text: The Amazonian Craton is a geologic province located in South America. It occupies a large portion of the central, north and eastern part of the continent. The Guiana Shield and Central Brazil Shield (Guaporé Shield) constitutes respectively the northern and southern exhumed parts of the craton. Between the two shields lies the Amazon Rift, a zone of weakness within the craton. Smaller cratons  of Precambrian rocks south of the Amazonian Shield are the Río de la Plata Craton and the São Francisco Craton, which lies to the east.

text: The Amazonian Craton is a

entity_name: Geologic province

text: geologic province

text: located in

entity_name: South America

text: South America

text: . It occupies a large portion of the central, north and eastern part of the continent. The

entity_name: Guiana Shield

text: Guiana Shield

text: and Central Brazil Shield (Guaporé Shield) constitutes respectively the northern and southern

entity_name: Exhumation (geology)

text: exhumed

text: parts of the craton. Between the two shields lies the

entity_name: Amazon Basin (sedimentary basin)

text: Amazon Rift

text: , a zone of weakness within the craton. Smaller cratons  of

entity_name: Precambrian

text: Precambrian

text: rocks south of the Amazonian Shield are the

entity_name: Río de la Plata Craton

text: Río de la Plata Craton

text: and the

entity_name: São Francisco Craton

text: São Francisco Craton

text: , which lies to the east.

method: UNH-tfidf-stem

method: UNH-tfidf-ptsim

method: UNH-tfidf-lem

method: UNH-qee

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answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Smaller cratons

answers: NDQ_005575

answers: the Amazonian Craton

answers: NDQ_005576

answers: Guiana Shield

answers: NDQ_005577

answers: Precambrian

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: The shield has remained relatively stable since its formation, over 3500 million years ago. It is delimited on the west, south and east by the present day coastline and Phanerozoic sediment cover. On the north, it is bounded by the Proterozoic Province. In the northeast, it is bounded by the Godavari graben preserving the Precambrian pakhal rocks and Gondwana sediments.The important components that make up the shield are:

text: The shield has remained relatively stable since its formation, over 3500 million years ago. It is delimited on the west, south and east by the present day coastline and

entity_name: Phanerozoic

text: Phanerozoic

text: sediment cover. On the north, it is bounded by the

entity_name: Proterozoic

text: Proterozoic

text: Province. In the northeast, it is bounded by the Godavari

entity_name: Graben

text: graben

text: preserving the

text: Precambrian

text: pakhal rocks and

entity_name: Gondwana

text: Gondwana

text: sediments.The important components that make up the shield are:

method: UNH-ecn

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: the shield has remained relatively stable

answers: NDQ_005574

answers: Godavari graben

answers: NDQ_005575

answers: 3500 million years ago

answers: NDQ_005576

answers: Godavari graben

answers: NDQ_005577

answers: Gondwana sediments

answers: NDQ_005579

answers: 3500 million years ago

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In the Directa, the Pope dealt with the fact that clerics (deacons, priests, and bishops) were still living with their wives and having children, thus contravening the Council of Elvira and the First Ecumenical Council. Priests were justifying this by referring to the traditions of the Levitical priesthood of the Old Testament. Siricius was emphatic that clerical continence belonged to immemorial, even apostolic, tradition. He declared that priests had been under a duty to observe temporary continence when serving in the Temple, but that the coming of Christ had brought the old priesthood to completion, and by this fact the duty of temporary continence had become an obligation to perpetual continence. Fifteen points are studied in the decretal, but the key passage is that

text: In the Directa, the Pope dealt with the fact that clerics (deacons, priests, and bishops) were still living with their wives and having children, thus contravening the

entity_name: Synod of Elvira

text: Council of Elvira

text: and the

entity_name: First Council of Nicaea

text: First Ecumenical Council

text: . Priests were justifying this by referring to the traditions of the

entity_name: Levite

text: Levitical priesthood

text: of the

entity_name: Old Testament

text: Old Testament

text: . Siricius was emphatic that clerical continence belonged to immemorial, even apostolic, tradition. He declared that priests had been under a duty to observe temporary continence when serving in

entity_name: Temple in Jerusalem

text: the Temple

text: , but that the

entity_name: Nativity of Jesus

text: coming of Christ

text: had brought the old priesthood to completion, and by this fact the duty of temporary continence had become an obligation to perpetual continence. Fifteen points are studied in the decretal, but the key passage is that

method: Bert-ConvKNRM

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text: Faculty and students continue to add significantly to the extensive paleobotanical collections, particularly Precambrian material containing early life forms.

entity_name: Faculty (division)

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answer: No

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text: Approximately 10,150,000 GM J platform cars were sold across eleven marques on six continents from 1982 through 1997, not counting Daewoo Espero sales. Consequently, it is the fifth best selling automobile platform in automotive history.

text: Approximately 10,150,000 GM J platform cars were sold across eleven marques on six continents from 1982 through 1997, not counting

entity_name: Daewoo Espero

text: Daewoo Espero

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answers: GM J

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answers: continents

answers: NDQ_005573

answers: 1982 through 1997

answers: NDQ_005574

answers: six continents

answers: NDQ_005575

answers: GM J platform cars

answers: NDQ_005576

answers: GM J platform

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: 1982 through 1997

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The craton is a composite of several different terranes of Archaean metasediments. The Dodoman is the oldest, and others include the Nyanzian and Kavirondian. Some of the greenstone belts are more than 3 billion years old. They were intruded by granites and migmatized in different events that date back to 2.9, 2.7, 2.4 and 1.85 billion years ago.The craton mainly consists of Archaean granitic complexes, but also includes rocks from the Dodoma System in the central area, and belts of greenstone to the south and east of Lake Victoria.Gneisses, schists, quartzites, migmatites, amphibolites and granulite are also found.There was widespread intrusion of kimberlites in the Cretaceous Period, mostly in the part of the craton that lies south of Lake Victoria.This includes the Mwadui kimberlite pipe in the center of Tanzania.

text: The craton is a composite of several different terranes of Archaean metasediments. The Dodoman is the oldest, and others include the Nyanzian and Kavirondian. Some of the greenstone belts are more than 3 billion years old. They were intruded by granites and

text: migmatized

text: in different events that date back to 2.9, 2.7, 2.4 and 1.85 billion years ago.The

text: craton

text: mainly consists of

text: Archaean

text: granitic

text: complexes, but also includes rocks from the Dodoma System in the central area, and belts of greenstone to the south and east of

text: Lake Victoria

text: .Gneisses, schists, quartzites, migmatites, amphibolites and granulite are also found.There was widespread intrusion of

text: kimberlite

text: s in the

text: Cretaceous

text: Period, mostly in the part of the craton that lies south of Lake Victoria.This includes the

text: Mwadui

text: kimberlite pipe in the center of Tanzania.

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answers: Archaean

answers: NDQ_005572

answers: Archaean

answers: NDQ_005573

answers: They were intruded by granites and migmatized

answers: NDQ_005574

answers: a composite of several different terranes of Archaean metasediments

answers: NDQ_005575

answers: 1.85 billion years ago

answers: NDQ_005576

answers: craton

answers: NDQ_005577

answers: Lake Victoria

answers: NDQ_005579

answers: Cretaceous Period

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The continent Euramerica (or Laurussia) was created in the early Devonian by the collision of Laurentia and Baltica, which rotated into the natural dry zone along the Tropic of Capricorn, which is formed as much in Paleozoic times as nowadays by the convergence of two great air-masses, the Hadley cell and the Ferrel cell. In these near-deserts, the Old Red Sandstone sedimentary beds formed, made red by the oxidized iron (hematite) characteristic of drought conditions.

text: The continent

text: Euramerica

text: (or Laurussia) was created in the early Devonian by the collision of

text: Laurentia

text: and

text: Baltica

text: , which rotated into the natural dry zone along the

text: Tropic of Capricorn

text: , which is formed as much in Paleozoic times as nowadays by the convergence of two great air-masses, the

text: Hadley cell

text: and the

text: Ferrel cell

text: . In these near-deserts, the

text: Old Red Sandstone

text: sedimentary beds formed, made red by the oxidized iron (

text: hematite

text: ) characteristic of drought conditions.

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answers: Paleozoic

answers: NDQ_005572

answers: the early Devonian

answers: NDQ_005573

answers: drought conditions

answers: NDQ_005574

answers: Laurentia and Baltica

answers: NDQ_005575

answers: Paleozoic times

answers: NDQ_005576

answers: sedimentary beds

answers: NDQ_005577

answers: hematite

answers: NDQ_005579

answers: Paleozoic times

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: It is a member of the Paediatric Continence Forum, which presses for improvements in paediatric continence care.

text: It is a member of the Paediatric Continence Forum, which presses for improvements in paediatric continence care.

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answers: NDQ_005571

answers: Continence

answers: NDQ_005572

answers: Paleogene

answers: NDQ_005573

answers: paediatric

answers: NDQ_005574

answers: Paediatric Continence Forum

answers: NDQ_005575

answers: paediatric continence care

answers: NDQ_005576

answers: Paediatric Continence Forum

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: when Earth's interior was warmer

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: The Precambrian metamorphic and igneous rocks of the Llano Uplift probably formed during the Mesoproterozoic Grenville orogeny, which was part of the assembly of the supercontinent Rodinia. Over time, the mountains of the Grenville orogeny were eroded flat, and later covered by Paleozoic and Mesozoic sediments that were not uplifted and eroded in their present manner  until the late Cenozoic.

text: The Precambrian metamorphic and igneous rocks of the

text: Llano Uplift

text: probably formed during the

text: Mesoproterozoic

text: Grenville orogeny

text: , which was part of the assembly of the

text: supercontinent

text: Rodinia

text: . Over time, the mountains of the Grenville orogeny were

text: eroded

text: flat, and later covered by Paleozoic and Mesozoic sediments that were not uplifted and eroded in their present manner  until the late

text: Cenozoic

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answers: NDQ_005571

answers: Mesoproterozoic

answers: NDQ_005572

answers: Rodinia

answers: NDQ_005573

answers: Grenville orogeny

answers: NDQ_005574

answers: Rodinia

answers: NDQ_005575

answers: Grenville orogeny

answers: NDQ_005576

answers: Grenville orogeny

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Mesoproterozoic

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: The Grouse Creek block is a block of 2.5 to 2.6 billion year old orthogneisses (a type of gneiss) and similar metasedimentary rocks. The Grouse Creek block is one of several Proterozoic and Archean accreted terranes that lie to the north and west of the Wyoming craton, including the Farmington Canyon Complex (<2.5 Ga), the Selway terrane (2.4-1.6 Ga), the Medicine Hat block (2.6-3.3 Ga) and the Priest River complex (>2.6-1.5 Ga).  Together, these terranes comprise part of the basement rock of the North American continent and have been critical to studies of crustal accretion in the Precambrian. Ongoing study of the Grouse Creek block will contribute to understanding the paleogeography of the Wyoming craton prior to its incorporation into the supercontinent Laurentia approximately 1.86 billion years ago. The name was proposed by David Foster and others.

text: The Grouse Creek block is a

text: block

text: of 2.5 to 2.6 billion year old orthogneisses (a type of

text: gneiss

text: ) and similar

text: metasediment

text: ary rocks. The Grouse Creek block is one of several

text: Proterozoic

text: and

text: Archean

text: accreted

text: terranes that lie to the north and west of the

text: Wyoming craton

text: , including the

text: Farmington Canyon Complex

text: Ga

text: ), the

text: Selway terrane

text: (2.4-1.6 Ga), the

text: Medicine Hat block

text: (2.6-3.3 Ga) and the

text: Priest River complex

text: (>2.6-1.5 Ga).  Together, these terranes comprise part of the

text: basement rock

text: of the North American continent and have been critical to studies of crustal accretion in the

text: Precambrian

text: . Ongoing study of the Grouse Creek block will contribute to understanding the

text: paleogeography

text: of the Wyoming craton prior to its incorporation into the

text: supercontinent

text: Laurentia

text: approximately 1.86 billion years ago. The name was proposed by David Foster and others.

