake, Carson River, Walker River, Old Spanish Trail etc. their current names. The Truckee River (called the Salmon-Trout River by Fremont) in California and Nevada was mapped. Lake Tahoe is shown but left unnamed. The major rivers in California are shown, presumably given the names used by the trappers and Mexican and foreign settlers there. The Humboldt was named (after the great explorer Alexander von Humboldt). Fremont and his topographers/cartographers did not have time (it would take literally decades of work to do this) to make extensive explorations of the entire Sierra Nevada range or Great Basin. Details of the Sierra Nevada and Great Basin concerning the best passes or possible emigrant routes for wagons would be explored and discovered from about 1846 to 1859 by numerous other explorers.

text: The first "decent" map of California and Oregon were drawn by Captain

text: John C. Frémont

text: of the

text: U.S. Army's Corps of Topographical Engineers

text: , and his

text: topographer

text: s and

text: cartographers

text: in about 1848. Fremont and his men, led by his guide and former trapper

text: Kit Carson

text: , made extensive expeditions starting in 1844 over parts of California and Oregon including the important

text: Humboldt River

text: and

text: Old Spanish Trail

text: routes. They made numerous topographical measurements of longitude, latitude and elevation as well as cartographic sketches of the observable surroundings. His map, although in error in minor ways, was the best map available in 1848.  John C. Frémont gave the

text: Great Salt Lake

text: Humboldt River

text: Pyramid Lake

text: Carson River

text: Walker River

text: Old Spanish Trail

text: etc. their current names. The

text: Truckee River

text: (called the Salmon-Trout River by Fremont) in California and Nevada was mapped.

text: Lake Tahoe

text: is shown but left unnamed. The major rivers in California are shown, presumably given the names used by the trappers and Mexican and foreign settlers there. The Humboldt was named (after the great explorer

text: Alexander von Humboldt

text: ). Fremont and his topographers/cartographers did not have time (it would take literally decades of work to do this) to make extensive explorations of the entire Sierra Nevada range or

text: Great Basin

text: . Details of the Sierra Nevada and Great Basin concerning the best passes or possible emigrant routes for wagons would be explored and discovered from about 1846 to 1859 by numerous other explorers.

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answers: Lake Tahoe is shown but left unnamed

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answers: make extensive explorations of the entire Sierra Nevada range

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answers: They made numerous topographical measurements

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text: The National Land Survey of Finland produces the Topographic Database (accuracy 1:5000-1:10 000) and publishes topographic maps of Finland at 1:25,000 and 1:50,000. In addition topographics maps can be viewed by using a free map service MapSite.

text: The National Land Survey of Finland produces the Topographic Database (accuracy 1:5000-1:10 000) and publishes topographic maps of

text: Finland

text: at 1:25,000 and 1:50,000. In addition topographics maps can be viewed by using a free map service MapSite.

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text: Microsoft Research Maps or MSR Maps was a free online repository of public domain aerial imagery and topographic maps provided by the U.S. Geological Survey (USGS). The site is a collaboration between Microsoft Research (MSR), Bing Maps, and the USGS. It has been in operation since June 1998. It had 30,000 to 50,000 visitors per day as of January 2010. The site was renamed in 2010, prior to which it had been known as TerraServer-USA (formerly Microsoft TerraServer).

text: Microsoft Research Maps or MSR Maps was a free online repository of

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text: , and the USGS. It has been in operation since June 1998. It had 30,000 to 50,000 visitors per day as of January 2010. The site was renamed in 2010, prior to which it had been known as TerraServer-USA (formerly Microsoft TerraServer).

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text: The Map & GIS Library is located in Room 202 of the Sterling C. Evans Library. The collection consists of over 250,000 individual sheet maps, 3,000 atlases and gazetteers, and 1000 CD/DVDs, including worldwide coverage of topographic and geological maps, GIS datasets. The collection also includes travel maps and guides. The Library offer GIS assistance for those seeking data and support. They also provide assistance to all colleges and agencies associated with Texas A&M, as well as members of the local community.

text: The Map & GIS Library is located in Room 202 of the Sterling C. Evans Library. The collection consists of over 250,000 individual sheet maps, 3,000 atlases and gazetteers, and 1000 CD/DVDs, including worldwide coverage of topographic and geological maps, GIS datasets. The collection also includes travel maps and guides. The Library offer GIS assistance for those seeking data and support. They also provide assistance to all colleges and agencies associated with Texas A&M, as well as members of the local community.

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text: While not officially "topographic" maps, the national surveys of other nations share many of the same features, and so they are often called "topographic maps."

text: While not officially "topographic" maps, the national surveys of other nations share many of the same features, and so they are often called "topographic maps."

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text: Topographic maps are also commonly called contour maps or topo maps. In the United States, where the primary national series is organized by a strict 7.5-minute grid, they are often called topo quads or quadrangles.

text: Topographic maps are also commonly called contour maps or topo maps. In the United States, where the primary national series is organized by a strict 7.5-minute grid, they are often called topo quads or quadrangles.

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answers: NDQ_001624

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answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: Topographic maps

answers: NDQ_001587

answers: quadrangles

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: topo quads or quadrangles

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: quadrangles

answers: NDQ_001592

answers: 7.5-minute grid

answers: NDQ_001593

answers: contour maps

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

answers: 7.5

answers: NDQ_001597

answers: 7.5-minute grid

answers: NDQ_001598

answers: contour maps

answers: NDQ_001600

answers: quadrangles

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Topographic

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: Topographic maps

answers: NDQ_001611

answers: quadrangles

answers: NDQ_001613

answers: quadrangles

answers: NDQ_001614

answers: Topographic maps

answers: NDQ_001618

answers: quadrangles

answers: NDQ_001619

answers: contour

answers: NDQ_001620

answers: contour lines

answers: NDQ_001621

answers: Topographic

answers: NDQ_001622

answers: quadrangles

answers: NDQ_001623

answers: contour

answers: NDQ_001624

answers: quadrangles

answers: NDQ_001625

answers: 7.5

text: The NDL has a collection of approximately 440,000 maps of Japan and other countries, including the topographical, geological, and hydrological maps and charts dating back to the early Meiji Period (1868–1912) and topographical maps of foreign countries.

text: The NDL has a collection of approximately 440,000 maps of Japan and other countries, including the topographical, geological, and hydrological maps and charts dating back to the early

text: Meiji Period

text: (1868–1912) and topographical maps of foreign countries.

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answers: NDQ_001586

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answers: NDQ_001587

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answers: NDQ_001589

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answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001600

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answers: NDQ_001605

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answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

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answers: NDQ_001623

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answers: NDQ_001624

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answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: topographical

answers: NDQ_001587

answers: topographical

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: topographical

answers: NDQ_001590

answers: topographical

answers: NDQ_001591

answers: hydrological

answers: NDQ_001592

answers: geological

answers: NDQ_001593

answers: topographical

answers: NDQ_001594

answers: hydrological

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: hydrological

answers: NDQ_001598

answers: topographical

answers: NDQ_001600

answers: topographical

answers: NDQ_001603

answers: geological

answers: NDQ_001605

answers: geological

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographical

answers: NDQ_001611

answers: topographical

answers: NDQ_001613

answers: topographical

answers: NDQ_001614

answers: topographical

answers: NDQ_001618

answers: topographic

answers: NDQ_001619

answers: hydrological

answers: NDQ_001620

answers: topographical

answers: NDQ_001621

answers: topographical

answers: NDQ_001622

answers: hydrological

answers: NDQ_001623

answers: topographical

answers: NDQ_001624

answers: hydrological

answers: NDQ_001625

answers: approximately 440,000

text: The National Map is the official replacement for the USGS topographic map program.

text: The National Map is the official replacement for the

text: USGS topographic map program

answers: tqa2:L_0039/T_0389/3eb574e104aa97e246137e9e5232abcf

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answers: USGS

text: Even though, in places, hydrographic survey data may be collected in sufficient detail to portray bottom topography in some areas, hydrographic charts only show depth information relevant for safe navigation and should not be considered as a product that accurately portrays the actual shape of the bottom.  The soundings selected from the raw source depth data for placement on the nautical chart are selected for safe navigation and are biased to show predominately the shallowest depths that relate to safe navigation. For instance, if there is a deep area that can not be reached because it is surrounded by shallow water, the deep area may not be shown. The color filled areas that show different ranges of shallow water are not the equivalent of contours on a topographic map since they are often drawn seaward of the actual shallowest depth portrayed. A bathymetric chart does show marine topology accurately. Details covering the above limitations can be found in Part 1 of Bowditch's American Practical Navigator. Another concept that affects safe navigation is the sparsity of detailed depth data from high resolution sonar systems.  In more remote areas, the only available depth information has been collected with lead lines. This collection method drops a weighted line to the bottom at intervals and records the depth, often from a rowboat or sail boat. There is no data between soundings or between sounding lines to guarantee that there is not a hazard such as a wreck or a coral head waiting there to ruin a sailor's day. Often, the navigation of the collecting boat does not match today's GPS navigational accuracies. The hydrographic chart will use the best data available and will caveat its nature in a caution note or in the legend of the chart.

text: Even though, in places, hydrographic survey data may be collected in sufficient detail to portray bottom topography in some areas,

text: hydrographic chart

text: Bowditch's American Practical Navigator

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answers: contour lines that are numbered

answers: NDQ_001587

answers: A bathymetric chart

answers: NDQ_001588

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answers: NDQ_001589

answers: accurately portrays the actual shape of the bottom

answers: NDQ_001590

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answers: NDQ_001591

answers: the actual shallowest depth

answers: NDQ_001592

answers: depict the actual shape of the bottom

answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: They are often drawn seaward of the actual shallowest depth portrayed

answers: NDQ_001598

answers: contours

answers: NDQ_001600

answers: contour lines that are so close together that they almost touch

answers: NDQ_001603

answers: not the equivalent of contours

answers: NDQ_001605

answers: color filled areas that show different ranges of shallow water

answers: NDQ_001606

answers: The contour interval

answers: NDQ_001608

answers: topographic map

answers: NDQ_001611

answers: hydrographic charts only show depth information relevant for safe navigation

answers: NDQ_001613

answers: contours on a topographic map

answers: NDQ_001614

answers: contours

answers: NDQ_001618

answers: bottom

answers: NDQ_001619

answers: hydrographic charts

answers: NDQ_001620

answers: contours

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: bottom

answers: NDQ_001623

answers: contours

answers: NDQ_001624

answers: shallowest depth

answers: NDQ_001625

answers: seaward

text: As of 1974, according to the Geographical Survey Institute, Kunrei-shiki was used for topographical maps while Modified Hepburn was used for geological maps and aeronautical charts.

text: As of 1974, according to the

entity_name: Geospatial Information Authority of Japan

text: Geographical Survey Institute

text: , Kunrei-shiki was used for topographical maps while Modified Hepburn was used for geological maps and aeronautical charts.

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answers: 4

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answers: 0

answers: NDQ_001588

answers: 4

answers: NDQ_001589

answers: 0

answers: NDQ_001590

answers: 4

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 4

answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 4

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answers: 4

answers: NDQ_001600

answers: 0

answers: NDQ_001603

answers: 0

answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 4

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answers: 0

answers: NDQ_001613

answers: 0

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answers: 4

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answers: 0

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answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 4

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: topographical

answers: NDQ_001587

answers: Kunrei-shiki

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: aeronautical charts

answers: NDQ_001590

answers: topographical maps

answers: NDQ_001591

answers: topographical

answers: NDQ_001592

answers: aeronautical charts

answers: NDQ_001593

answers: topographical

answers: NDQ_001594

answers: Bathymetric

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: topographical

answers: NDQ_001598

answers: topographical

answers: NDQ_001600

answers: topographical

answers: NDQ_001603

answers: unanswerable

answers: NDQ_001605

answers: Modified Hepburn

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographical

answers: NDQ_001611

answers: Modified Hepburn

answers: NDQ_001613

answers: Modified Hepburn

answers: NDQ_001614

answers: topographical maps

answers: NDQ_001618

answers: topographical

answers: NDQ_001619

answers: nautical charts

answers: NDQ_001620

answers: topographical

answers: NDQ_001621

answers: topographical

answers: NDQ_001622

answers: Kunrei

answers: NDQ_001623

answers: Hepburn

answers: NDQ_001624

answers: Modified Hepburn

answers: NDQ_001625

answers: Kunrei

text: The characteristics of AV maps are their large scale (usually 1:25,000), high accuracy and great wealth of terrain detail in the high mountains (rock, rubble, glaciers, etc.). The contour interval is a maximum of 20 metres. The mountaineer should therefore be able to orient himself well using Alpine Club maps, both on the marked trails or in open terrain, i.e. away from the marked routes. In addition, the map sheets are divided in a way suitable for climbers and hikers with overlapping map sheets and a focus on the high mountain regions. Map names and height information (spot heights) are more densely printed than in other comparable maps.

text: The characteristics of AV maps are their large scale (usually 1:25,000), high accuracy and great wealth of terrain detail in the high mountains (rock, rubble, glaciers, etc.). The

text: contour interval

text: is a maximum of 20 metres. The

text: mountaineer

text: should therefore be able to orient himself well using Alpine Club maps, both on the marked trails or in open terrain, i.e. away from the marked routes. In addition, the map sheets are divided in a way suitable for climbers and hikers with overlapping map sheets and a focus on the high mountain regions. Map names and height information (spot heights) are more densely printed than in other comparable maps.

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text: Most commonly contour lines are drawn in plan view, or as an observer in space would view the Earth's surface: ordinary map form. However, some parameters can often be displayed in profile view showing a vertical profile of the parameter mapped. Some of the most common parameters mapped in profile are air pollutant concentrations and sound levels.  In each of those cases it may be important to analyze (air pollutant concentrations or sound levels) at varying heights so as to determine the air quality or noise health effects on people at different elevations, for example, living on different floor levels of an urban apartment.  In actuality, both plan and profile view contour maps are used in air pollution and noise pollution studies.

text: Most commonly contour lines are drawn in plan view, or as an observer in space would view the Earth's surface: ordinary map form. However, some parameters can often be displayed in profile view showing a vertical profile of the parameter mapped. Some of the most common parameters mapped in profile are

text: air pollutant concentrations

text: and

text: sound level

text: s.  In each of those cases it may be important to analyze (air pollutant concentrations or sound levels) at varying heights so as to determine the air quality or

text: noise health effects

text: on people at different elevations, for example, living on different floor levels of an urban apartment.  In actuality, both plan and profile view contour maps are used in

text: air pollution

text: and

text: noise pollution

text: studies.

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answers: NDQ_001590

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answers: NDQ_001591

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answers: NDQ_001592

answers: live on different floor levels

answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: Both plan and profile view contour maps are used in air pollution and noise pollution studies

answers: NDQ_001605

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answers: NDQ_001606

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answers: NDQ_001608

answers: Plan view

answers: NDQ_001611

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001618

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answers: NDQ_001619

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answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

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text: The game's terrain texture maps were made with satellite images rendered at four square meters per pixel, the highest resolution used in a flight simulator at that time. Artist Karen Wolff designed the terrain by combining large topographic maps into a "mosaic", which recreated the elevations and depressions of the Seattle area. The satellite imagery was layered over the resultant polygonal mesh. Real elevation data was also used for the eight lower-resolution Western American states outside of the Seattle area. Budget concerns and the storage limitations of the CD-ROM format prevented the team from rendering the entire United States, despite fan demand. The 3D objects that move across the terrain were created by Yoosun Cho, who used numerous photography books for inspiration. Flight Unlimited IIIs object editor let her set these objects to "move once along the path, back and forth or cycle". The weather system, co-designed by James, generates, moves and disperses weather fronts based on real-time calculations of atmospheric conditions such as humidity and orographic lift.

text: The game's terrain

text: texture maps

text: were made with

text: satellite images

text: rendered at four

text: square meters per pixel

text: , the highest resolution used in a flight simulator at that time. Artist Karen Wolff designed the terrain by combining large

text: topographic map

text: s into a "mosaic", which recreated the elevations and depressions of the Seattle area. The satellite imagery was layered over the resultant polygonal mesh. Real elevation data was also used for the eight lower-resolution Western American states outside of the Seattle area. Budget concerns and the

text: storage

text: limitations of the

text: CD-ROM

text: format prevented the team from rendering the entire United States, despite fan demand. The 3D objects that move across the terrain were created by Yoosun Cho, who used numerous photography books for inspiration. Flight Unlimited IIIs object editor let her set these objects to "move once along the path, back and forth or cycle". The weather system, co-designed by James, generates, moves and disperses

text: weather front

text: s based on real-time calculations of atmospheric conditions such as

text: humidity

text: and

text: orographic lift

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text: Line type refers to whether the basic contour line is solid, dashed, dotted or broken in some other pattern to create the desired effect.  Dotted or dashed lines are often used when the underlying base map conveys very important (or difficult to read) information.  Broken line types are used when the location of the contour line is inferred.

text: Line type refers to whether the basic contour line is solid, dashed, dotted or broken in some other pattern to create the desired effect.  Dotted or dashed lines are often used when the underlying base map conveys very important (or difficult to read) information.  Broken line types are used when the location of the contour line is inferred.

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text: Brief history: A need for a geological map of France goes back in time to a decree promulgated by Napoleon III, dated the First of October 1868, which established the "Service de la carte géologique de la France et des topographies souterraines" (English: The geologic map of France and groundwater topography service). The earliest geologic maps date back to 1664 (by ) and 1746 (by Jean-Étienne Guettard). Since 1794, the Corps des mines have been responsible for drawing up geological maps. Jean Baptiste Julien d'Omalius d'Halloy sketched the geology of the Parisian basin and it environs in 1816, scaling the map at 1/800 000. Ours-Pierre-Armand Petit-Dufrénoy and Jean-Baptiste Élie de Beaumont, who were both mining engineers, were charged with the task of drawing up the first French geological map in 1841, using a scale of  1 / 500 000.

text: Brief history: A need for a geological map of France goes back in time to a decree promulgated by

text: Napoleon III

text: , dated the First of October 1868, which established the "Service de la carte géologique de la France et des topographies souterraines" (English: The geologic map of France and groundwater topography service). The earliest geologic maps date back to 1664 (by ) and 1746 (by

text: Jean-Étienne Guettard

text: ). Since 1794, the

text: Corps des mines

text: have been responsible for drawing up geological maps.

text: Jean Baptiste Julien d'Omalius d'Halloy

text: sketched the geology of the Parisian basin and it environs in 1816, scaling the map at 1/800 000.

text: Ours-Pierre-Armand Petit-Dufrénoy

text: and

text: Jean-Baptiste Élie de Beaumont

text: , who were both mining engineers, were charged with the task of drawing up the first French geological map in 1841, using a scale of  1 / 500 000.