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answers: gneiss

answers: NDQ_005572

answers: Wyoming craton

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answers: a type of gneiss

answers: NDQ_005574

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answers: NDQ_005575

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answers: NDQ_005576

answers: craton

answers: NDQ_005577

answers: Priest River complex

answers: NDQ_005579

answers: the Precambrian

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: The Nyanzian Supergroup rocks host the majority of known gold deposits in Tanzania and contain most of the greenstone belts found in the Tanzanian Craton. Granite rocks surrounding these greenstone belts are also known to host gold mineralisation and previous exploration and mining has been centred on these rocks. The Tanzanian Craton has many similarities to other globally-significant gold-producing cratons such as the Yilgarn Craton in Western Australia, the Kaapvaal and Zimbabwe Cratons in Southern Africa, and the Superior Craton of the Canadian Shield.

text: The Nyanzian Supergroup rocks host the majority of known gold deposits in Tanzania and contain most of the

text: greenstone

text: belts found in the

text: Tanzanian Craton

text: . Granite rocks surrounding these greenstone belts are also known to host gold

text: mineralisation

text: and previous exploration and mining has been centred on these rocks. The Tanzanian Craton has many similarities to other globally-significant gold-producing cratons such as the

text: Yilgarn Craton

text: in Western Australia, the

text: Kaapvaal

text: and

text: Zimbabwe Craton

text: s in Southern Africa, and the

text: Superior Craton

text: of the

text: Canadian Shield

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answers: Nyanzian

answers: NDQ_005572

answers: Nyanzian Supergroup

answers: NDQ_005573

answers: gold mineralisation

answers: NDQ_005574

answers: Tanzanian Craton

answers: NDQ_005575

answers: Canadian Shield

answers: NDQ_005576

answers: greenstone belts

answers: NDQ_005577

answers: The Tanzanian Craton

answers: NDQ_005579

answers: the Tanzanian Craton

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: In late Precambrian time, extension from a large tectonic plate or smaller plates moving away from Laurentia thinned its continental crust, forming large rift basins that would ultimately fail to split the continent. Eventually, this sunken region of Laurentia was flooded with a shallow seaway that extended from at least present-day Lake Superior to Glacier National Park in Montana to the Grand Canyon and the Uinta Mountains. The resulting Grand Canyon Supergroup of sedimentary units is composed of nine varied geologic formations that were laid down from 1.2 billion and 740 million years ago in this sea. Good exposures of the supergroup can be seen in eastern Grand Canyon in the Inner Gorge and from Desert View, Lipan Point and Moran point.

text: In late Precambrian time, extension from a large

text: tectonic plate

text: or smaller plates moving away from

text: Laurentia

text: thinned its

text: continental crust

text: , forming large

text: rift basin

text: s that would ultimately fail to split the continent. Eventually, this sunken region of Laurentia was flooded with a shallow seaway that extended from at least present-day

text: Lake Superior

text: to

text: Glacier National Park

text: in

text: Montana

text: to the Grand Canyon and the

text: Uinta Mountains

text: . The resulting Grand Canyon Supergroup of sedimentary units is composed of nine varied

text: geologic formation

text: s that were laid down from 1.2 billion and 740 million years ago in this sea. Good exposures of the supergroup can be seen in eastern Grand Canyon in the Inner Gorge and from Desert View, Lipan Point and Moran point.

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answers: sedimentary units

answers: NDQ_005572

answers: Laurentia

answers: NDQ_005573

answers: 1.2 billion and 740 million years ago

answers: NDQ_005574

answers: Laurentia

answers: NDQ_005575

answers: Laurentia

answers: NDQ_005576

answers: Grand Canyon Supergroup

answers: NDQ_005577

answers: this sunken region of Laurentia was flooded

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Some commuter rail stations, mostly newer stations and those in larger cities, do have full-length high-level platforms that allow for accessible boarding on all cars. (The standard MBTA high-level side platform is 12 feet wide and 800 feet long, capable of fully handling a 9-car train  – longer than any trainset currently in service. Some stations, including Forest Hills and Route 128, have Amtrak-style 1050-foot 12-car platforms.) The MBTA builds full-length high-level platforms at most new stations, and ultimately plans to build full-length high-level platforms at most stations except those requiring clearance for freight trains. Full-length platforms allow automatic power doors to be used, which allows passengers to board at all doors and thus speeding boarding times. High-level platforms are in place at all stations on the Greenbush Line, Plymouth/Kingston Line, and the Middleborough/Lakeville Line (all three of which have power doors in use), as well as all stations on the Fairmount Line except Fairmount and Readville. Other stations with full-length high-level platforms include:

text: Some commuter rail stations, mostly newer stations and those in larger cities, do have full-length high-level platforms that allow for accessible boarding on all cars. (The standard MBTA high-level side platform is 12 feet wide and 800 feet long, capable of fully handling a 9-car train  – longer than any trainset currently in service. Some stations, including

text: Forest Hills

text: and

text: Route 128

text: , have Amtrak-style 1050-foot 12-car platforms.) The MBTA builds full-length high-level platforms at most new stations, and ultimately plans to build full-length high-level platforms at most stations except those requiring clearance for freight trains. Full-length platforms allow automatic power doors to be used, which allows passengers to board at all doors and thus speeding boarding times. High-level platforms are in place at all stations on the

text: Greenbush Line

text: Plymouth/Kingston Line

text: , and the

text: Middleborough/Lakeville Line

text: (all three of which have power doors in use), as well as all stations on the

text: Fairmount Line

text: except

text: Fairmount

text: and

text: Readville

text: . Other stations with full-length high-level platforms include:

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answers: Forest Hills

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answers: Forest Hills and Route 128,

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answers: Forest Hills and Route 128,

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answers: Forest Hills and Route 128,

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answers: Forest Hills and Route 128,

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answers: Forest Hills and Route 128,

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answers: Forest Hills and Route 128,

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: The geological history of Europe traces back to the formation of the Baltic Shield (Fennoscandia) and the Sarmatian craton, both around 2.25 billion years ago, followed by the Volgo–Uralia shield, the three together leading to the East European craton (≈ Baltica) which became a part of the supercontinent Columbia. Around 1.1 billion years ago, Baltica and Arctica (as part of the Laurentia block) became joined to Rodinia, later resplitting around 550 million years ago to reform as Baltica. Around 440 million years ago Euramerica was formed from Baltica and Laurentia; a further joining with Gondwana then leading to the formation of Pangea. Around 190 million years ago, Gondwana and Laurasia split apart due to the widening of the Atlantic Ocean. Finally, and very soon afterwards, Laurasia itself split up again, into Laurentia (North America) and the Eurasian continent. The land connection between the two persisted for a considerable time, via Greenland, leading to interchange of animal species. From around 50 million years ago, rising and falling sea levels have determined the actual shape of Europe, and its connections with continents such as Asia. Europe's present shape dates to the late Tertiary period about five million years ago.

text: The geological history of Europe traces back to the formation of the

text: Baltic Shield

text: (Fennoscandia) and the

text: Sarmatian craton

text: , both around 2.25 billion years ago, followed by the

text: Volgo–Uralia

text: shield, the three together leading to the

text: East European craton

text: Baltica

text: ) which became a part of the

text: supercontinent

text: Columbia

text: . Around 1.1 billion years ago, Baltica and Arctica (as part of the

text: Laurentia

text: block) became joined to

text: Rodinia

text: , later resplitting around 550 million years ago to reform as Baltica. Around 440 million years ago

text: Euramerica

text: was formed from Baltica and Laurentia; a further joining with

text: Gondwana

text: then leading to the formation of

text: Pangea

text: . Around 190 million years ago, Gondwana and

text: Laurasia

text: split apart due to the widening of the Atlantic Ocean. Finally, and very soon afterwards, Laurasia itself split up again, into Laurentia (North America) and the Eurasian continent. The land connection between the two persisted for a considerable time, via

text: Greenland

text: , leading to interchange of animal species. From around 50 million years ago, rising and falling sea levels have determined the actual shape of Europe, and its connections with continents such as Asia. Europe's present shape dates to the late

text: Tertiary period

text: about five million years ago.

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answers: Sarmatian

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answers: the Volgo–Uralia shield

answers: NDQ_005573

answers: rising and falling sea levels

answers: NDQ_005574

answers: Sarmatian craton

answers: NDQ_005575

answers: 2.25 billion years ago

answers: NDQ_005576

answers: craton

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: around 2.25 billion years ago

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The geological basin, which is smaller than the drainage basin, is a Phanerozoic sedimentary basin formed during the plate divergence that opened the South Atlantic ocean. The basin lies between the West African Craton and Congo Craton, and formed around the same time as the Benue Trough. It covers an area of about . It merges into the Iullemmeden Basin to the west at the Damergou gap between the Aïr and Zinder massifs.The floor of the basin is made of Precambrian bedrock covered by more than  of sedimentary deposits.

text: The geological basin, which is smaller than the drainage basin, is a

text: Phanerozoic

text: sedimentary basin formed during the plate divergence that opened the South Atlantic ocean. The basin lies between the

text: West African Craton

text: and

text: Congo Craton

text: , and formed around the same time as the

text: Benue Trough

text: . It covers an area of about . It merges into the

text: Iullemmeden Basin

text: to the west at the Damergou gap between the

text: Aïr

text: and

text: Zinder

text: massifs.The floor of the basin is made of

text: Precambrian

text: bedrock covered by more than  of sedimentary deposits.

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answers: Precambrian

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answers: plate divergence

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answers: Precambrian

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answers: Congo Craton

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answers: more than

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answers: basin

answers: NDQ_005577

answers: sedimentary deposits

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answers: Phanerozoic

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: The older rocks of the terrane rest in the Precambrian with younger Cambrian rocks resting unconformably upon them. The Precambrian rocks are noted to be calc-alkaline plutonic intrusions dated to approximately 700-600Ma (Phase 1 to Phase 2 Neoproterozoic). These have associated (younger) volcanics that dominate the overlying sedimentary rocks that date between 570 and 560Ma. The signatures of the rocks are interpreted as having an intra-plate geochemical signature that may be attributed to arc-rifting. The diachronous formations of the bedded Uriconian and Coomb Volcanic Formation.

text: The older rocks of the terrane rest in the

text: Precambrian

text: with younger

text: Cambrian

text: rocks resting unconformably upon them. The Precambrian rocks are noted to be calc-alkaline plutonic intrusions dated to approximately 700-600Ma (Phase 1 to Phase 2

text: Neoproterozoic

text: ). These have associated (younger) volcanics that dominate the overlying sedimentary rocks that date between 570 and 560Ma. The signatures of the rocks are interpreted as having an intra-plate geochemical signature that may be attributed to arc-rifting. The diachronous formations of the bedded

text: Uriconian

text: and

text: Coomb Volcanic Formation

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: arc-rifting

answers: NDQ_005574

answers: arc-rifting

answers: NDQ_005575

answers: 700-600Ma

answers: NDQ_005576

answers: terrane

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: The lake sits atop the dividing line between the Precambrian granite Canadian Shield to the north, and the Paleozoic and Ordovician limestone to the south.Granite outcroppings can be seen beginning at the midpoint of the lake, including a small island in the north end of the lake with a cottage built upon it. On the south-east end, the limestone cuesta, which marks the boundary of the limestone and granite north of the lake, rises as a sheer cliff face several metres out of the water, following the length of the river southwest through Coboconk.

text: The lake sits atop the dividing line between the Precambrian granite

text: Canadian Shield

text: to the north, and the

text: Paleozoic

text: and Ordovician limestone to the south.Granite outcroppings can be seen beginning at the midpoint of the lake, including a small island in the north end of the lake with a cottage built upon it. On the south-east end, the limestone

text: cuesta

text: , which marks the boundary of the limestone and granite north of the lake, rises as a sheer cliff face several metres out of the water, following the length of the river southwest through Coboconk.