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text: There were several U.S. government-sponsored explorers who explored part of the Oregon Trail and wrote extensively about their explorations. Captain Benjamin Bonneville on his expedition of 1832 to 1834 explored much of the Oregon trail and brought wagons up the Platte, North Platte, Sweetwater route across South Pass to the Green River in Wyoming. He explored most of Idaho and the Oregon Trail to the Columbia. The account of his explorations in the west was published by Washington Irving in 1838.). John C. Frémont of the U.S. Army's Corps of Topographical Engineers and his guide Kit Carson led three expeditions from 1842 to 1846 over parts of California and Oregon. His explorations were written up by him and his wife Jessie Benton Frémont and were widely published. The first "decent" map of California and Oregon were drawn by Frémont and his topographers and cartographers in about 1848.

text: There were several U.S. government-sponsored explorers who explored part of the Oregon Trail and wrote extensively about their explorations. Captain

text: Benjamin Bonneville

text: on his expedition of 1832 to 1834 explored much of the Oregon trail and brought wagons up the Platte, North Platte, Sweetwater route across South Pass to the Green River in Wyoming. He explored most of Idaho and the Oregon Trail to the Columbia. The account of his explorations in the west was published by

text: Washington Irving

text: in 1838.).

text: John C. Frémont

text: of the

text: U.S. Army's Corps of Topographical Engineers

text: and his guide Kit Carson led three expeditions from 1842 to 1846 over parts of California and Oregon. His explorations were written up by him and his wife

text: Jessie Benton Frémont

text: and were widely published. The first "decent" map of California and Oregon were drawn by Frémont and his

text: topographer

text: s and

text: cartographers

text: in about 1848.

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answers: about 1848

text: Topographic map of Vlissingen (city), Sept. 2014

text: Topographic map of Vlissingen (city), Sept. 2014

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answers: 1000 feet

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text: Besides being a topographic map of surprisingly modern aspect, the Turin Papyrus is also a geological map (the earliest known) because it accurately shows the local distribution of different rock types (with black and pink hills), the lithologically diverse wadi gravels (with brown, green and white dots), and it contains information on quarrying and mining. The draughtsman clearly and carefully distributed distinctive features in accordance with the reality of a particular area, adding clarity by the use of legends and contrasting colors. In this respect, the Turin Papyrus may be regarded as the earliest known Geographic Information System.<ref>McMahon, David M., "The Turin Papyrus Map The Oldest Known Map with Geological Significance", Earth Sciences History 11 no. 1 (1992): 9-12.

text: Besides being a

text: topographic map

text: of surprisingly modern aspect, the Turin Papyrus is also a

text: geological map

text: (the earliest known) because it accurately shows the local distribution of different rock types (with black and pink hills), the

text: lithologically

text: diverse wadi

text: gravel

text: s (with brown, green and white dots), and it contains information on quarrying and mining. The draughtsman clearly and carefully distributed distinctive features in accordance with the reality of a particular area, adding clarity by the use of legends and contrasting colors. In this respect, the Turin Papyrus may be regarded as the earliest known

text: Geographic Information System

text: .<ref>McMahon, David M., "The Turin Papyrus Map The Oldest Known Map with Geological Significance", Earth Sciences History 11 no. 1 (1992): 9-12.

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answers: NDQ_001588

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answers: NDQ_001590

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answers: NDQ_001592

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: topographic map

answers: NDQ_001598

answers: contrasting colors

answers: NDQ_001600

answers: hills

answers: NDQ_001603

answers: It accurately shows the local distribution

answers: NDQ_001605

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answers: NDQ_001606

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answers: NDQ_001608

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answers: NDQ_001613

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answers: NDQ_001623

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answers: NDQ_001624

answers: brown, green and white dots

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answers: 9-12

text: The whole north western corner of Ardnamurchan contains a complex of underground volcanic structures, often described, perhaps inaccurately, as a caldera. It is in fact known that the structure of the north-western corner of the Ardnamurchan peninsula is due to a lopolith (previously interpreted as a ring dyke) which has been exposed at the surface. Evidence for a lopolith is seen in rock exposures in the area which show plagioclase crystals aligned towards the centre of the complex, an alignment caused by magmatic flow within a lopolith. Relatively small areas of lava that were ejected onto the surface are found in some parts of the peninsula. At least seven other similar complexes of the same tectonic episode are dotted up the west coast of Britain, and these are popular sites for many university geological training courses. Geological research is continuing in the area. The sub-concentric rings of the volcanic complex can easily be seen in satellite photographs and topographic maps, though they are less obvious on the ground.

text: The whole north western corner of Ardnamurchan contains a complex of underground volcanic structures, often described, perhaps inaccurately, as a

text: caldera

text: . It is in fact known that the structure of the north-western corner of the Ardnamurchan peninsula is due to a

text: lopolith

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answers: NDQ_001587

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answers: NDQ_001588

answers: parallel

answers: NDQ_001589

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answers: NDQ_001590

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answers: NDQ_001591

answers: sub-concentric rings

answers: NDQ_001592

answers: satellite photographs

answers: NDQ_001593

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answers: NDQ_001594

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answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001613

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answers: NDQ_001614

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answers: The sub-concentric rings

answers: NDQ_001619

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answers: NDQ_001621

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answers: NDQ_001623

answers: dyke

answers: NDQ_001624

answers: The sub-concentric rings

answers: NDQ_001625

answers: sub-concentric rings

text: Land forms are shown using contour lines with a contour interval of 5 metres. Additional symbols are provided to show e.g. earth bank, knoll, depression, small depression, pit, broken ground etc.

text: Land forms are shown using

text: contour line

text: s with a contour interval of 5 metres. Additional symbols are provided to show e.g. earth bank,

text: knoll

text: depression

text: , small depression, pit, broken ground etc.

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text: Messent Peak () is one of the Bristly Peaks, rising to about  just west of Brodie Peak and  southwest of Mount Castro in the central Antarctic Peninsula. It was named by the Advisory Committee on Antarctic Names in 1977 for David R. Messent, a geodesist at the U.S. Army Topographic Command (later the Defense Mapping Agency, Hydrographic/Topographic Center), Palmer Station, winter party 1969.

text: Messent Peak () is one of the

text: Bristly Peaks

text: , rising to about  just west of

text: Brodie Peak

text: and  southwest of

text: Mount Castro

text: in the central

text: Antarctic Peninsula

text: . It was named by the

text: Advisory Committee on Antarctic Names

text: in 1977 for

text: David R. Messent

text: , a geodesist at the U.S. Army Topographic Command (later the

text: Defense Mapping Agency

text: , Hydrographic/Topographic Center),

text: Palmer Station

text: , winter party 1969.

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text: The Nyquist contour mapped through the function

text: The Nyquist contour mapped through the function

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answers: The Nyquist contour mapped through the function

answers: NDQ_001590

answers: Nyquist function

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answers: NDQ_001613

answers: hatch marks are drawn on the side of the circle with the higher elevation.

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text: As they evolved, topographic map series became a national resource in modern nations in planning infrastructure and resource exploitation. In the United States, the national map-making function which had been shared by both the Army Corps of Engineers and the Department of the Interior migrated to the newly created United States Geological Survey in 1879, where it has remained since.

text: As they evolved, topographic map series became a national resource in modern nations in planning infrastructure and resource exploitation. In the United States, the national map-making function which had been shared by both the

text: Army Corps of Engineers

text: and the

text: Department of the Interior

text: migrated to the newly created

text: United States Geological Survey

text: in 1879, where it has remained since.

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answers: NDQ_001586

answers: topographic map

answers: NDQ_001587

answers: topographic map series

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: a national resource in modern nations

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: infrastructure

answers: NDQ_001592

answers: resource exploitation

answers: NDQ_001593

answers: topographic map

answers: NDQ_001594

answers: Bathymetric map

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: topographic map

answers: NDQ_001598

answers: topographic map

answers: NDQ_001600

answers: Plain or plateau

answers: NDQ_001603

answers: Geological Survey

answers: NDQ_001605

answers: Geological Survey

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic map

answers: NDQ_001611

answers: topographic map

answers: NDQ_001613

answers: topographic map series

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: topographic

answers: NDQ_001619

answers: topographic

answers: NDQ_001620

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answers: NDQ_001621

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text: The idea of lines that join points of equal value was rediscovered several times.  In 1701, Edmond Halley used such lines (isogons) on a chart of magnetic variation.  The Dutch engineer Nicholas Cruquius drew the bed of the river Merwede with lines of equal depth (isobaths) at intervals of 1 fathom in 1727, and Philippe Buache used them at 10-fathom intervals on a chart of the English Channel that was prepared in 1737 and published in 1752.  Such lines were used to describe a land surface (contour lines) in a map of the Duchy of Modena and Reggio by Domenico Vandelli in 1746, and they were studied theoretically by Ducarla in 1771, and Charles Hutton used them in the Schiehallion experiment.  In 1791, a map of France by J. L. Dupain-Triel used contour lines at 20-metre intervals, hachures, spot-heights and a vertical section.  In 1801, the chief of the Corps of Engineers, Haxo, used contour lines at the larger scale of 1:500 on a plan of his projects for Rocca d'Aufo.

text: The idea of lines that join points of equal value was rediscovered several times.  In 1701,

text: Edmond Halley

text: used such lines (isogons) on a chart of magnetic variation.  The

text: Dutch

text: engineer

text: Nicholas Cruquius

text: drew the bed of the river

text: Merwede

text: with lines of equal depth (isobaths) at intervals of 1

text: fathom

text: in 1727, and

text: Philippe Buache

text: used them at 10-fathom intervals on a chart of the

text: English Channel

text: that was prepared in 1737 and published in 1752.  Such lines were used to describe a land surface (contour lines) in a map of the Duchy of Modena and Reggio by Domenico Vandelli in 1746, and they were studied theoretically by Ducarla in 1771, and

text: Charles Hutton

text: used them in the

text: Schiehallion experiment

text: .  In 1791, a map of

text: France

text: by J. L. Dupain-Triel used contour lines at 20-metre intervals, hachures, spot-heights and a vertical section.  In 1801, the chief of the Corps of Engineers,

text: Haxo

text: , used contour lines at the larger scale of 1:500 on a plan of his projects for Rocca d'Aufo.

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text: The program originally allowed volunteers to collect geographic coordinates (latitude and longitude) via GPS receivers. The data was entered in spreadsheet format or in ESRI shapefiles and submitted via e-mail to the USGS National Geospatial Technical Operations Center(s) in Denver, Colorado, and Rolla, Missouri. During the registration process, prospective volunteers submitted a list of the 7.5 minute quadrangle maps on which they wished to work. Once accepted into the project, volunteers received their assignment and 1:24,000 scale topographic map of their quad. While there was no deadline for completing maps, the project's administrators preferred volunteers to submit coordinates for all structures in the quad no more than one year after beginning work.

text: The program originally allowed volunteers to collect

text: geographic coordinates

text: latitude

text: and

text: longitude

text: ) via

text: GPS

text: receivers. The data was entered in

text: spreadsheet

text: format or in

text: ESRI

text: shapefile

text: s and submitted via e-mail to the USGS National Geospatial Technical Operations Center(s) in

text: Denver, Colorado

text: , and

text: Rolla, Missouri

text: . During the registration process, prospective volunteers submitted a list of the 7.5 minute

text: quadrangle

text: maps on which they wished to work. Once accepted into the project, volunteers received their assignment and 1:24,000 scale

text: topographic map

text: of their quad. While there was no deadline for completing maps, the project's administrators preferred volunteers to submit coordinates for all structures in the quad no more than one year after beginning work.

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text: Anticyclogenesis is the development or strengthening of anticyclonic circulation in the atmosphere. It is the opposite of anticyclolysis, and has a cyclonic equivalent—cyclogenesis.  Anticyclones are alternatively referred to as high pressure systems.  High pressure areas form due to downward motion through the troposphere, the atmospheric layer where weather occurs.  Preferred areas within a synoptic flow pattern in higher levels of the troposphere are beneath the western side of troughs.  On weather maps, these areas show converging winds (isotachs), also known as confluence, or converging height lines near or above the level of non-divergence, which is near the 500 hPa pressure surface about midway up through the troposphere.  On weather maps, high pressure centers are associated with the letter H.  On constant pressure upper level charts, it is located within the highest height line contour.

text: Anticyclogenesis is the development or strengthening of

text: anticyclonic circulation

text: in the atmosphere. It is the opposite of

text: anticyclolysis

text: , and has a cyclonic equivalent—

text: cyclogenesis

text: .  Anticyclones are alternatively referred to as

text: high pressure systems

text: .  High pressure areas form due to downward motion through the

text: troposphere

text: , the

text: atmospheric

text: layer where

text: weather

text: occurs.  Preferred areas within a

text: synoptic

text: flow pattern in higher levels of the troposphere are beneath the western side of troughs.  On weather maps, these areas show converging winds (isotachs), also known as

text: confluence

text: , or converging height lines near or above the level of non-divergence, which is near the 500 hPa pressure surface about midway up through the troposphere.  On weather maps, high pressure centers are associated with the letter H.  On constant pressure upper level charts, it is located within the highest height line contour.

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answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: isotachs

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: high pressure centers are associated with the letter H

answers: NDQ_001590

answers: contour

answers: NDQ_001591

answers: high pressure centers

answers: NDQ_001592

answers: Anticyclogenesis

answers: NDQ_001593

answers: high pressure centers are associated with the letter H

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: On constant pressure upper level charts

answers: NDQ_001598

answers: highest height line contour

answers: NDQ_001600

answers: troughs

answers: NDQ_001603

answers: On weather maps

answers: NDQ_001605

answers: On weather maps

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: On constant pressure upper level charts

answers: NDQ_001611

answers: converging height lines

answers: NDQ_001613

answers: On constant pressure upper level charts

answers: NDQ_001614

answers: topographic maps

answers: NDQ_001618

answers: high pressure centers

answers: NDQ_001619

answers: contour

answers: NDQ_001620

answers: height line

answers: NDQ_001621

answers: contour

answers: NDQ_001622

answers: high pressure centers

answers: NDQ_001623

answers: height line

answers: NDQ_001624

answers: highest height line

answers: NDQ_001625

answers: highest height line

text: The gap's midpoint is located at , which is 1.07 km west of Kuzman Knoll, 2.39 km northwest of Zograf Peak, 3.76 km north of Mount Friesland, 2.64 km east-northeast of Pliska Peak, 3.79 km east of Burdick Peak, 2.49 km south-southeast of Mount Bowles and 1.53 km south of Montana Bluff.  British mapping in 1968 and Spanish in 1991, Bulgarian topographic surveys in 1995/96 and 2004/05, and mapping in 1996, 2005 and 2009.

text: The gap's midpoint is located at , which is 1.07 km west of

text: Kuzman Knoll

text: , 2.39 km northwest of

text: Zograf Peak

text: , 3.76 km north of

text: Mount Friesland

text: , 2.64 km east-northeast of

text: Pliska Peak

text: , 3.79 km east of

text: Burdick Peak

text: , 2.49 km south-southeast of

text: Mount Bowles

text: and 1.53 km south of

text: Montana Bluff

text: .  British mapping in 1968 and Spanish in 1991, Bulgarian topographic surveys in 1995/96 and

text: , and mapping in 1996, 2005 and 2009.

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

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answers: NDQ_001624

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answers: NDQ_001625

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answers: NDQ_001586

answers: The gap's midpoint

answers: NDQ_001587

answers: The gap's midpoint is located at

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: British mapping in 1968 and Spanish in 1991

answers: NDQ_001590

answers: The gap's midpoint is located at

answers: NDQ_001591

answers: the gap

answers: NDQ_001592

answers: midpoint is located at

answers: NDQ_001593

answers: 2.49 km south-southeast of Mount Bowles and 1.53 km south of Montana Bluff

answers: NDQ_001594

answers: The gap's midpoint is located at, which is 1.07 km west of Kuzman Knoll

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: 2.49 km south-southeast

answers: NDQ_001598

answers: east-northeast

answers: NDQ_001600

answers: The gap's midpoint

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: The gap's midpoint is located

answers: NDQ_001606

answers: The gap's midpoint

answers: NDQ_001608

answers: British mapping in 1968 and Spanish in 1991

answers: NDQ_001611

answers: Kuzman Knoll

answers: NDQ_001613

answers: The gap's midpoint is located at

answers: NDQ_001614

answers: The gap's midpoint

answers: NDQ_001618

answers: Kuzman Knoll

answers: NDQ_001619

answers: Montana Bluff

answers: NDQ_001620

answers: The gap's midpoint

answers: NDQ_001621

answers: topographic surveys

answers: NDQ_001622

answers: The gap

answers: NDQ_001623

answers: The gap

answers: NDQ_001624

answers: The gap

answers: NDQ_001625

answers: 1.07 km

text: A topographical map is the main type of map used to depict elevation, often through use of contour lines.In a Geographic Information System (GIS), digital elevation models (DEM) are commonly used to represent the surface (topography) of a place, through a raster (grid) dataset of elevations.  Digital terrain models are another way to represent terrain in GIS.

text: A

text: topographical map

text: is the main type of

text: map

text: used to depict elevation, often through use of

text: contour line

text: s.In a

text: Geographic Information System

text: (GIS),

text: digital elevation model

text: s (DEM) are commonly used to represent the surface (topography) of a place, through a

text: raster

text: (grid) dataset of elevations.

text: Digital terrain model

text: s are another way to represent terrain in GIS.

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answers: NDQ_001620

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answers: NDQ_001622

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answers: NDQ_001623

answers: 4

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: contour lines

answers: NDQ_001587

answers: contour lines

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: use of contour lines

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: elevation

answers: NDQ_001592

answers: depict elevation

answers: NDQ_001593

answers: elevation

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: contour lines

answers: NDQ_001598

answers: contour lines

answers: NDQ_001600

answers: contour lines

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: contour lines

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topography

answers: NDQ_001611

answers: contour lines

answers: NDQ_001613

answers: contour lines

answers: NDQ_001614

answers: topographic map

answers: NDQ_001618

answers: elevation

answers: NDQ_001619

answers: contour lines

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: topography

answers: NDQ_001622

answers: elevation

answers: NDQ_001623

answers: contour lines

answers: NDQ_001624

answers: elevation

answers: NDQ_001625

answers: contour lines

text: The peak is located at  which is 890 m east of Castillo Nunatak, 4.66 km east-southeast of Sinemorets Hill, 2.36 km south-southwest of Burdick Peak, 2.48 km west-southwest of Pliska Peak, 4.96 km west-northwest of Mount Friesland, 4.63 km north-northwest of Stambolov Crag and 3.21 km northeast of Napier Peak.  British mapping in 1968, Spanish in 1991, and Bulgarian topographic survey in 1995/96 and mapping in 1996, 2005 and 2009.

text: The peak is located at  which is 890 m east of Castillo Nunatak, 4.66 km east-southeast of

text: Sinemorets Hill

text: , 2.36 km south-southwest of

text: Burdick Peak

text: , 2.48 km west-southwest of

text: Pliska Peak

text: , 4.96 km west-northwest of

text: Mount Friesland

text: , 4.63 km north-northwest of

text: Stambolov Crag

text: and 3.21 km northeast of

text: Napier Peak

text: .  British mapping in 1968, Spanish in 1991, and Bulgarian topographic survey in 1995/96 and mapping in 1996, 2005 and 2009.