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Canadian Shield

answers: NDQ_005575

answers: Canadian Shield

answers: NDQ_005576

answers: limestone

answers: NDQ_005577

answers: lake

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: A high pressure system over the central United States drifted east and added a westward component to Gordon's southward motion, pulling the storm southwest towards Florida. The persistent shear and a continued lack of deep convection eventually reduced the storm's winds to below tropical storm force, and on the morning on November 20 Gordon became a tropical depression. The high pressure system over the continent continued pulling the depression towards the west until it made its final landfall near Cape Canaveral that night with winds of 30 mph (45 km/h). Between its three Floridian landfalls, Hurricane Gordon dumped 5–10 in (13–25 cm) of rain on Florida, with a station at Cooperstown recording 16.1 in (40.9 cm). The storm moved northward across Florida, northeastward across Georgia, and finally merged with a frontal system over South Carolina.

text: A high pressure system over the central United States drifted east and added a westward component to Gordon's southward motion, pulling the storm southwest towards Florida. The persistent shear and a continued lack of deep convection eventually reduced the storm's winds to below tropical storm force, and on the morning on November 20 Gordon became a tropical depression. The high pressure system over the continent continued pulling the depression towards the west until it made its final landfall near

text: Cape Canaveral

text: that night with winds of 30 mph (45 km/h). Between its three Floridian landfalls, Hurricane Gordon dumped 5–10 in (13–25 cm) of rain on Florida, with a station at

text: Cooperstown

text: recording 16.1 in (40.9 cm). The storm moved northward across Florida, northeastward across

text: Georgia

text: , and finally merged with a frontal system over South Carolina.

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text: In the early 1980s Luigi Faccia and Flavio Contin left Liga Veneta, the mainstream regionalist party in Veneto, because the considered it too moderate. On 25 January 1987 Faccia and Contin launched the VSG. In 1992 the group was joined by Fausto Faccia, brother of Luigi, and, later, by Bepin Segato, who was appointed "ambassador" of the VSG. Since 1996 the group is protagonist of raids into the frequencies of RAI, the Italian state owned public service broadcaster, in Veneto with separatist proclamations in Venetian language.

text: In the early 1980s

text: Luigi Faccia

text: and

text: Flavio Contin

text: left

text: Liga Veneta

text: , the mainstream regionalist party in Veneto, because the considered it too moderate. On 25 January 1987 Faccia and Contin launched the VSG. In 1992 the group was joined by

text: Fausto Faccia

text: , brother of Luigi, and, later, by

text: Bepin Segato

text: , who was appointed "ambassador" of the VSG. Since 1996 the group is protagonist of raids into the frequencies of

text: RAI

text: , the Italian state owned

text: public service

text: broadcaster

text: , in Veneto with separatist proclamations in

text: Venetian language

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text: The Onverwacht Group or Onverwacht Series is a series of greenstone belts and volcanic rock formations from the Archean Eon in the Kaapvaal Craton in South Africa and Swaziland.

text: The Onverwacht Group or Onverwacht Series is a series of

text: greenstone belt

text: s and

text: volcanic rock

text: formations from the

text: Archean

text: Eon in the

text: Kaapvaal Craton

text: in

text: South Africa

text: and

text: Swaziland

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answers: Archean Eon

answers: NDQ_005576

answers: Onverwacht Group

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Archean Eon

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: The next oldest possible animal fossils are found towards the end of the Precambrian, around 610 million years ago, and are known as the Ediacaran or Vendian biota. These are difficult to relate to later fossils, however. Some may represent precursors of modern phyla, but they may be separate groups, and it is possible they are not really animals at all.

text: The next oldest possible animal fossils are found towards the end of the

text: Precambrian

text: , around 610 million years ago, and are known as the

text: Ediacaran or Vendian biota

text: . These are difficult to relate to later fossils, however. Some may represent precursors of modern phyla, but they may be separate groups, and it is possible they are not really animals at all.

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answers: Precambrian

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answers: the Precambrian

answers: NDQ_005573

answers: 610 million years ago

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answers: Precambrian

answers: NDQ_005575

answers: 610 million years ago

answers: NDQ_005576

answers: Grand Canyon

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: around 610 million years ago

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Phytoplankton absorb energy from the Sun and nutrients from the water to produce their own food. In the process of photosynthesis, phytoplankton release molecular oxygen () into the water. It is estimated that between 50% — 85% of the world's oxygen is produced via phytoplankton photosynthesis. The rest is produced via photosynthesis on land by plants. Furthermore, phytoplankton photosynthesis has controlled the atmospheric / balance since the early Precambrian Eon.

text: Phytoplankton

text: absorb energy from the Sun and nutrients from the water to produce their own food. In the process of photosynthesis, phytoplankton release molecular

text: oxygen

text: () into the water. It is estimated that between 50% — 85% of the world's oxygen is produced via phytoplankton photosynthesis. The rest is produced via photosynthesis on land by

text: plant

text: s. Furthermore, phytoplankton photosynthesis has controlled the atmospheric / balance since the early

text: Precambrian

text: Eon.

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian Eon

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: phytoplankton

answers: NDQ_005575

answers: phytoplankton

answers: NDQ_005576

answers: phytoplankton

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: The West African Craton underlies the modern countries of Morocco, Algeria, Mauritania, Senegal, The Gambia, Guinea Bissau, Guinea, Mali, Burkina Faso, Sierra Leone, Liberia, Ivory Coast, Ghana, Togo and Benin.

text: The West African Craton underlies the modern countries of

text: Morocco

text: Algeria

text: Mauritania

text: Senegal

text: The Gambia

text: Guinea Bissau

text: Guinea

text: Mali

text: Burkina Faso

text: Sierra Leone

text: Liberia

text: Ivory Coast

text: Ghana

text: Togo

text: and

text: Benin

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answers: West African Craton

answers: NDQ_005572

answers: West African Craton

answers: NDQ_005573

answers: modern

answers: NDQ_005574

answers: West African Craton

answers: NDQ_005575

answers: West African Craton

answers: NDQ_005576

answers: West African Craton

answers: NDQ_005577

answers: Zircons are a type of mineral

answers: NDQ_005579

answers: Craton

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Roughly 3 million years ago (Ma), the volcanic Isthmus of Panama formed between the North and South American continents creating a bridge over what was the Central American Seaway and allowing the migration of flora and fauna between the two landmasses in the Great American Interchange. Starting 2.58 Ma, the Quaternary glaciation covered much of the continent with ice, centered west of Hudson Bay, the floor of which is slowly rebounding after being depressed by the great weight of the ice. Glaciers descended the slopes of the Rocky Mountains and those of the Pacific Margin. Extensive glacial lakes, such as Glacial Lake Missoula, Bonneville, Lahontan, Agassiz, and Algonquin, formed by glacial melt water. "Remnants of them are still visible in the Great Basin and along the edge of the Canadian Shield in the form of the Great Salt Lake, the Great Lakes, and the large lakes of west central Canada." The last glacial period of the current ice age caused a lowering of the sea level, exposing the Bering Land Bridge between Alaska and Siberia, which resulted in human migration from Asia to the Americas between 40,000 and 15,000 years ago.

text: Roughly 3 million years ago (

text: Ma

text: ), the

text: volcanic

text: Isthmus of Panama

text: formed between the North and

text: South American

text: continents creating a bridge over what was the

text: Central American Seaway

text: and allowing the migration of flora and fauna between the two landmasses in the

text: Great American Interchange

text: . Starting 2.58 Ma, the

text: Quaternary glaciation

text: covered much of the continent with ice, centered west of Hudson Bay, the floor of which is slowly rebounding after being depressed by the great weight of the ice. Glaciers descended the slopes of the Rocky Mountains and those of the

text: Pacific Margin

text: . Extensive glacial lakes, such as

text: Glacial Lake Missoula

text: Bonneville

text: Lahontan

text: Agassiz

text: , and

text: Algonquin

text: , formed by glacial melt water. "Remnants of them are still visible in the

text: Great Basin

text: and along the edge of the Canadian Shield in the form of the

text: Great Salt Lake

text: , the

text: Great Lakes

text: , and the large lakes of west central Canada." The

text: last glacial period

text: of the current ice age caused a lowering of the sea level, exposing the

text: Bering Land Bridge

text: between Alaska and

text: Siberia

text: , which resulted in

text: human migration from Asia to the Americas

text: between 40,000 and 15,000 years ago.

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answers: volcanic

answers: NDQ_005572

answers: volcanic Isthmus of Panama

answers: NDQ_005573

answers: volcanoes

answers: NDQ_005574

answers: Rocky Mountains

answers: NDQ_005575

answers: 3 million years ago

answers: NDQ_005576

answers: Isthmus

answers: NDQ_005577

answers: The presence of zircons in ancient rocks indicates that there was water in the environment

answers: NDQ_005579

answers: 3 million years ago

answer: No

answer: No

answer: Yes

answer: No

answer: Yes

answer: 1

text: The complete lack of fossils is consistent with a Precambrian age for the sequence. This is also shown by the age of the earliest known intrusions that cut the sequence, dated at around 870 Ma. There is also no evidence of the sequence being affected by the 1300-1000 Ma Grenville orogeny. This together suggests an early Neoproterozoic sedimentation age. A possible correlation with the lithologically similar Torridon Group, an unmetamorphosed sequence of similar age found beneath the Moine Thrust, remains unproven.

text: The complete lack of fossils is consistent with a Precambrian age for the sequence. This is also shown by the age of the earliest known

text: intrusion

text: s that cut the sequence, dated at around 870 Ma. There is also no evidence of the sequence being affected by the 1300-1000 Ma

text: Grenville orogeny

text: . This together suggests an early

text: Neoproterozoic

text: sedimentation age. A possible correlation with the lithologically similar

text: Torridon Group

text: , an unmetamorphosed sequence of similar age found beneath the Moine Thrust, remains unproven.

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answers: Precambrian

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answers: Precambrian

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answers: Moine Thrust

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answers: 870 Ma

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answers: Zircons indicate that there was water in the environment

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answer: No

answer: No

answer: No

answer: No

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answer: 1

text: Diamond-bearing rock is carried from the mantle to the Earth's surface by deep-origin volcanic eruptions. The magma for such a volcano must originate at a depth where diamonds can be formed— or more (three times or more the depth of source magma for most volcanoes). This is a relatively rare occurrence. These typically small surface volcanic craters extend downward in formations known as volcanic pipes. The pipes contain material that was transported toward the surface by volcanic action, but was not ejected before the volcanic activity ceased. During eruption these pipes are open to the surface, resulting in open circulation; many xenoliths of surface rock and even wood and fossils are found in volcanic pipes. Diamond-bearing volcanic pipes are closely related to the oldest, coolest regions of continental crust (cratons). This is because cratons are very thick, and their lithospheric mantle extends to great enough depth that diamonds are stable. Not all pipes contain diamonds, and even fewer contain enough diamonds to make mining economically viable.

text: Diamond-bearing rock is carried from the mantle to the Earth's surface by deep-origin volcanic eruptions. The magma for such a volcano must originate at a depth where diamonds can be formed— or more (three times or more the depth of source magma for most volcanoes). This is a relatively rare occurrence. These typically small surface volcanic craters extend downward in formations known as

text: volcanic pipe

text: s. The pipes contain material that was transported toward the surface by volcanic action, but was not ejected before the volcanic activity ceased. During eruption these pipes are open to the surface, resulting in open circulation; many

text: xenolith

text: s of surface rock and even wood and fossils are found in volcanic pipes. Diamond-bearing volcanic pipes are closely related to the oldest, coolest regions of

text: continental crust

text: (cratons). This is because cratons are very thick, and their lithospheric mantle extends to great enough depth that diamonds are stable. Not all pipes contain diamonds, and even fewer contain enough diamonds to make mining economically viable.

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answers: NDQ_005571

answers: mantle

answers: NDQ_005572

answers: cratons

answers: NDQ_005573

answers: diamonds are stable

answers: NDQ_005574

answers: The oldest, coolest regions of continental crust

answers: NDQ_005575

answers: cratons

answers: NDQ_005576

answers: volcanic pipes

answers: NDQ_005577

answers: Diamond-bearing rock

answers: NDQ_005579

answers: Diamond-bearing volcanic pipes

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A poorly organized area of convection persisted about  off the southern coast of Guatemala on September 9. It moved west-northwestward, and after three days without further organization a circulation developed off the southwest coast of Mexico. The system quickly organized, resulting in Dvorak classifications beginning later that day. Convective banding became better organized, and late on September 12 it developed into Tropical Depression Ten while located about  south-southwest of Manzanillo, Colima. The depression moved to the northwest, and following an increase in deep convection it intensified into Tropical Storm Ismael early on September 13.Upon attaining tropical storm status, Ismael was located in an area of warm water temperatures with well-established upper-level outflow. Initially the storm moved to the northwest, though in response to the interaction with an upper-level low over Baja California Ismael gradually turned to the north. Such a change in motion was not operationally predicted by forecasters, though they noted uncertainty in Ismael's track due to the low. Ismael steadily strengthened as it moved northward, though it failed to organize significantly; early on September 14 the center remained poorly defined despite winds of . However, the outflow remained well-organized as it remained over warm waters. Ismael became better organized, and later on September 14 it intensified into a hurricane while located 210 miles (340 km) west-southwest of Puerto Vallarta.

text: A poorly organized area of convection persisted about  off the southern coast of

text: Guatemala

text: on September 9. It moved west-northwestward, and after three days without further organization a circulation developed off the southwest coast of

text: Mexico

text: . The system quickly organized, resulting in

text: Dvorak classifications

text: beginning later that day. Convective

text: banding

text: became better organized, and late on September 12 it developed into Tropical Depression Ten while located about  south-southwest of

text: Manzanillo, Colima

text: . The depression moved to the northwest, and following an increase in deep convection it intensified into Tropical Storm Ismael early on September 13.Upon attaining tropical storm status, Ismael was located in an area of warm water temperatures with well-established

text: upper-level outflow

text: . Initially the storm moved to the northwest, though in response to the interaction with an upper-level low over

text: Baja California

text: Ismael gradually turned to the north. Such a change in motion was not operationally predicted by forecasters, though they noted uncertainty in Ismael's track due to the low. Ismael steadily strengthened as it moved northward, though it failed to organize significantly; early on September 14 the center remained poorly defined despite winds of . However, the outflow remained well-organized as it remained over warm waters. Ismael became better organized, and later on September 14 it intensified into a hurricane while located 210 miles (340 km) west-southwest of

text: Puerto Vallarta

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answers: igneous

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answers: southwest coast of Mexico

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answers: Tropical Depression Ten

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answers: Tropical Depression Ten

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answers: Tropical Depression Ten

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: East Antarctica is geologically very old, dating from the Precambrian, with some rocks formed more than 3 billion years ago. It is composed of a metamorphic and igneous platform which is the basis of the continental shield. On top of this base are various more modern rocks, such as sandstones, limestones, coal and shales laid down during the Devonian and Jurassic periods to form the Transantarctic Mountains. In coastal areas such as Shackleton Range and Victoria Land some faulting has occurred.

text: East Antarctica is geologically very old, dating from the

text: Precambrian

text: , with some rocks formed more than 3 billion years ago. It is composed of a

text: metamorphic

text: and

text: igneous

text: platform which is the basis of the

text: continental shield

text: . On top of this base are various more modern rocks, such as

text: sandstone

text: s,

text: limestone

text: s, coal and

text: shale

text: s laid down during the Devonian and Jurassic periods to form the

text: Transantarctic Mountains

text: . In coastal areas such as

text: Shackleton Range

text: and

text: Victoria Land

text: some

text: faulting

text: has occurred.

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answers: Precambrian

answers: NDQ_005572

answers: Devonian

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answers: Devonian

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answers: Transantarctic Mountains

answers: NDQ_005575

answers: continental shield

answers: NDQ_005576

answers: continental shield

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Evidence of the details of plate motions and other tectonic activity in the Precambrian has been poorly preserved. It is generally believed that small proto-continents existed prior to 3000 Ma, and that most of the Earth's landmasses collected into a single supercontinent around 1000 Ma. The supercontinent, known as Rodinia, broke up around 600 Ma. A number of glacial periods have been identified going as far back as the Huronian epoch, roughly 2200 Ma. One of the best studied is the Sturtian-Varangian glaciation, around 600 Ma, which may have brought glacial conditions all the way to the equator, resulting in a "Snowball Earth".

text: Evidence of the details of

text: plate motions

text: and other

text: tectonic

text: activity in the Precambrian has been poorly preserved. It is generally believed that small proto-continents existed prior to 3000 Ma, and that most of the Earth's landmasses collected into a single

text: supercontinent

text: around 1000 Ma. The supercontinent, known as

text: Rodinia

text: , broke up around 600 Ma. A number of

text: glacial periods

text: have been identified going as far back as the

text: Huronian

text: epoch, roughly 2200 Ma. One of the best studied is the

text: Sturtian-Varangian

text: glaciation, around 600 Ma, which may have brought glacial conditions all the way to the equator, resulting in a "

text: Snowball Earth

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answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Rodinia

answers: NDQ_005573

answers: tectonic activity

answers: NDQ_005574

answers: plate motions

answers: NDQ_005575

answers: 3000 Ma

answers: NDQ_005576

answers: Grand Canyon

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The North China Craton is composed of several major blocks that have been heavily tilted and folded over time as a result of collisions with other continental land masses. The main blocks include the Eastern Block, the Western Block and the Central Orogenic Belt. The Central Orogenic Belt runs from western Liaoning through Beijing municipality to western Henan and contains chiefly igneous rocks of Paleoproterozoic age. The Western Block extends west from this region through Shanxi, Shaanxi, Inner Mongolia and northern Gansu. This block is the oldest and most stable part of the Craton and contains some of the oldest and mineralogically most valuable rocks in Asia, especially in Inner Mongolia where huge deposits of coal and iron ore are found.

text: The North China Craton is composed of several major blocks that have been heavily tilted and

text: folded

text: over time as a result of collisions with other

text: continent

text: al land masses. The main blocks include the Eastern Block, the Western Block and the Central Orogenic Belt. The Central Orogenic Belt runs from western

text: Liaoning

text: through

text: Beijing

entity_name: Direct-controlled municipalities of China

text: municipality

text: to western

text: Henan

text: and contains chiefly

text: igneous rock

text: s of

text: Paleoproterozoic

text: age. The Western Block extends west from this region through

text: Shanxi

text: Shaanxi

text: Inner Mongolia

text: and northern

text: Gansu

text: . This block is the oldest and most stable part of the Craton and contains some of the oldest and mineralogically most valuable rocks in

text: Asia

text: , especially in Inner Mongolia where huge deposits of

text: coal

text: and

text: iron ore

text: are found.

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answers: Paleoproterozoic age

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Floating bridge/Pontoon Bridge construction has a long history in military and civilian applications on every continent except Antarctica. According to the engineers who designed this bridge, it was designed using recent American technology for floating bridges, combined with Norwegian technology for offshore platforms. The bridge designers researched other bridges in the world and traveled to the state of Washington in the United States to visit the Homer M. Hadley Memorial Bridge and the Hood Canal Bridge—two floating bridges. The continuous floating concrete structure used in the Washington bridges was ultimately ruled out in favor of the discrete floating concrete pier design. This design afforded: 1) an elevated roadway that reduced traffic hazards in storms, 2) a reduction in corrosion of the bridge deck, and 3) improved passage of water beneath the bridge thereby supporting native species.

text: Floating bridge/

text: Pontoon Bridge

text: construction has a long history in military and civilian applications on every continent except

text: Antarctica

text: . According to the engineers who designed this bridge, it was designed using recent American technology for floating bridges, combined with Norwegian technology for

text: offshore platform

text: s. The bridge designers researched other bridges in the world and traveled to the state of

text: Washington

text: in the

text: United States

text: to visit the

text: Homer M. Hadley Memorial Bridge

text: and the

text: Hood Canal Bridge

text: —two floating bridges. The continuous floating

text: concrete

text: structure used in the Washington bridges was ultimately ruled out in favor of the discrete floating concrete pier design. This design afforded: 1) an elevated roadway that reduced traffic hazards in storms, 2) a reduction in

text: corrosion

text: of the

text: bridge deck

text: , and 3) improved passage of water beneath the bridge thereby supporting native species.

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answers: NDQ_005571

answers: sedimentary

answers: NDQ_005572

answers: Antarctica

answers: NDQ_005573

answers: greenstones in cratons

answers: NDQ_005574

answers: Antarctica

answers: NDQ_005575

answers: Antarctica

answers: NDQ_005576

answers: floating bridge/Pontoon Bridge

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Antarctica

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Around 750 million years ago Rodinia rifted apart into three continents: Proto-Laurasia, the Congo craton and Proto-Gondwana. The West African Craton may then have combined with other cratons to form Pannotia, a hypothetical supercontinent that existed from the Pan-African orogeny about 600 million years ago to the end of the Precambrian about 540 million years ago. Later it became part of Gondwana, and later still part of Pangaea, the supercontinent that existed during the Paleozoic and Mesozoic eras about 250 million years ago, before North and South America separated from Eurasia and Africa and the continents started to drift towards their current configuration.

text: Around 750 million years ago Rodinia

text: rifted

text: apart into three continents:

text: Proto-Laurasia

text: , the

text: Congo craton

text: and

text: Proto-Gondwana

text: . The West African Craton may then have combined with other cratons to form

text: Pannotia

text: , a hypothetical

text: supercontinent

text: that existed from the

text: Pan-African orogeny

text: about 600 million years ago to the end of the

text: Precambrian

text: about 540 million years ago. Later it became part of

text: Gondwana

text: , and later still part of

text: Pangaea

text: , the

text: supercontinent

text: that existed during the

text: Paleozoic

text: and

text: Mesozoic

text: eras about 250 million years ago, before North and South America separated from Eurasia and Africa and the continents started to drift towards their current configuration.

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text: John Douglas Craton is an American classical composer. His works have been performed throughout the United States, Europe, and Japan. While his compositions cover a diverse range, he is best known for his operas, ballets, and works for classical mandolin.

text: John Douglas Craton is an American

entity_name: List of classical music composers by era

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text: As part of the Canada Carries On series, Wings of a Continent was produced in 35 mm for the theatrical market and also released as Les Ailes d'un Continent, a version dubbed in French. Each film was shown over a six-month period as part of the shorts or newsreel segments in approximately 800 theatres across Canada. When shown in Ottawa, the reviewer commented that, "The strategic significance of air transportation in Canada in a world now totally at war is graphically described in the December release of the National Film Board's 'Wings of a Continent'." Along with others in the Canada Carries On series, Wings of a Continent received widespread circulation.

text: As part of the Canada Carries On series, Wings of a Continent was produced in 35 mm for the theatrical market and also released as Les Ailes d'un Continent, a version dubbed in French. Each film was shown over a six-month period as part of the shorts or newsreel segments in approximately 800 theatres across Canada. When shown in Ottawa, the reviewer commented that, "The strategic significance of air transportation in Canada in a world now totally at war is graphically described in the December release of the National Film Board's 'Wings of a Continent'." Along with others in the Canada Carries On series, Wings of a Continent received widespread circulation.

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text: However, in October 1947, the now-revived paper was named The Shield. This name lasted until 1966. The Shield was named after the founder, Bishop Bernard J. Schiel. The school paper shortened its name to Shield in 1966, and published the paper in a magazine format.

text: However, in October 1947, the now-revived paper was named The Shield. This name lasted until 1966. The Shield was named after the founder, Bishop Bernard J. Schiel. The school paper shortened its name to Shield in 1966, and published the paper in a magazine format.

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text: Joyous Celebration is a South African Gospel choir which was formed in 1994 following the success of South Africa's first democratic elections. What was merely meant to be a one-time studio project by South African musicians turned into a massive platform for upcoming South African artists. The choir has enjoyed success in South Africa and the rest of the African continent, having released 20 albums as of 2016. It is one of South Africa's  most successful gospel choirs, following acts like The Soweto Gospel Choir.

text: Joyous Celebration is a

text: South African

text: Gospel choir which was formed in 1994 following the success of South Africa's first democratic elections. What was merely meant to be a one-time studio project by South African musicians turned into a massive platform for upcoming South African artists. The choir has enjoyed success in South Africa and the rest of the African continent, having released 20 albums as of 2016. It is one of South Africa's  most successful gospel choirs, following acts like The

text: Soweto Gospel Choir

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text: By late on May 29, a weak trough over the Yucatán Peninsula produced a small area of convection over the Yucatán Channel. Convection increased in association with the trough, and the next day a broad envelop of cyclonic turning developed within the system. By May 30, the moisture from the trough extended from Nicaragua through the southeastern Gulf of Mexico, with the greatest area of convection near Cuba. A westward moving tropical wave spawned a broad area of low pressure on May 30, and by May 31 a circulation developed within the system to the southeast of Cozumel, Mexico. The low moved north-northeastward, and gradually became better organized despite high amounts of vertical wind shear. The deep convection became more concentrated near the center, and it is estimated the system developed into a tropical depression at 1200 UTC on June 1 just to the northwest of the western tip of Cuba. Operationally, it was not classified until eleven hours later.

text: By late on May 29, a weak

text: trough

text: over the

text: Yucatán Peninsula

text: produced a small area of

text: convection

text: over the

text: Yucatán Channel

text: . Convection increased in association with the trough, and the next day a broad envelop of cyclonic turning developed within the system. By May 30, the moisture from the trough extended from

text: Nicaragua

text: through the southeastern

text: Gulf of Mexico

text: , with the greatest area of convection near

text: Cuba

text: . A westward moving

text: tropical wave

text: spawned a broad area of low pressure on May 30, and by May 31 a circulation developed within the system to the southeast of

text: Cozumel

text: , Mexico. The low moved north-northeastward, and gradually became better organized despite high amounts of vertical

text: wind shear

text: . The deep convection became more concentrated near the center, and it is estimated the system developed into a tropical depression at 1200

text: UTC

text: on June 1 just to the northwest of the western tip of

text: Cuba

text: . Operationally, it was not classified until eleven hours later.