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answers: 0: The answer is not relevant or complete at all.

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answers: The peak is located at which is 890 m

answers: NDQ_001587

answers: The peak is located at which is 890 m east of Castillo Nunatak

answers: NDQ_001588

answers: Parallel

answers: NDQ_001589

answers: The peak is located at which is 890 m east of Castillo Nunatak

answers: NDQ_001590

answers: 2.48 km west-southwest of Pliska Peak

answers: NDQ_001591

answers: Napier Peak

answers: NDQ_001592

answers: the peak is located at

answers: NDQ_001593

answers: 4.66 km east-southeast of Sinemorets Hill

answers: NDQ_001594

answers: Contour lines represent the distance to the bottom of the water

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: west-northwest

answers: NDQ_001598

answers: west-southwest

answers: NDQ_001600

answers: Castillo Nunatak

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: Stambolov Crag

answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: Contour lines help us to see the three-dimensional shape of the land.

answers: NDQ_001611

answers: Sinemorets Hill

answers: NDQ_001613

answers: The peak is located at which is 890 m east of Castillo Nunatak

answers: NDQ_001614

answers: Horizontal distances cannot be shown on topographic maps.

answers: NDQ_001618

answers: Burdick Peak

answers: NDQ_001619

answers: depth map

answers: NDQ_001620

answers: 890 m

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: Castillo Nunatak

answers: NDQ_001623

answers: Burdick Peak

answers: NDQ_001624

answers: Castillo Nunatak

answers: NDQ_001625

answers: 2.48 km

text: The following are lists of mountains in New Zealand ordered by height. Names, heights, topographic prominence and isolation, and coordinates were extracted from the official Land Information New Zealand (LINZ) Topo50 topographic maps at the interactive topographic map of New Zealand site.

text: The following are lists of mountains in

text: New Zealand

text: ordered by height. Names, heights, topographic

text: prominence

text: and

text: isolation

text: , and coordinates were extracted from the official

text: Land Information New Zealand

text: (LINZ) Topo50 topographic maps at the interactive topographic map of New Zealand site.

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answers: Topo50

answers: NDQ_001587

answers: New Zealand

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: topographic prominence and isolation

answers: NDQ_001590

answers: Topo50

answers: NDQ_001591

answers: mountains

answers: NDQ_001592

answers: lists of mountains in New Zealand ordered by height

answers: NDQ_001593

answers: topographic prominence

answers: NDQ_001594

answers: Topo50

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: coordinates

answers: NDQ_001598

answers: topographic prominence

answers: NDQ_001600

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answers: NDQ_001603

answers: interactive topographic map

answers: NDQ_001605

answers: Topo50

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: Topographic

answers: NDQ_001611

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answers: NDQ_001613

answers: topographic prominence and isolation

answers: NDQ_001614

answers: Topographic maps

answers: NDQ_001618

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answers: NDQ_001619

answers: Topographic

answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001622

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answers: NDQ_001623

answers: topographic prominence

answers: NDQ_001624

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answers: NDQ_001625

answers: Topo50

text: The Land Registry Kadaster (formerly Topografische Dienst) collects, processes and provides topographical information of the entire Dutch territory. The history of the Land Registry goes back to the year 1815, that year was commissioned to create a large map, known as Map of Krayenhoff. Around 1836 they began printing the topographic map on a scale of 1: 50,000, followed in 1865 by the topographic map on a scale of 1: 25,000. In 1951 began the start of production of the topographic map on a scale of 1: 10,000. From various reorganizations arose in 1932 the Topografische Dienst as national mapping agency of the Netherlands, since January 2004 housed within the Land Registry Kadaster.

text: The Land Registry

text: Kadaster

text: (formerly Topografische Dienst) collects, processes and provides topographical information of the entire Dutch territory. The history of the Land Registry goes back to the year 1815, that year was commissioned to create a large map, known as Map of Krayenhoff. Around 1836 they began printing the topographic map on a scale of 1: 50,000, followed in 1865 by the topographic map on a scale of 1: 25,000. In 1951 began the start of production of the topographic map on a scale of 1: 10,000. From various reorganizations arose in 1932 the Topografische Dienst as

text: national mapping agency

text: of the Netherlands, since January 2004 housed within the Land Registry Kadaster.

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text: Matthes believed topographers should not merely draw lines but also study the geology of the land forms to produce relevant maps.  To that end, Matthes wrote his first scientific publication during the winter of 1899 entitled Glacial Sculpture of the Bighorn Mountains, Wyoming which served as a standard reference and in which Matthes applied the first usage of the term "nivation".  His geologic writing was not a customary effort for topographers and his descriptive style was critiqued by the USGS but the popularity of his narratives continues today.

text: Matthes believed topographers should not merely draw lines but also study the geology of the land forms to produce relevant maps.  To that end, Matthes wrote his first scientific publication during the winter of 1899 entitled Glacial Sculpture of the Bighorn Mountains, Wyoming which served as a standard reference and in which Matthes applied the first usage of the term "

text: nivation

text: ".  His geologic writing was not a customary effort for topographers and his descriptive style was critiqued by the USGS but the popularity of his narratives continues today.

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answers: 135 m

text: A note about methodology: when using a topographic map to determine prominence, one often has to estimate the height of the key col (and sometimes, the height of the peak as well) based on the contour lines. Assume for simplicity that only the col elevation is uncertain. There are three simple choices.  The pessimistic, or clean prominence, assumes that the col is as high as it can be, i.e., its elevation is that of the higher contour line nearest the saddle. This gives a lower bound on the possible prominence of the peak, ignoring map error; inaccuracies in mapping lead to further uncertainties and a larger error bound.  Optimistic prominence assumes that the col is as low as possible, yielding an upper bound value for the prominence. Midrange or mean prominence uses the mean of these two values. Mean prominence is sometimes referred to as rise. In Britain, where topographic mapping is more detailed than in many countries, it is customary to use a fourth method: interpolated prominence. The true prominence is estimated by visualising the three dimensional surface in the neighborhood of the col and interpolating between the enclosing contours.

text: A note about methodology: when using a

text: topographic map

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answers: 0

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answers: 4

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answers: 0

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answers: 4

answers: NDQ_001589

answers: 0

answers: NDQ_001590

answers: 4

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 0

answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 0

answers: NDQ_001598

answers: 0

answers: NDQ_001600

answers: 0

answers: NDQ_001603

answers: 0

answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 4

answers: NDQ_001608

answers: 4

answers: NDQ_001611

answers: 0

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 0

answers: NDQ_001618

answers: 4

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 4

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 4

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: as high as it can be

answers: NDQ_001587

answers: is sometimes referred to as rise

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: ignoring map error; inaccuracies in mapping lead to further uncertainties and a larger error bound