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answers: Yucatán Peninsula

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answers: The presence of zircons in ancient rocks indicates that there was water in the environment

answers: NDQ_005579

answers: May 29

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The basement consists of Precambrian rocks of the Arabian-Nubian Shield.  Gneisses, volcanics and metasediments are intruded by granites, granodiorites and a suite of dolerite dykes. These rocks contain shear zones, such as the Rehba Shear Zone of western Sinai, that are interpreted to have partly controlled the orientation and location of rift structures.

text: The basement consists of Precambrian rocks of the

text: Arabian-Nubian Shield

text: Gneiss

text: es, volcanics and

text: metasediment

text: s are intruded by

text: granite

text: s,

text: granodiorite

text: s and a suite of

text: dolerite

text: dykes

text: . These rocks contain shear zones, such as the Rehba Shear Zone of western Sinai, that are interpreted to have partly controlled the orientation and location of rift structures.

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answers: Precambrian

answers: NDQ_005572

answers: Arabian-Nubian Shield

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Gneisses

answers: NDQ_005575

answers: rocks

answers: NDQ_005576

answers: basement

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: The movement of Earth's plates has caused the formation and break-up of continents over time, including occasional formation of a super-continent containing most or all of the landmass. The earliest known super-continent was Vaalbara. It formed from proto-continents and was a super-continent 3.1 billion years ago. Vaalbara broke up c. 2.8 Ga ago. The super-continent Kenorland was formed c. 2.7 Ga ago and then broke sometime after 2.5 Ga into the proto-continent cratons called Laurentia, Baltica, Australia, and Kalahari. The super-continent Columbia or Nuna formed 2.0–1.8 billion years ago and broke up about 1.5–1.3 billion years ago. The super-continent Rodinia is thought to have formed about 1 billion years ago, to have embodied most or all of Earth's continents and to have broken up into eight continents around 600 million years ago.

text: The movement of Earth's

text: plates

text: has caused the formation and break-up of continents over time, including occasional formation of a super-continent containing most or all of the landmass. The earliest known super-continent was

text: Vaalbara

text: . It formed from proto-continents and was a super-continent 3.1 billion years ago.

text: Vaalbara

text: broke up c. 2.8

text: Ga

text: ago. The super-continent

text: Kenorland

text: was formed c. 2.7

text: Ga

text: ago and then broke sometime after 2.5

text: Ga

text: into the proto-continent

text: craton

text: s called

text: Laurentia

text: Baltica

text: Australia

text: , and

text: Kalahari

text: . The super-continent

text: Columbia

text: or Nuna formed 2.0–1.8 billion years ago and broke up about 1.5–1.3 billion years ago. The super-continent

text: Rodinia

text: is thought to have formed about 1 billion years ago, to have embodied most or all of Earth's continents and to have broken up into eight continents around 600 million years ago.

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answers: proto-continent

answers: NDQ_005574

answers: proto-continent

answers: NDQ_005575

answers: 600 million years ago

answers: NDQ_005576

answers: super-continent

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: 3.1 billion years ago

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: The 2009 Four Continents Figure Skating Championships was the Four Continents Figure Skating Championships for the 2008–09 season. Skaters competed in the disciplines of men's singles, ladies' singles, pair skating, and ice dancing. The competition was open to skaters from a non-European Member nation of the International Skating Union. The four continents of the event's name refer to the Americas, Asia, Africa, and Oceania, which are four of the continents represented in the Olympic rings, omitting Europe.

text: The 2009 Four Continents Figure Skating Championships was the

entity_name: Four Continents Figure Skating Championships

text: Four Continents Figure Skating Championships

text: for the

text: 2008–09 season

text: . Skaters competed in the disciplines of

text: men's singles, ladies' singles

text: pair skating

text: , and

text: ice dancing

text: . The competition was open to skaters from a non-European

text: Member nation

text: of the

text: International Skating Union

text: . The four continents of the event's name refer to the

text: Americas

text: Asia

text: Africa

text: , and

text: Oceania

text: , which are four of the continents represented in the

text: Olympic rings

text: , omitting Europe.

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answers: the Americas, Asia, Africa, and Oceania

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answer: No

answer: No

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text: At the Berlin Conference of 1885, the scope of the Principle of Effective Occupation was heavily contested between Germany and France. The Germans, who were new to the continent of Africa, believed that as far as the extension of power in Africa was concerned, no colonial power should have any legal right to a territory, unless the state exercised strong and effective political control. Since Germany was a latecomer to the continent and was unlikely to gain any possessions, it had an interest in embarrassing the other European powers on the continent and forcing them to give up their possessions if they could not muster a strong political presence. On the other side, the United Kingdom (UK) had large territorial "possessions" on the continent and wanted to keep them while minimising its responsibilities and administrative costs. In the end, the British view prevailed.

text: At the Berlin Conference of 1885, the scope of the Principle of Effective Occupation was heavily contested between Germany and France. The Germans, who were new to the continent of Africa, believed that as far as the extension of power in Africa was concerned, no colonial power should have any legal right to a territory, unless the state exercised strong and effective political control. Since Germany was a latecomer to the continent and was unlikely to gain any possessions, it had an interest in embarrassing the other European powers on the continent and forcing them to give up their possessions if they could not muster a strong political presence. On the other side, the United Kingdom (UK) had large territorial "possessions" on the continent and wanted to keep them while minimising its responsibilities and administrative costs. In the end, the British view prevailed.

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answers: a strong political presence

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answers: the Berlin Conference of 1885

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text: however, strong wind shear caused all the deep convection to become displaced to the south of the center. At 1800 UTC, wind shear began to decrease, and the cyclone developed a well-defined circulation. Based on this, the JTWC upgraded the system into Tropical Storm Hal.

text: however, strong

text: wind shear

text: caused all the

text: deep convection

text: to become displaced to the south of the center. At 1800 UTC, wind shear began to decrease, and the cyclone developed a well-defined circulation. Based on this, the JTWC upgraded the system into Tropical Storm Hal.

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text: Craton’s music is highly tonal and in general reflects a style of English pastoralism, often incorporating onomatopoeic elements sometimes described as “nature music.” His music has been variously characterized as “atmospheric,” “dramatic and challenging,” “largely traditional ... playful,” and occasionally even reflecting “a medieval/Renaissance flavor.” He has been performed by such artists and ensembles as Sebastiaan de Grebber, Gertrud Weyhofen, Eva van den Dool, Christiaan Saris, Ljubomir Velickovic, Het CONSORT, the Orkest van het Oosten, Townsend Opera Players, and the Amsterdam Symphony Orchestra. Romanian opera composer and conductor Leonard Dumitriu has described Craton's music as "coming from some other time and planet,” stating that although he “may be an American living in the present, ... [his] music comes from the time of Haydn and Mozart, or, better, from a world without time, where ... even the cares are easy and bright ... a musical world of sonorous peace and joy." Many of Craton’s works are published by Wolfhead Music.

text: Craton’s music is highly tonal and in general reflects a style of English pastoralism, often incorporating onomatopoeic elements sometimes described as “nature music.” His music has been variously characterized as “atmospheric,” “dramatic and challenging,” “largely traditional ... playful,” and occasionally even reflecting “a medieval/Renaissance flavor.” He has been performed by such artists and ensembles as

text: Sebastiaan de Grebber

text: Gertrud Weyhofen

text: Eva van den Dool

text: Christiaan Saris

text: Ljubomir Velickovic

text: Het CONSORT

text: , the

text: Orkest van het Oosten

text: Townsend Opera Players

text: , and the

text: Amsterdam Symphony Orchestra

text: . Romanian opera composer and conductor

text: Leonard Dumitriu

text: has described Craton's music as "coming from some other time and planet,” stating that although he “may be an American living in the present, ... [his] music comes from the time of

text: Haydn

text: and

text: Mozart

text: , or, better, from a world without time, where ... even the cares are easy and bright ... a musical world of sonorous peace and joy." Many of Craton’s works are published by

text: Wolfhead Music

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text: The Congo Craton occupies a large part of central southern Africa, extending from the Kasai region of the DRC into Sudan and Angola. It forms parts of the countries of Gabon, Cameroon, and the Central African Republic. A small portion extends into Zambia as well, where it is called the Bangweulu Block.

text: The Congo Craton occupies a large part of central southern Africa, extending from the Kasai region of the

text: DRC

text: into

text: Sudan

text: and

text: Angola

text: . It forms parts of the countries of

text: Gabon

text: Cameroon

text: , and the

text: Central African Republic

text: . A small portion extends into

text: Zambia

text: as well, where it is called the

text: Bangweulu Block

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answer: No

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answer: No

answer: 1

text: When sea levels were lower during the Pleistocene ice ages, greater areas of continental shelf were exposed as dry land, forming land bridges. At those times Australia–New Guinea was a single, continuous continent. Likewise the Americas and Afro-Eurasia were joined by the Bering land bridge. Other islands such as Great Britain were joined to the mainlands of their continents. At that time there were just three discrete continents: Afro-Eurasia-America, Antarctica, and Australia-New Guinea.

text: When sea levels were lower during the

text: Pleistocene

text: ice age

text: s, greater areas of continental shelf were exposed as dry land, forming

text: land bridge

text: s. At those times

text: Australia–New Guinea

text: was a single, continuous continent. Likewise the Americas and Afro-Eurasia were joined by the

text: Bering land bridge

text: . Other islands such as Great Britain were joined to the mainlands of their continents. At that time there were just three discrete continents: Afro-Eurasia-America, Antarctica, and Australia-New Guinea.

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answers: NDQ_005571

answers: continental

answers: NDQ_005572

answers: Pleistocene

answers: NDQ_005573

answers: sea levels were lower

answers: NDQ_005574

answers: Antarctica

answers: NDQ_005575

answers: Pleistocene

answers: NDQ_005576

answers: land bridges

answers: NDQ_005577

answers: sea levels were lower

answers: NDQ_005579

answers: Pleistocene ice ages

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Sites such as the Wopmay Orogen provide evidence for early and ongoing plate tectonics. Traces of old oceanic crust, island arcs, and colliding continents indicate that the same forces at work today have been at work in the early Proterozoic and probably earlier. Alignments of magnetic particles in rocks demonstrate that continents were drifting across the surface of the Earth relative to the magnetic poles then as now, and that the ocean floor was rifting and subducting, all at least 1.5 billion years ago. This crust cycling is referred to as the supercontinent cycle.

text: Sites such as the Wopmay Orogen provide evidence for early and ongoing

text: plate tectonics

text: . Traces of old

text: oceanic crust

text: island arcs

text: , and

text: colliding continents

text: indicate that the same forces at work today have been at work in the early Proterozoic and probably earlier. Alignments of magnetic particles in rocks demonstrate that continents were drifting across the surface of the Earth relative to the magnetic poles then as now, and that the ocean floor was rifting and subducting, all at least 1.5 billion years ago. This crust cycling is referred to as the

text: supercontinent cycle

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answers: oceanic

answers: NDQ_005572

answers: the early Proterozoic

answers: NDQ_005573

answers: the same forces at work today

answers: NDQ_005574

answers: island arcs

answers: NDQ_005575

answers: plate tectonics

answers: NDQ_005576

answers: Orogen

answers: NDQ_005577

answers: Wopmay Orogen

answers: NDQ_005579

answers: early Proterozoic

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: There have been six cratonic sequences since the beginning of the Cambrian Period.  For North America, from oldest to youngest, they are the Sauk, Tippecanoe, Kaskaskia, Absaroka, Zuñi, and the Tejas. Attempts to identify equivalent cratonic sequences on other continents have met with only limited success, suggesting that eustasy is unlikely to be the sole responsible mechanism.

text: There have been six cratonic sequences since the beginning of the

text: Cambrian Period

text: .  For North America, from oldest to youngest, they are the

text: Sauk

text: Tippecanoe

text: Kaskaskia

text: Absaroka

text: Zuñi

text: , and the

text: Tejas

text: . Attempts to identify equivalent cratonic sequences on other continents have met with only limited success, suggesting that eustasy is unlikely to be the sole responsible mechanism.