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: height of the key col

answers: NDQ_001592

answers: estimate the height of the key col

answers: NDQ_001593

answers: contour lines

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: unanswerable

answers: NDQ_001598

answers: contour lines

answers: NDQ_001600

answers: saddle

answers: NDQ_001603

answers: using a topographic map

answers: NDQ_001605

answers: contour lines

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: topographic map

answers: NDQ_001611

answers: contour lines

answers: NDQ_001613

answers: pessimistic, or clean prominence

answers: NDQ_001614

answers: contour lines

answers: NDQ_001618

answers: col

answers: NDQ_001619

answers: contour lines

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: topographic map

answers: NDQ_001622

answers: col

answers: NDQ_001623

answers: contour lines

answers: NDQ_001624

answers: saddle

answers: NDQ_001625

answers: higher contour line nearest the saddle

text: For Waipiata topographic info see Map 260 H42 Waipiata - LINZ

text: For Waipiata topographic info see Map 260 H42 Waipiata - LINZ

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

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answers: 0

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answers: 0

answers: NDQ_001586

answers: 4

answers: NDQ_001587

answers: 0

answers: NDQ_001588

answers: 0

answers: NDQ_001589

answers: 0

answers: NDQ_001590

answers: 0

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 4

answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 0

answers: NDQ_001598

answers: 0

answers: NDQ_001600

answers: 0

answers: NDQ_001603

answers: 0

answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 0

answers: NDQ_001608

answers: 4

answers: NDQ_001611

answers: 0

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 0

answers: NDQ_001618

answers: 0

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 0

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: LINZ

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: Waipiata

answers: NDQ_001587

answers: Waipiata

answers: NDQ_001588

answers: parallel

answers: NDQ_001589

answers: Waipiata topographic info

answers: NDQ_001590

answers: Waipiata

answers: NDQ_001591

answers: topographic info

answers: NDQ_001592

answers: LINZ

answers: NDQ_001593

answers: Waipiata

answers: NDQ_001594

answers: Waipiata

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Waipiata

answers: NDQ_001598

answers: Waipiata

answers: NDQ_001600

answers: a plain

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: LINZ

answers: NDQ_001606

answers: Contour interval

answers: NDQ_001608

answers: Waipiata

answers: NDQ_001611

answers: Waipiata

answers: NDQ_001613

answers: Waipiata

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: topographic

answers: NDQ_001619

answers: Waipiata

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: topographic

answers: NDQ_001622

answers: topographic

answers: NDQ_001623

answers: LINZ

answers: NDQ_001624

answers: LINZ

answers: NDQ_001625

answers: LINZ

text: A variety of techniques have been used to establish the topographic maps in the brain.  The existence of topographical maps was shown early by electrical stimulation of the cortex, tracing patterns of epileptic seizures, stimulation sequences, and impairments due to lesions.  Details in the maps came later through microelectrode stimulation and recording techniques became commonly used in demonstrating somatotopic maps and later in the auditory and visual systems, both cortically and in subcortical structures such as the colliculi and geniculate nuclei of the thalamus.  Single-cell recording, Transcranial magnetic stimulation(TMS), electrical stimulation of the cortex, and Functional magnetic resonance imaging(fMRI) are some of the techniques used to study maps in the brain.  Many of the existing topographic maps have been further studied or refined using fMRI.  For example, Hubel and Wiesel originally studied the retinotopic maps in the primary visual cortex using single-cell recording.  Recently, however, imaging of the retinotopic map in the cortex and in sub-cortical areas, such as the lateral geniculate nucleus, have been improved using the fMRI technique.

text: A variety of techniques have been used to establish the topographic maps in the brain.  The existence of topographical maps was shown early by electrical stimulation of the cortex, tracing patterns of epileptic seizures, stimulation sequences, and impairments due to lesions.  Details in the maps came later through

text: microelectrode

text: stimulation and recording techniques became commonly used in demonstrating somatotopic maps and later in the auditory and visual systems, both cortically and in subcortical structures such as the

text: colliculi

text: and

text: geniculate nuclei

text: of the

text: thalamus

text: Single-cell recording

text: Transcranial magnetic stimulation

text: (TMS), electrical stimulation of the cortex, and

text: Functional magnetic resonance imaging

text: (fMRI) are some of the techniques used to study maps in the brain.  Many of the existing topographic maps have been further studied or refined using fMRI.  For example,

text: Hubel

text: and

text: Wiesel

text: originally studied the retinotopic maps in the primary visual cortex using single-cell recording.  Recently, however, imaging of the retinotopic map in the cortex and in sub-cortical areas, such as the lateral geniculate nucleus, have been improved using the fMRI technique.

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answers: Functional magnetic resonance imaging(fMRI)

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answers: 1  100

text: The YJ-22 is a LACM (land-attack cruise missile) development of the anti-ship C-802 with a 400 km range, and possible Satellite guidance/terrain mapping guidance currently said to be under development, Initial Operational Capability was expected after 2005. This 135-kilometer range system would be the first Chinese cruise missile to incorporate BeiDou Navigation Satellite System-assisted navigation. Satellite-aided guidance could be augmented by terrain contour matching TERCOM (Terrain Contour Matching) guidance. Some sources believe BeiDou-aided navigation could result in cruise missiles like the YJ-22 to achieve accuracies of up to 10 meters.

text: The YJ-22 is a LACM (land-attack

text: cruise missile

text: ) development of the anti-ship

text: with a 400 km range, and possible

text: Satellite guidance

text: terrain mapping

text: guidance currently said to be under development,

text: Initial Operational Capability

text: was expected after 2005. This 135-kilometer range system would be the first Chinese cruise missile to incorporate

text: BeiDou Navigation Satellite System

text: -assisted navigation. Satellite-aided guidance could be augmented by terrain contour matching

text: TERCOM

text: (Terrain Contour Matching) guidance. Some sources believe BeiDou-aided navigation could result in cruise missiles like the YJ-22 to achieve accuracies of up to 10 meters.

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answers: NDQ_001611

answers: terrain contour matching

answers: NDQ_001613

answers: BeiDou Navigation Satellite System

answers: NDQ_001614

answers: terrain contour

answers: NDQ_001618

answers: TERCOM

answers: NDQ_001619

answers: terrain contour

answers: NDQ_001620

answers: meters

answers: NDQ_001621

answers: terrain contour

answers: NDQ_001622

answers: terrain

answers: NDQ_001623

answers: terrain contour

answers: NDQ_001624

answers: terrain

answers: NDQ_001625

answers: 10 meters

text: This is a list of highest points in the U.S. state of Arizona, in alphabetical order by county. Elevations are from USGS 1:24,000 scale topographic quadrangle maps. Elevations followed by a plus sign (+) are minimal values. The contour interval is shown after the (+).

text: This is a list of highest points in the U.S. state of

text: Arizona

text: , in alphabetical order by county. Elevations are from USGS 1:24,000 scale topographic quadrangle maps. Elevations followed by a plus sign (+) are minimal values. The contour interval is shown after the (+).

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answers: NDQ_001625

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answers: NDQ_001586

answers: The contour interval

answers: NDQ_001587

answers: USGS 1:24,000 scale topographic quadrangle maps

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: The contour interval is shown after the (+)

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: minimal values

answers: NDQ_001592

answers: alphabetical order by county

answers: NDQ_001593

answers: The contour interval

answers: NDQ_001594

answers: contour interval

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: contour interval

answers: NDQ_001598

answers: contour interval

answers: NDQ_001600

answers: contour interval

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: contour interval

answers: NDQ_001606

answers: The contour interval

answers: NDQ_001608

answers: contour interval

answers: NDQ_001611

answers: The contour interval

answers: NDQ_001613

answers: The contour interval

answers: NDQ_001614

answers: Elevations

answers: NDQ_001618

answers: contour interval

answers: NDQ_001619

answers: contour interval

answers: NDQ_001620

answers: The contour interval

answers: NDQ_001621

answers: topographic quadrangle maps

answers: NDQ_001622

answers: contour interval

answers: NDQ_001623

answers: contour interval

answers: NDQ_001624

answers: contour interval

answers: NDQ_001625

answers: 1:24,000

text: In the United Kingdom the term geological map is used. The UK and Isle of Man have been extensively mapped by the British Geological Survey (BGS) since 1835; a separate Geological Survey of Northern Ireland (drawing on BGS staff) has operated since 1947.

text: In the

text: United Kingdom

text: the term geological map is used. The UK and

text: Isle of Man

text: have been extensively mapped by the

text: British Geological Survey

text: (BGS) since 1835; a separate Geological Survey of Northern Ireland (drawing on BGS staff) has operated since 1947.

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text: The equirectangular projection (also called the equidistant cylindrical projection, geographic projection, or la carte parallélogrammatique projection, and which includes the special case of the plate carrée projection or geographic projection) is a simple map projection attributed to Marinus of Tyre, who Ptolemy claims invented the projection about AD 100. The projection maps meridians to vertical straight lines of constant spacing (for meridional intervals of constant spacing), and circles of latitude to horizontal straight lines of constant spacing (for constant intervals of parallels). The projection is neither equal area nor conformal. Because of the distortions introduced by this projection, it has little use in navigation or cadastral mapping and finds its main use in thematic mapping. In particular, the plate carrée has become a standard for global raster datasets, such as Celestia and NASA World Wind, because of the particularly simple relationship between the position of an image pixel on the map and its corresponding geographic location on Earth.

text: The equirectangular projection (also called the equidistant cylindrical projection, geographic projection, or la carte parallélogrammatique projection, and which includes the special case of the plate carrée projection or geographic projection) is a simple

text: map projection

text: attributed to

text: Marinus of Tyre

text: , who

text: Ptolemy

text: claims invented the projection about AD 100. The projection maps

text: meridians

text: to vertical straight lines of constant spacing (for

text: meridional

text: intervals of constant spacing), and

text: circles of latitude

text: to horizontal straight lines of constant spacing (for constant intervals of

text: parallels

text: ). The projection is neither equal area nor

text: conformal

text: . Because of the distortions introduced by this projection, it has little use in

text: navigation

text: or

text: cadastral

text: mapping and finds its main use in

text: thematic map

text: ping. In particular, the plate carrée has become a standard for global

text: raster datasets

text: , such as

text: Celestia

text: and

text: NASA World Wind

text: , because of the particularly simple relationship between the position of an

text: image pixel

text: on the map and its corresponding geographic location on Earth.

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answers: Because of the distortions introduced by this projection, it has little use in navigation or cadastral mapping and finds its main use in thematic mapping

answers: NDQ_001594

answers: bathymetric

answers: NDQ_001595

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answers: NDQ_001597

answers: Because of the distortions introduced by this projection, it has little use in navigation or cadastral mapping

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answers: NDQ_001600

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answers: NDQ_001603

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text: In discussing pollution, density maps can be very useful in indicating sources and areas of greatest contamination. Contour maps are especially useful for diffuse forms or scales of pollution. Acid precipitation is indicated on maps with isoplats.  Some of the most widespread applications of environmental science contour maps involve mapping of environmental noise (where lines of equal sound pressure level are denoted isobels), air pollution, soil contamination, thermal pollution and groundwater contamination.  By contour planting and contour ploughing, the rate of water runoff and thus soil erosion can be substantially reduced; this is especially important in riparian zones.

text: In discussing pollution, density maps can be very useful in indicating sources and areas of greatest contamination. Contour maps are especially useful for diffuse forms or scales of pollution. Acid precipitation is indicated on maps with isoplats.  Some of the most widespread applications of environmental science contour maps involve mapping of

text: environmental noise

text: (where lines of equal sound pressure level are denoted isobels),

text: air pollution

text: soil contamination

text: thermal pollution

text: and

text: groundwater

text: contamination.  By

text: contour planting

text: and

text: contour ploughing

text: , the rate of

text: water runoff

text: and thus

text: soil erosion

text: can be substantially reduced; this is especially important in

text: riparian

text: zones.

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answers: acid precipitation is indicated on maps with isoplats

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: areas of greatest contamination

answers: NDQ_001592

answers: indicating sources and areas of greatest contamination

answers: NDQ_001593

answers: soil erosion

answers: NDQ_001594

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answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001598

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answers: isobels

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answers: lines of equal sound pressure level

text: Topographic maps for general use are available at 1:50,000 and 1:100,000 from the Hellenic Military Geographical Service (HMGS). They use a national projection system called EGSA'87, which is a Transverse Mercatorial Projection mapping Gre    ece in one zone. A few areas are also available at 1:25,000. Some private firms sell topographic maps of national parks based on HMGS topography.

text: Topographic maps for general use are available at 1:50,000 and 1:100,000 from the

text: Hellenic Military Geographical Service

text: (HMGS). They use a national projection system called EGSA'87, which is a Transverse Mercatorial Projection mapping Gre    ece in one zone. A few areas are also available at 1:25,000. Some private firms sell topographic maps of national parks based on HMGS topography.

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answers: 1:50,000

answers: NDQ_001586

answers: Topographic maps

answers: NDQ_001587

answers: EGSA'87

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: 1:25,000

answers: NDQ_001590

answers: 1:50,000

answers: NDQ_001591

answers: Transverse Mercatorial

answers: NDQ_001592

answers: 1:100,000

answers: NDQ_001593

answers: They use a national projection system

answers: NDQ_001594

answers: Bathymetric

answers: NDQ_001595

answers: 1:50,000

answers: NDQ_001597

answers: Transverse Mercatorial Projection

answers: NDQ_001598

answers: 1:25,000

answers: NDQ_001600

answers: 1:25,000

answers: NDQ_001603

answers: general use

answers: NDQ_001605

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answers: NDQ_001606

answers: 1:100,000

answers: NDQ_001608

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answers: NDQ_001611

answers: 1:25,000

answers: NDQ_001613

answers: 1:100,000

answers: NDQ_001614

answers: Transverse Mercatorial Projection

answers: NDQ_001618

answers: national parks

answers: NDQ_001619

answers: 1:25,000

answers: NDQ_001620

answers: 1:25,000

answers: NDQ_001621

answers: Topographic

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answers: 1:25,000

answers: NDQ_001624

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answers: NDQ_001625

answers: 1:25,000

text: Dutch Topographic map of Ommen, June 2015

text: Dutch Topographic map of Ommen, June 2015

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

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answers: NDQ_001587

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answers: NDQ_001588

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answers: NDQ_001589

answers: Topographic map of Ommen, June 2015

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: Ommen

answers: NDQ_001592

answers: orient itself

answers: NDQ_001593

answers: The slope of the land

answers: NDQ_001594

answers: contour lines

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

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answers: NDQ_001598

answers: The steepest side

answers: NDQ_001600

answers: a plain or plateau

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: different colors

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: contour lines

answers: NDQ_001611

answers: Concentric lines

answers: NDQ_001613

answers: the side of the circle with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Ommen

answers: NDQ_001619

answers: Topographic map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

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answers: NDQ_001622

answers: Ommen

answers: NDQ_001623

answers: equator

answers: NDQ_001624

answers: Ommen

answers: NDQ_001625

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text: Topographic map of North Versailles and surrounding area

text: Topographic map of North Versailles and surrounding area

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answers: contour lines

answers: NDQ_001587

answers: is a type of map

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: A bathymetric map is a map of the ocean.

answers: NDQ_001590

answers: The contour interval

answers: NDQ_001591

answers: surrounding area

answers: NDQ_001592

answers: map of North Versailles

answers: NDQ_001593

answers: The slope of the land

answers: NDQ_001594

answers: contour lines represent the distance to the bottom

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Rivers and streams flow north

answers: NDQ_001598

answers: The steepest side

answers: NDQ_001600

answers: Nearly touching

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: red

answers: NDQ_001606

answers: The difference between two contour lines

answers: NDQ_001608

answers: contour lines help us to see the three-dimensional shape

answers: NDQ_001611

answers: Concentric lines show a high, steep hill

answers: NDQ_001613

answers: The side of the circle with the higher elevation

answers: NDQ_001614

answers: horizontal

answers: NDQ_001618

answers: Topographic map

answers: NDQ_001619

answers: depth map

answers: NDQ_001620

answers: elevation

answers: NDQ_001621

answers: Topographic map

answers: NDQ_001622

answers: North Versailles

answers: NDQ_001623

answers: elevation line

answers: NDQ_001624

answers: North Versailles

answers: NDQ_001625

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text: The product of the calculations is usually a set of isopleths or mapped contour lines either in plan view or cross sectional view.  Typically these might be stated as concentrations of carbon monoxide, total reactive hydrocarbons, oxides of nitrogen, particulate or benzene.  The air quality scientist  can run the model successively to study techniques of reducing adverse air pollutant concentrations (for example, by redesigning roadway geometry, altering speed controls or limiting certain types of trucks).  The model is frequently utilized in an Environmental Impact Statement involving a major new roadway or land use change which will induce new vehicular traffic.

text: The product of the calculations is usually a set of isopleths or mapped

text: contour lines

text: either in

text: plan view

text: or

text: cross sectional

text: view.  Typically these might be stated as concentrations of

text: carbon monoxide

text: , total reactive

text: hydrocarbons

text: oxides of nitrogen

text: particulate

text: or

text: benzene

text: .  The air quality scientist  can run the model successively to study techniques of reducing adverse

text: air pollutant concentrations

text: (for example, by redesigning roadway geometry, altering speed controls or limiting certain types of trucks).  The model is frequently utilized in an

text: Environmental Impact Statement

text: involving a major new roadway or land use change which will induce new vehicular traffic.

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answers: NDQ_001590

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answers: NDQ_001592

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answers: NDQ_001597

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text: The highest point in Clark County, Washington, is Sturgeon Rock, a basalt outcrop that lies on the county line just west of the Silver Star summit.  For many years an error on United States Geological Survey topographical maps has misnamed a broad wooded peak lower on the ridge near the Tarbell Trail as Sturgeon Rock.

text: The highest point in

text: Clark County, Washington

text: , is Sturgeon Rock, a

text: basalt

text: outcrop that lies on the county line just west of the Silver Star summit.  For many years an error on

text: United States Geological Survey

text: topographical

text: maps

text: has misnamed a broad wooded peak lower on the ridge near the Tarbell Trail as Sturgeon Rock.

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answers: The highest point

answers: NDQ_001587

answers: basalt outcrop

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: the highest point in Clark County, Washington, is Sturgeon Rock

answers: NDQ_001590

answers: contour lines

answers: NDQ_001591

answers: the highest point

answers: NDQ_001592

answers: name a broad wooded peak

answers: NDQ_001593

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answers: NDQ_001594

answers: Sturgeon Rock

answers: NDQ_001595

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answers: NDQ_001597

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answers: NDQ_001598

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answers: NDQ_001600

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answers: NDQ_001603

answers: United States Geological Survey

answers: NDQ_001605

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answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

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answers: NDQ_001611

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answers: NDQ_001613

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answers: NDQ_001614

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answers: NDQ_001619

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answers: NDQ_001620

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answers: NDQ_001621

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answers: NDQ_001623

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answers: NDQ_001624

answers: Silver Star summit

answers: NDQ_001625

answers: Silver Star summit

text: The Institute was transferred to the Ministry of Interior in 1960 and expanded its operations to include some basic cartographic activities and extended research.  The organisation had benefited from the ]United States Point Four Programme of financial aid until it was discontinued in 1962, at which time the country entered into an agreement with the United States for the U.S. Army Map Service, later known as Topographic Command (Topocom), to produce base maps of the country.  The topographic surveying was provided by soldiers from the 64th Engineer Battalion, 29th Engineer Company, and the project was known as the Ethiopia-United States Mapping Mission.  Using the survey data from the Mapping Mission, The Army Map Service/Topocom completed the photogrammetric map compilation and cartographic map finishing operations.  The resulting 1:250,000-scale base maps of the country and 1:50,000-scale maps of special interest areas served as the impetus for the Institute to begin its cartographic map maintenance and distribution programme.  The organisation was placed under a Director General with two Directors and seventy employees, and was reorganized into three subdivisions:  Photogrammetry, Cartography and Photo Laboratory.  The Institute was reorganized again in 1980 and was renamed the Ethiopian Mapping Authority.

text: The Institute was transferred to the Ministry of Interior in 1960 and expanded its operations to include some basic cartographic activities and extended research.  The organisation had benefited from the ]

text: United States

text: Point Four Programme of financial aid until it was discontinued in 1962, at which time the country entered into an agreement with the United States for the

text: U.S. Army Map Service

text: , later known as Topographic Command (Topocom), to produce base maps of the country.  The

text: topographic surveying

text: was provided by soldiers from the 64th Engineer Battalion, 29th Engineer Company, and the project was known as the

entity_name: Ethiopia – United States Mapping Mission

text: Ethiopia-United States Mapping Mission

text: .  Using the survey data from the Mapping Mission, The Army Map Service/Topocom completed the photogrammetric map compilation and cartographic map finishing operations.  The resulting 1:250,000-scale base maps of the country and 1:50,000-scale maps of special interest areas served as the impetus for the Institute to begin its cartographic map maintenance and distribution programme.  The organisation was placed under a Director General with two Directors and seventy employees, and was reorganized into three subdivisions:

text: Photogrammetry

text: Cartography

text: and Photo Laboratory.  The Institute was reorganized again in 1980 and was renamed the Ethiopian Mapping Authority.