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answers: Kaskaskia

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answers: the Cambrian Period

answers: NDQ_005573

answers: eustasy

answers: NDQ_005574

answers: have been six cratonic sequences

answers: NDQ_005575

answers: North America, from oldest to youngest

answers: NDQ_005576

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answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: the Cambrian Period

answer: Yes

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Earlier theories (e.g. by Alfred Wegener and Alexander du Toit) of continental drift were that continents "ploughed" through the sea. The idea that the seafloor itself moves (and also carries the continents with it) as it expands from a central axis was proposed by Harry Hess from Princeton University in the 1960s. The theory is well accepted now, and the phenomenon is known to be caused by convection currents in the asthenosphere, which is ductile, or  plastic, and the brittle lithosphere.

text: Earlier theories (e.g. by

text: Alfred Wegener

text: and

text: Alexander du Toit

text: ) of continental drift were that

text: continent

text: s "ploughed" through the sea. The idea that the seafloor itself moves (and also carries the continents with it) as it expands from a central axis was proposed by

text: Harry Hess

text: from

text: Princeton University

text: in the 1960s. The theory is well accepted now, and the phenomenon is known to be caused by

text: convection

text: currents in the

text: asthenosphere

text: , which is ductile, or

text: plastic

text: , and the brittle

text: lithosphere

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answers: lithosphere

answers: NDQ_005572

answers: the sea

answers: NDQ_005573

answers: continental drift

answers: NDQ_005574

answers: continental drift

answers: NDQ_005575

answers: brittle lithosphere

answers: NDQ_005576

answers: Grand Canyon

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Earlier theories

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The exposed geology of the Yosemite area includes primarily  granitic rocks with some older metamorphic rock. The first rocks were laid down in Precambrian times, when the area around Yosemite National Park was on the edge of a very young North American continent. The sediment that formed the area first settled in the waters of a shallow sea, and compressive forces from a subduction zone in the mid-Paleozoic fused the seabed rocks and sediments, appending them to the continent. Heat generated from the subduction created island arcs of volcanoes (not unlike Japan) that were also thrust into the area of the park. In time, the igneous and sedimentary rocks of the area were later heavily metamorphosed.

text: The exposed geology of the Yosemite area includes primarily

text: granitic

text: rocks with some older

text: metamorphic rock

text: . The first rocks were laid down in

text: Precambrian

text: times, when the area around

text: Yosemite National Park

text: was on the edge of a very young

text: North America

text: n continent. The

text: sediment

text: that formed the area first settled in the waters of a shallow sea, and compressive forces from a

text: subduction

text: zone in the mid-

text: Paleozoic

text: fused the seabed

text: rock

text: s and sediments, appending them to the continent. Heat generated from the subduction created

text: island arc

text: s of

text: volcano

text: es (not unlike

text: Japan

text: ) that were also thrust into the area of the park. In time, the

text: igneous

text: and

text: sedimentary rock

text: s of the area were later heavily

text: metamorphosed

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answers: NDQ_005571

answers: granitic

answers: NDQ_005572

answers: a subduction zone

answers: NDQ_005573

answers: volcanoes

answers: NDQ_005574

answers: volcanoes

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answers: Yosemite

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answers: subduction zone

answers: NDQ_005577

answers: shallow sea

answers: NDQ_005579

answers: Precambrian times

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: The term 'shields' first appears in the Star Trek episode "Balance of Terror", in which they were deployed, albeit to little effect, by a Federation outpost under attack from a Romulan Warbird. The first depicted use of shields by a starship was in the Star Trek episode "Arena", in which the USS Enterprise raises its shields after being attacked by an alien warship. Shields are not referred to during the earlier seasons of the Star Trek: Enterprise series, starships instead using "polarized hull plating" to make their hull more resistant to damage.

text: The term 'shields' first appears in the

text: Star Trek

text: episode "

text: Balance of Terror

text: ", in which they were deployed, albeit to little effect, by a

text: Federation

text: outpost under attack from a

text: Romulan

text: Warbird

text: . The first depicted use of shields by a starship was in the Star Trek episode "

text: Arena

text: ", in which the

text: USS Enterprise

text: raises its shields after being attacked by an alien warship. Shields are not referred to during the earlier seasons of the

text: Star Trek: Enterprise

text: series, starships instead using "polarized hull plating" to make their hull more resistant to damage.

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answers: polarized

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answers: Star Trek: Enterprise series

answers: NDQ_005576

answers: Star Trek episode "Arena

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answers: Zircons

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answers: earlier seasons

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Next, the metamorphosed Precambrian basement rocks were uplifted and a nearly 500-million-year-long gap in the geologic record, a major unconformity, affected the region. Geologists do not know what happened to the eroded sediment that must have overlain the complex, but they do know that regional uplift was responsible; the area was originally below the surface of a shallow sea.

text: Next, the metamorphosed Precambrian basement rocks were uplifted and a nearly 500-million-year-long gap in the geologic record, a major

text: unconformity

text: , affected the region. Geologists do not know what happened to the eroded sediment that must have overlain the complex, but they do know that regional uplift was responsible; the area was originally below the surface of a shallow sea.

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answers: Precambrian

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answers: basement rocks

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answers: NDQ_005577

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answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Platform types include the bay platform, side platform (also called through platform), split platform and island platform. A bay platform is one at which the track terminates, i.e. a dead-end or siding. Trains serving a bay platform must reverse in or out. A side platform is the more usual type, alongside tracks where the train arrives from one end and leaves towards the other. An island platform has through platforms on both sides; it may be indented on one or both ends, with bay platforms. To reach an island platform there may be a bridge, a tunnel, or a level crossing. The climb up to the bridge or down to the tunnel may use stairs, ramps, escalators, lifts, or a combination of the above.

text: Platform types include the

text: bay platform

text: side platform

text: (also called through platform),

text: split platform

text: and

text: island platform

text: . A bay platform is one at which the track terminates, i.e. a dead-end or

text: siding

text: . Trains serving a bay platform must reverse in or out. A side platform is the more usual type, alongside tracks where the train arrives from one end and leaves towards the other. An island platform has through platforms on both sides; it may be indented on one or both ends, with bay platforms. To reach an island platform there may be a

text: bridge

text: , a

text: tunnel

text: , or a

text: level crossing

text: . The climb up to the bridge or down to the tunnel may use stairs, ramps, escalators, lifts, or a combination of the above.

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text: On August 30, an area of low pressure developed near the edge of Météo-France's area of responsibility within an unseasonably active monsoonal band which coincided with the Madden–Julian oscillation. Tracking towards the southeast, the low experience strong deep-level wind shear which kept most of the convection displaced from the center of circulation. On August 31, convection managed to develop around the west and southwestern portions of the low before and was designated as Tropical Depression 01. The depression reached its peak intensity at this time with winds of 55 km/h (35 mph

text: On August 30, an

text: area of low pressure

text: developed near the edge of

text: Météo-France

text: 's area of responsibility within an unseasonably active

text: monsoon

text: al band which coincided with the

text: Madden–Julian oscillation

text: . Tracking towards the southeast, the low experience strong deep-level

text: wind shear

text: which kept most of the

text: convection

text: displaced from the

text: center of circulation

text: . On August 31, convection managed to develop around the west and southwestern portions of the low before and was designated as Tropical Depression 01. The depression reached its peak intensity at this time with winds of 55 km/h (35 mph

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text: Many thousand years of dormancy are expected between large explosive eruptions of volcanoes in the Garibaldi Belt. A possible explanation for the lower rates of volcanism in the Garibaldi chain is that the associated terrain is being compressed in contrast to the more southern portions of the Cascade Arc. In continental rift zones, magma is able to push its way up through the Earth's crust rapidly along faults, providing less chance for differentiation. This is likely the case south of Mount Hood to the California border and east-southeast of the massive Newberry shield volcano adjacent to the Cascade Range in central Oregon because the Brothers Fault Zone lies in this region. This rift zone might explain the massive amounts of basaltic lava in this part of the central Cascade Arc. A low convergence rate in a compressional setting with massive stationary bodies of magma under the surface could explain the low volume and differentiated magmas throughout the Garibaldi Volcanic Belt. In 1958, Canadian volcanologist Bill Mathews proposed there could be a connection between regional glaciation of the North American continent during glacial periods and higher rates of volcanic activity during regional glacial unload of the continent. However, this is hard to predict due to the infrequent geological record in this region. But there is specific data, including the temporal grouping of eruptions synglacially or just postglacial within the Garibaldi Belt, that suggests this could be probable.

text: Many thousand years of dormancy are expected between large

text: explosive eruption

text: s of volcanoes in the Garibaldi Belt. A possible explanation for the lower rates of volcanism in the Garibaldi chain is that the associated

text: terrain

text: is being compressed in contrast to the more southern portions of the Cascade Arc. In continental

text: rift

text: zones, magma is able to push its way up through the Earth's crust rapidly along faults, providing less chance for differentiation. This is likely the case south of

text: Mount Hood

text: to the

text: California

text: border and east-southeast of the massive

text: Newberry shield volcano

text: adjacent to the

text: Cascade Range

text: in central

text: Oregon

text: because the

text: Brothers Fault Zone

text: lies in this region. This rift zone might explain the massive amounts of basaltic lava in this part of the central Cascade Arc. A low convergence rate in a compressional setting with massive stationary bodies of magma under the surface could explain the low volume and differentiated magmas throughout the Garibaldi Volcanic Belt. In 1958, Canadian volcanologist

text: Bill Mathews

text: proposed there could be a connection between regional glaciation of the North American continent during

text: glacial period

text: s and higher rates of volcanic activity during regional glacial unload of the continent. However, this is hard to predict due to the infrequent geological record in this region. But there is specific data, including the temporal grouping of eruptions synglacially or just postglacial within the Garibaldi Belt, that suggests this could be probable.

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answer: No

answer: No

answer: No

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text: The Cape Peninsula is a peninsula that juts out into the Atlantic Ocean at the south-western extremity of the African continent. At its tip is the Cape of Good Hope. The peninsula forms the west side of False Bay. The two main rock formations are the late-Precambrian Malmesbury group (metamorphic rock) and the Peninsula granite,  a huge batholith that was intruded into the Malmesbury Group about 630 million years ago.

text: The

text: Cape Peninsula

text: is a

text: peninsula

text: that juts out into the

text: Atlantic Ocean

text: at the south-western extremity of the

text: Africa

text: n continent. At its tip is the

text: Cape of Good Hope

text: . The peninsula forms the west side of False Bay. The two main rock formations are the late-

text: Precambrian

text: Malmesbury group (metamorphic rock) and the Peninsula granite,  a huge batholith that was intruded into the Malmesbury Group about 630 million years ago.

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answers: Malmesbury Group

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answers: Malmesbury Group

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answers: 630 million years ago

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answers: Malmesbury Group

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answers: 630 million years ago

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answers: batholith

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answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: No

answer: No

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text: The passive continental margin became active when the Farallon Plate started to dive below the North American Plate. Geologists call the resulting mountain-building event the Sevier orogeny. Compressive forces detached sedimentary units across western Utah and Nevada from their Precambrian basement rocks and pushed them eastward. The weight of the resulting high mountain range that formed to the west, lowered much of Utah and allowed the sea to invade. This grew into a vast sea that periodically divided North America in the Cretaceous called the Western Interior Seaway.

text: The passive continental margin became active when the

text: Farallon Plate

text: started to dive below the

text: North American Plate

text: . Geologists call the resulting mountain-building event the

text: Sevier orogeny

text: . Compressive forces detached sedimentary units across western Utah and

text: Nevada

text: from their Precambrian basement rocks and pushed them eastward. The weight of the resulting high

text: mountain range

text: that formed to the west, lowered much of Utah and allowed the sea to invade. This grew into a vast sea that periodically divided North America in the Cretaceous called the

text: Western Interior Seaway

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answers: Precambrian

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answers: Precambrian

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answers: Cretaceous

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answers: mountain

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answers: basement rocks

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answers: high mountain range

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

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answers: Precambrian

answer: No

answer: Yes

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answer: No

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text: Africa is the world's second-largest and second-most-populous continent. At about 30.3 million km² (11.7 million square miles) including adjacent islands, it covers six per cent of Earth's total surface area and 20.4 per cent of its total land area. With 1.1 billion people as of 2013, it accounts for about 15% of the world's human population. The continent is surrounded by the Mediterranean Sea to the north, both the Suez Canal and the Red Sea along the Sinai Peninsula to the northeast, the Indian Ocean to the southeast, and the Atlantic Ocean to the west. The continent includes Madagascar and various archipelagos. It contains 54 fully recognized sovereign states (countries), nine territories and two de facto independent states with limited or no recognition.

text: Africa is the world's second-largest and second-most-populous

text: continent

text: . At about 30.3 million km² (11.7 million square miles) including adjacent islands, it covers six per cent of

text: Earth

text: 's total surface area and 20.4 per cent of its total land area. With 1.1 billion people as of 2013, it accounts for about 15% of the world's human population. The continent is surrounded by the

text: Mediterranean Sea

text: to the north, both the

text: Suez Canal

text: and the

text: Red Sea

text: along the

text: Sinai Peninsula

text: to the northeast, the

text: Indian Ocean

text: to the southeast, and the

text: Atlantic Ocean

text: to the west. The continent includes

text: Madagascar

text: and various

text: archipelago

text: s. It contains 54

text: fully recognized

text: sovereign state

text: s (

text: countries

text: ), nine

text: territories

text: and two de facto independent

text: states with limited or no recognition

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text: The geological basement of the central and eastern regions Equatorial Guinea is composed of Precambrian rocks which form a part of the Congo craton. They include gneiss, greenstone, schist-amphibolite and granitoids. These older rocks are overlain by sedimentary rocks of Mesozoic, Neogene and Quaternary age in the west and along the coast. The islands of Pagalu and Bioko (Annobon and Fernando Poo) are of relatively recent volcanic origin, forming a part of the Cameroon Volcanic Line.

text: The geological

text: basement

text: of the central and eastern regions

text: Equatorial Guinea

text: is composed of

text: Precambrian

text: rocks which form a part of the

text: Congo craton

text: . They include

text: gneiss

text: greenstone

text: schist

text: amphibolite

text: and

text: granitoids

text: . These older rocks are overlain by

text: sedimentary rock

text: s of

text: Mesozoic

text: Neogene

text: and

text: Quaternary

text: age in the west and along the coast. The islands of

text: Pagalu

text: and

text: Bioko

text: (Annobon and Fernando Poo) are of relatively recent

text: volcanic origin

text: , forming a part of the

text: Cameroon Volcanic Line

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text: The Guiana Shield is one of the three cratons of the South American Plate. It is a 1.7 billion-year-old Precambrian geological formation in northeast South America that forms a portion of the northern coast. The higher elevations on the shield are called the Guiana Highlands, which is where the table-like mountains called tepuis are found. The Guiana Highlands are also the source of some of the world's most spectacular waterfalls such as Angel Falls, Kaieteur Falls and Kuquenan Falls.

text: The Guiana Shield is one of the three

text: craton

text: s of the

text: South American Plate

text: . It is a 1.7 billion-year-old

text: Precambrian

text: geological formation in northeast

text: South America

text: that forms a portion of the northern coast. The higher elevations on the

text: shield

text: are called the Guiana Highlands, which is where the table-like mountains called

text: tepui

text: s are found. The Guiana Highlands are also the source of some of the world's most spectacular waterfalls such as

text: Angel Falls

text: Kaieteur Falls

text: and

text: Kuquenan Falls

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answers: Precambrian

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answers: Precambrian

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answers: 1.7 billion-year-old

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answers: one of the three

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answers: geological formation

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answers: tepuis

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answers: Precambrian

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answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: In 1889 and 1909 Roberto Mantovani published a hypothesis of Earth expansion and continental drift. He assumed that a closed continent covered the entire surface of a smaller Earth. Thermal expansion led to volcanic activity, which broke the land mass into smaller continents. These continents drifted away from each other because of further expansion at the rip-zones, where oceans currently lie. Although Alfred Wegener noticed some similarities to his own hypothesis of continental drift, he did not mention Earth expansion as the cause of drift in Mantovani's hypothesis.

text: In 1889 and 1909

text: Roberto Mantovani

text: published a hypothesis of Earth expansion and continental drift. He assumed that a closed continent covered the entire surface of a smaller Earth.

text: Thermal expansion

text: led to

text: volcanic

text: activity, which broke the land mass into smaller continents. These continents drifted away from each other because of further expansion at the rip-zones, where oceans currently lie. Although

text: Alfred Wegener

text: noticed some similarities to his own hypothesis of

text: continental drift

text: , he did not mention Earth expansion as the cause of drift in Mantovani's hypothesis.

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answers: volcanic

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answers: volcanic activity

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answers: thermal expansion

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answers: volcanic activity

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answers: a smaller Earth

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answers: rip-zone

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answers: oceans

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answers: Thermal expansion

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Because of this early uncontrolled exploitation, much of the reserves in the Mid-continent have been depleted. Oil operators, in addition to continued exploration, use a variety of techniques to increase production, including deep wells, injection wells, etc. Natural gas, which in the early days was vented to the atmosphere or burned off, now accounts for a large percentage of the exploration efforts and profitability of the petroleum industry in the Mid-continent.

text: Because of this early uncontrolled exploitation, much of the reserves in the Mid-continent have been depleted. Oil operators, in addition to continued exploration, use a variety of techniques to increase production, including deep wells, injection wells, etc. Natural gas, which in the early days was vented to the atmosphere or burned off, now accounts for a large percentage of the exploration efforts and profitability of the petroleum industry in the Mid-continent.

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answers: Mid-continent

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answers: Mid-continent

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answers: uncontrolled exploitation

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answers: Mid-continent

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answers: uncontrolled exploitation

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answers: deep wells

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: in the early days

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Arvoredo archipelago (27°17' S; 48°28' W) is formed by three islands (Arvoredo, Galés and Deserta) and a rocky outcrop (São Pedro). The archipelago lies over the continental platform and is characterized by the presence of Precambrian crystalline rock shorelines. The depth throughout the archipelago varies from , rarely deeper than .

text: The Arvoredo archipelago (27°17' S; 48°28' W) is formed by three islands (Arvoredo, Galés and Deserta) and a rocky outcrop (São Pedro). The archipelago lies over the continental platform and is characterized by the presence of

text: Precambrian

text: crystalline rock shorelines. The depth throughout the archipelago varies from , rarely deeper than .

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text: By day the globe was illuminated by the light from the glass set into the dome directly above it and by night with gas lighting. Visitors entered the globe through an opening into the Pacific Ocean, then ascended through a series of four platforms. At each stage they could see a different portion of the world represented on the concave interior face of the globe. The platform scaffolding was built up from the conveniently desolate Southern Ocean; Antarctica was largely unknown at the time – Wyld dismissed stories of the existence of a great Southern continent: The platforms were separated by about  and those closer to the Globe's equator were wider so there was always a gap of about  between the platform and the surface of the globe. Although the staircase and platforms allowed closer examination of individual sections, the structure prevented an appreciation of the globe as a single unit, and later there were plans for its removal. Some ventilation was provided by a system housed at the North Pole, which had the advantage of being quite featureless and located at the top of the globe, but the heat generated from the gas lighting and the mass of visitors meant the attraction was still uncomfortably hot; Henry Morley remarked that "the heat reflected on all sides from the concave surfaces rises to make a little Sahara of the North Pole Station", and Punch commented that the temperature was "equal to that of any baker's oven."

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text: Some 30 years later, a number of studies have documented an abundance of geochemical and microfossil evidence showing that life covered the continents as far back as 2.2 billion years ago. Many paleobiologists now accept the idea that simple life forms existed on land during the Precambrian, but are opposed to the more radical idea that multicellular life thrived on land more than 600 million years ago.

text: Some 30 years later, a number of studies have documented an abundance of geochemical and microfossil evidence showing that life covered the continents as far back as 2.2 billion years ago. Many paleobiologists now accept the idea that simple life forms existed on land during the Precambrian, but are opposed to the more radical idea that multicellular life thrived on land more than 600 million years ago.

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answers: Precambrian

answers: NDQ_005572

answers: the Precambrian

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answers: life

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answers: continents

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answers: life covered the continents

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answers: Grand Canyon

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answers: microfossil

answers: NDQ_005579

answers: the Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Over the past 1 billion years, East Antarctica has traveled from tropical (to subtropical) southerly latitudes to its current location with the entire East Antarctic Shield positioned south of the Antarctic Circle. Despite its relative lack of motion over the past 75 million years, the East Antarctic Shield has played a significant role in the arrangement and motion of its surrounding plates during the amalgamation and separation of the supercontinents, Rodinia, Gondwana, and Pangea. Because the surface of the shield is covered by ice and thus, inaccessible by man, the information about its tectonic history comes primarily from seismic and core-sample data. Geologists have used this data to define the rock types present, age the rocks using radioactive dating techniques, unveil the climate history from isotope ratios, and trace the shield’s motion based on varying magnetic properties. Unfortunately, there are only a few places where data can be collected directly from the basement rock, and even at these locations, the exposed areas of the central craton can be misleading due to factors such as reworking during high-grade late Neoproterozoic to Cambrian deformation, variable overprinting by Cambrian tectonics, and the presence of younger metasediments. However, it has been determined that the East Antarctic Shield has a Precambrian to Ordovician basement of igneous and sedimentary rocks that are deformed and metamorphosed to varying degrees, and intruded by syn- to post-tectonic granites. The basement is locally overlain by undeformed Devonian to Jurassic sediments, and intruded by Jurassic tholeiitic plutonic and volcanic rocks. This knowledge of the shield’s structural features and compositions leads to the development of a tectonic history. The traditional models of East Antarctic Shield geology typically involve a three-stage tectonic history that includes:

text: Over the past 1 billion years,

text: East Antarctica

text: has traveled from tropical (to subtropical) southerly latitudes to its current location with the entire East Antarctic Shield positioned south of the

text: Antarctic Circle

text: . Despite its relative lack of motion over the past 75 million years, the East Antarctic Shield has played a significant role in the arrangement and motion of its surrounding plates during the amalgamation and separation of the

text: supercontinents

text: Rodinia

text: Gondwana

text: , and

text: Pangea

text: . Because the surface of the

text: shield

text: is covered by ice and thus, inaccessible by man, the information about its tectonic history comes primarily from seismic and core-sample data. Geologists have used this data to define the rock types present, age the rocks using

text: radioactive dating techniques

text: , unveil the climate history from

text: isotope

text: ratios, and trace the shield’s motion based on varying magnetic properties. Unfortunately, there are only a few places where data can be collected directly from the basement rock, and even at these locations, the exposed areas of the central craton can be misleading due to factors such as reworking during high-grade late

text: Neoproterozoic

text: to

text: Cambrian

text: deformation, variable overprinting by

text: Cambrian

text: tectonics, and the presence of younger

text: metasediment

text: s. However, it has been determined that the East Antarctic Shield has a

text: Precambrian

text: to

text: Ordovician

text: basement

text: of

text: igneous

text: and

text: sedimentary rock

text: s that are deformed and metamorphosed to varying degrees, and intruded by syn- to post-tectonic

text: granite

text: s. The basement is locally overlain by undeformed

text: Devonian

text: to

text: Jurassic

text: sediments, and intruded by

text: Jurassic

text: tholeiitic

text: pluton

text: ic and volcanic rocks. This knowledge of the shield’s structural features and compositions leads to the development of a tectonic history. The traditional models of East Antarctic Shield geology typically involve a three-stage tectonic history that includes:

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answers: Devonian

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answers: Devonian

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answers: Cambrian tectonics

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answers: igneous and sedimentary rocks

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answers: tectonic

answers: NDQ_005577

answers: Precambrian to Ordovician

answers: NDQ_005579

answers: Precambrian to Ordovician

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil record is poorer than that of the succeeding Phanerozoic, and those fossils present (e.g. stromatolites) are of limited biostratigraphic use. This is because many Precambrian rocks have been heavily metamorphosed, obscuring their origins, while others have been destroyed by erosion, or remain deeply buried beneath Phanerozoic strata.

text: Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the

text: Earth's history

text: , and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil record is poorer than that of the succeeding

text: Phanerozoic

text: , and those fossils present (e.g.

text: stromatolites

text: ) are of limited

text: biostratigraphic

text: use. This is because many Precambrian rocks have been heavily

text: metamorphosed

text: , obscuring their origins, while others have been destroyed by erosion, or remain deeply buried beneath Phanerozoic strata.