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text: In the United States, the FDA has approved LASIK for age 18 and over. More importantly the patient's eye prescription should be stable for at least one year prior to surgery.The patient may be examined with pupillary dilation and education given prior to the procedure. Before the surgery, the patient's corneas are examined with a pachymeter to determine their thickness, and with a topographer, or corneal topography machine, to measure their surface contour. Using low-power lasers, a topographer creates a topographic map of the cornea. The procedure is contraindicated if the topographer finds difficulties such as keratoconus The preparatory process also detects astigmatism and other irregularities in the shape of the cornea. Using this information, the surgeon calculates the amount and the location of corneal tissue to be removed. The patient is prescribed and self-administers an antibiotic beforehand to minimize the risk of infection after the procedure and is sometimes offered a short acting oral sedative medication as a pre-medication. Prior to the procedure, anaesthetic eye drops are instilled. Factors that may rule out LASIK for some patients include large pupils, thin corneas and extremely dry eyes.

text: In the United States, the FDA has approved LASIK for age 18 and over. More importantly the patient's eye prescription should be stable for at least one year prior to surgery.The patient may be examined with pupillary dilation and education given prior to the procedure. Before the surgery, the patient's

text: cornea

text: s are examined with a

text: pachymeter

text: to determine their thickness, and with a topographer, or corneal topography machine, to measure their surface contour. Using low-power

text: laser

text: s, a topographer creates a

text: topographic map

text: of the cornea. The procedure is contraindicated if the topographer finds difficulties such as

text: keratoconus

text: The preparatory process also detects

text: astigmatism

text: and other irregularities in the shape of the cornea. Using this information, the surgeon calculates the amount and the location of corneal tissue to be removed. The patient is prescribed and self-administers an antibiotic beforehand to minimize the risk of infection after the procedure and is sometimes offered a short acting oral sedative medication as a pre-medication. Prior to the procedure, anaesthetic eye drops are instilled. Factors that may rule out LASIK for some patients include large pupils, thin corneas and extremely dry eyes.

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answers: 0

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 0

answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 0

answers: NDQ_001598

answers: 0

answers: NDQ_001600

answers: 0

answers: NDQ_001603

answers: 0

answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 4

answers: NDQ_001608

answers: 0

answers: NDQ_001611

answers: 0

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 3

answers: NDQ_001618

answers: 0

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 0

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 0

answers: NDQ_001586

answers: contour lines that are numbered

answers: NDQ_001587

answers: corneas

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: topographer creates a topographic map of the cornea

answers: NDQ_001590

answers: surface contour

answers: NDQ_001591

answers: keratoconus

answers: NDQ_001592

answers: keratoconus

answers: NDQ_001593

answers: a topographic map

answers: NDQ_001594

answers: a topographer creates a topographic map of the cornea

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: Using low-power lasers

answers: NDQ_001598

answers: topographic map of the cornea

answers: NDQ_001600

answers: surface contour

answers: NDQ_001603

answers: unanswerable

answers: NDQ_001605

answers: geologic maps use different colors to represent different types of rocks

answers: NDQ_001606

answers: contour interval

answers: NDQ_001608

answers: surface contour

answers: NDQ_001611

answers: The patient may be examined with pupillary dilation and education given prior to the procedure

answers: NDQ_001613

answers: keratoconus

answers: NDQ_001614

answers: topographic map of the cornea

answers: NDQ_001618

answers: surface contour

answers: NDQ_001619

answers: topographic map

answers: NDQ_001620

answers: surface contour

answers: NDQ_001621

answers: topographic map

answers: NDQ_001622

answers: surface contour

answers: NDQ_001623

answers: topographic map

answers: NDQ_001624

answers: surface contour

answers: NDQ_001625

answers: surface contour

text: [[File:Lake Michigan bathymetry map.png|thumb|Lake Michigan bathymetric map. The deepest point is marked with "×".]]

text: [[File:Lake Michigan bathymetry map.png|thumb|Lake Michigan

text: bathymetric

text: map. The deepest point is marked with "×".]]

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answers: 5: The answer is highly relevant, complete, and accurate.

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answers: NDQ_001620

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answers: NDQ_001622

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answers: NDQ_001623

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answers: NDQ_001624

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answers: NDQ_001625

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answers: NDQ_001586

answers: The deepest point

answers: NDQ_001587

answers: The deepest point is marked with " "

answers: NDQ_001588

answers: intersect

answers: NDQ_001589

answers: The deepest point is marked with " "

answers: NDQ_001590

answers: The contour interval of a topographic map

answers: NDQ_001591

answers: deepest point

answers: NDQ_001592

answers: bathymetric map

answers: NDQ_001593

answers: The deepest point is marked with " "

answers: NDQ_001594

answers: The deepest point

answers: NDQ_001595

answers: 1000 feet

answers: NDQ_001597

answers: NDQ_001598

answers: The deepest point

answers: NDQ_001600

answers: NDQ_001603

answers: It's impossible to say

answers: NDQ_001605

answers: NDQ_001606

answers: the contour interval

answers: NDQ_001608

answers: The deepest point is marked with " "

answers: NDQ_001611

answers: The deepest point is marked with " "

answers: NDQ_001613

answers: The deepest point

answers: NDQ_001614

answers: The deepest point is marked with "

answers: NDQ_001618

answers: bathymetric map

answers: NDQ_001619

answers: bathymetric map

answers: NDQ_001620

answers: bathymetric

answers: NDQ_001621

answers: bathymetric map

answers: NDQ_001622

answers: bathymetric

answers: NDQ_001623

answers: NDQ_001624

answers: bathymetric map

answers: NDQ_001625

text: where R may be calculated from the width W of the map by R = . For example, on a map with R = 1 the values of y = 0, 1, 2, 3 correspond to latitudes of φ = 0°, 50°, 75°, 84° and therefore the successive intervals of 1 cm on the map correspond to latitude intervals on the globe of 50°, 25°, 9° and distances of 5,560 km, 2,780 km, and 1,000 km on the Earth.

text: where R may be calculated from the width W of the map by R = . For example, on a map with R = 1 the values of y = 0, 1, 2, 3 correspond to latitudes of φ = 0°, 50°, 75°, 84° and therefore the successive intervals of 1 cm on the map correspond to latitude intervals on the globe of 50°, 25°, 9° and distances of 5,560 km, 2,780 km, and 1,000 km on the Earth.

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answers: tqa2:L_0039/T_0394/887c3a67f14f037595ba29962136333b

answers: 0

answers: tqa2:L_0039/T_0394/6d728b60d5f64842627cebc2b23b865c

answers: 0

answers: tqa2:L_0039/T_0395/6aad7f1f8d291b5761a8b73d39008410

answers: 0

answers: tqa2:L_0039/T_0395/e4440cb133c19079cf1de06142182459

answers: 0

answers: tqa2:L_0039/T_0395/a1ad3c980328bce73604a21928ff7929

answers: 0

answers: tqa2:L_0039/T_0395/b3ed9fe004e17c5d260376b7dc97546c

answers: 0

answers: tqa2:L_0039/T_0395/617bb1adf869087f60ef513ffed01cc1

answers: 4

answers: tqa2:L_0039/T_0395/3a25e8f10326f778d0e4ce880cf48373

answers: 0

answers: tqa2:L_0039/T_0395/6e7058ba6ae907b02aadde87cadc8f56

answers: 0

answers: tqa2:L_0039/T_0395/3442c8987c1161ceca69ab5226dd316e

answers: 0

answers: tqa2:L_0039/T_0395/4c9d21d7c8934e2cf4b88c65d430fc09

answers: 0

answers: tqa2:L_0039/T_0395/e1278a8201ddf520d5b19846047bf656

answers: 0

answers: NDQ_001586

answers: 4

answers: NDQ_001587

answers: 0

answers: NDQ_001588

answers: 4

answers: NDQ_001589

answers: 0

answers: NDQ_001590

answers: 4

answers: NDQ_001591

answers: 0

answers: NDQ_001592

answers: 0

answers: NDQ_001593

answers: 4

answers: NDQ_001594

answers: 0

answers: NDQ_001595

answers: 0

answers: NDQ_001597

answers: 0

answers: NDQ_001598

answers: 0

answers: NDQ_001600

answers: 0

answers: NDQ_001603

answers: 0

answers: NDQ_001605

answers: 0

answers: NDQ_001606

answers: 4

answers: NDQ_001608

answers: 4

answers: NDQ_001611

answers: 0

answers: NDQ_001613

answers: 0

answers: NDQ_001614

answers: 0

answers: NDQ_001618

answers: 0

answers: NDQ_001619

answers: 0

answers: NDQ_001620

answers: 0

answers: NDQ_001621

answers: 0

answers: NDQ_001622

answers: 0

answers: NDQ_001623

answers: 0

answers: NDQ_001624

answers: 0

answers: NDQ_001625

answers: 1