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answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: heavy metamorphosed

answers: NDQ_005574

answers: Precambrian

answers: NDQ_005575

answers: seven-eighths

answers: NDQ_005576

answers: strata

answers: NDQ_005577

answers: stromatolites

answers: NDQ_005579

answers: the Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Canadian shield, Precambrian shield, makes up the bedrock geology highlighted by rocks and lakes and a boreal forest area.  There are transitional areas between boreal and tundra flora. The lower boundary of the Canadian Shield cuts across the province diagonally from the latitude 57 degrees in the north west to 54 degrees in the south east.  Three orogenies formed the Precambrian shield, the Kenoran (Laurentian-Algoman), Hudsonian (Penokean) and Grenville Orogeny.  Between 2.2 and 2.5 billion years ago was the Kenoran Orogeny, which was overlain by the Hudsonian Orogeny 1700 to 1900 million years ago.  The earth was experiencing hotter and more volatile Archean tectonics, evidencing island arc volcanic activity and mountain building. The Trans-Hudson Orogen occurred when a number of Archean continental blocks came together, including the Superior Craton from the southeast and Hearne-Rae craton from the northwest.  A microcontinent named the Sask Craton was underlain in this collision zone.  The Canadian Grenville province occurred between 1080 and 980 Ma and did not affect the geology of the Canadian Shield in Saskatchewan.  The Grenvillian Orogeny deformed much of eastern Canada, and includes the Grenville Front Tectonic Zone in Quebec and Labrador, the Appalachian structural front to the south between what we now name the Great Lakes and Newfoundland.

text: The Canadian shield, Precambrian shield, makes up the bedrock geology highlighted by rocks and lakes and a

text: boreal forest

text: area.  There are transitional areas between boreal and tundra flora. The lower boundary of the Canadian Shield cuts across the province diagonally from the

text: latitude 57 degrees

text: in the north west to

text: 54 degrees

text: in the south east.  Three

text: orogenies

text: formed the Precambrian shield, the Kenoran (Laurentian-

text: Algoman

text: Hudsonian

text: (Penokean) and

text: Grenville Orogeny

text: .  Between 2.2 and 2.5 billion years ago was the Kenoran Orogeny, which was overlain by the Hudsonian Orogeny 1700 to 1900 million years ago.  The earth was experiencing hotter and more volatile Archean tectonics, evidencing island arc volcanic activity and mountain building. The Trans-Hudson Orogen occurred when a number of Archean continental blocks came together, including the Superior Craton from the southeast and Hearne-Rae craton from the northwest.  A microcontinent named the

text: Sask Craton

text: was underlain in this collision zone.  The Canadian Grenville province occurred between 1080 and 980 Ma and did not affect the geology of the Canadian Shield in Saskatchewan.  The Grenvillian Orogeny deformed much of eastern Canada, and includes the

text: Grenville Front Tectonic Zone

text: in Quebec and Labrador, the Appalachian structural front to the south between what we now name the Great Lakes and Newfoundland.

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answers: Precambrian

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answers: Kenoran Orogeny

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answers: The earth was experiencing hotter

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answers: Archean tectonics

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Continental shields occur on all continents, for example:

text: Continental shields occur on all continents, for example:

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answers: continental shield

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answers: continental shields

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answers: continental shields occur on all continents

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answers: continental shields

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answers: continental shields

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answers: continental shields occur on all continents

answers: NDQ_005577

answers: Zircon is a mineral.

answers: NDQ_005579

answers: continental shields occur on all continents

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: After attaining tropical storm status, the maximum sustained winds fluctuated for three days between 40 mph (65 km/h) and 50 mph (85 km/h). This was due to the large size of Florence; the overall wind field reached a diameter of 460 miles (745 km), and the radius of maximum winds reached about 110 miles (170 km). By September 6, a well-defined cloud swirl became evident, with thin rainbands developing in the southeast and northwest quadrants. As a result, hurricane forecasters anticipated Florence would develop significantly and attain major hurricane status. Though convection gradually migrated closer to the center of the storm, forecasters could not detect a well-defined center of circulation by late on September 6. On September 7, convection developed over and to the west of the center for the first time in its duration. However, Florence failed to intensify further, as its wind field had increased to more than 1,035 miles (1,670 km) in diameter. This led to difficulties in forecasting, as its environment favored further strengthening; the storm tracked through an area of 84° F (29° C) water temperatures and light shear, and the system maintained a large low-level cyclonic envelop with abundant convection. By early on September 8, the storm consisted of an elongated, shapeless cloud pattern atypical of a tropical cyclone. Later that day, as an anticyclone developed over Florence, the storm began to consolidate around a vorticity center on the western side of the large cyclonic envelope. It began to strengthen more steadily as it turned to the northwest. Early on September 10, an eye began developing within a round central dense overcast over the center, and shortly thereafter Florence attained hurricane status while located about 390 miles (630 km) south of Bermuda.

text: After attaining tropical storm status, the maximum sustained winds fluctuated for three days between 40 mph (65 km/h) and 50 mph (85 km/h). This was due to the large size of Florence; the overall wind field reached a diameter of 460 miles (745 km), and the radius of maximum winds reached about 110 miles (170 km). By September 6, a well-defined cloud swirl became evident, with thin rainbands developing in the southeast and northwest quadrants. As a result, hurricane forecasters anticipated Florence would develop significantly and attain

text: major hurricane status

text: . Though convection gradually migrated closer to the center of the storm, forecasters could not detect a well-defined center of circulation by late on September 6. On September 7, convection developed over and to the west of the center for the first time in its duration. However, Florence failed to intensify further, as its wind field had increased to more than 1,035 miles (1,670 km) in diameter. This led to difficulties in forecasting, as its environment favored further strengthening; the storm tracked through an area of 84°

text: F

text: C

text: ) water temperatures and light shear, and the system maintained a large low-level cyclonic envelop with abundant convection. By early on September 8, the storm consisted of an elongated, shapeless cloud pattern atypical of a tropical cyclone. Later that day, as an

text: anticyclone

text: developed over Florence, the storm began to consolidate around a vorticity center on the western side of the large cyclonic envelope. It began to strengthen more steadily as it turned to the northwest. Early on September 10, an

text: eye

text: began developing within a round central dense overcast over the center, and shortly thereafter Florence attained hurricane status while located about 390 miles (630 km) south of

text: Bermuda

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answers: 390 miles (630 km)

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answers: Florence attained hurricane status

answers: NDQ_005577

answers: water

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answers: tropical storm status

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: The Be number plays in forced convection the same role that the Rayleigh number plays in natural convection.

text: The Be number plays in forced convection the same role that the

text: Rayleigh number

text: plays in natural convection.

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answers: Be number

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answers: natural convection

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answers: convection

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answers: forced convection

answers: NDQ_005576

answers: The Be number plays in forced convection

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment.

answers: NDQ_005579

answers: natural convection

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Besides having compositional effects on the upper mantle by replenishing the large-ion lithophile elements, volcanism affects the plate movement. The plates will be moved towards a geoidal low perhaps where the slab avalanche occurred and pushed away from the geoidal high that can be caused by the plumes or superplumes. This causes the continents to push together to form supercontinents and was evidently the process that operated to cause the early continental crust to aggregate into Protopangea. Dispersal of supercontinents is caused by the accumulation of heat underneath the crust due to the rising of very large convection cells or plumes, and a massive heat release resulted in the final break-up of Paleopangea. Accretion occurs over geoidal lows that can be caused by avalanche slabs or the downgoing limbs of convection cells. Evidence of the accretion and dispersion of supercontinents is seen in the geological rock record.

text: Besides having compositional effects on the upper mantle by replenishing the

text: large-ion lithophile elements

text: , volcanism affects the plate movement. The plates will be moved towards a geoidal low perhaps where the slab avalanche occurred and pushed away from the geoidal high that can be caused by the plumes or superplumes. This causes the continents to push together to form supercontinents and was evidently the process that operated to cause the early continental crust to aggregate into Protopangea. Dispersal of supercontinents is caused by the accumulation of heat underneath the crust due to the rising of very large

text: convection cell

text: s or plumes, and a massive heat release resulted in the final break-up of Paleopangea. Accretion occurs over geoidal lows that can be caused by avalanche slabs or the downgoing limbs of convection cells. Evidence of the accretion and dispersion of supercontinents is seen in the geological rock record.

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answers: lithophile

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answers: NDQ_005573

answers: supercontinents

answers: NDQ_005574

answers: supercontinents

answers: NDQ_005575

answers: Paleopangea

answers: NDQ_005576

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answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Paleopangea

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Through most of the Archean Eon, the Earth had a heat production at least twice that of the present, which caused tectonic processes to be more active. As a result, plates and continents were smaller. No broad blocks as old as 3 Ga are found in Precambrian shields. Toward the end of the Archean, however, some of these blocks or terranes came together to form larger blocks welded together by greenstone belts.

text: Through most of the

text: Archean

text: Eon, the Earth had a heat production at least twice that of the present, which caused

text: tectonic

text: processes to be more active. As a result, plates and continents were smaller. No broad blocks as old as 3 Ga are found in

text: Precambrian

text: shields

text: . Toward the end of the Archean, however, some of these blocks or

text: terranes

text: came together to form larger blocks welded together by

text: greenstone belts

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answers: 3

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answers: 0

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answers: 0

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answers: 4

answers: NDQ_005571

answers: greenstone

answers: NDQ_005572

answers: Precambrian shields

answers: NDQ_005573

answers: larger blocks welded together

answers: NDQ_005574

answers: tectonic processes

answers: NDQ_005575

answers: 3 Ga

answers: NDQ_005576

answers: shields

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Archean Eon

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The positions of Laurentia and other landmasses in the Precambrian super continent of Rodinia are controversial. Although geological and isotopic data support an East Antarctic fit with western Laurentia, alternative reconstructions favor the juxtaposition of Australia, Siberia, or South China. New geologic, age, and isotopic data provide a positive test of the juxtaposition with East Antarctica: Neodymium isotopes of Neoproterozoic rift-margin strata are similar; hafnium isotopes of about 1.4 billion year old Antarctic-margin detrital zircons match those in Laurentian granites of similar age; and a glacial clast of A-type granite has a uranium-lead zircon age of ~1440 million years, an epsilon-hafnium initial value of +7, and an epsilon-neodymium initial value of +4. These tracers indicate the presence of granites in East Antarctica having the same age, geochemical properties, and isotopic signatures as the distinctive granites in Laurentia.

text: The positions of Laurentia and other landmasses in the Precambrian super continent of

text: Rodinia

text: are controversial. Although geological and isotopic data support an East Antarctic fit with western Laurentia, alternative reconstructions favor the juxtaposition of Australia, Siberia, or South China. New geologic, age, and isotopic data provide a positive test of the juxtaposition with East Antarctica: Neodymium isotopes of Neoproterozoic rift-margin strata are similar; hafnium isotopes of about 1.4 billion year old Antarctic-margin detrital zircons match those in Laurentian granites of similar age; and a glacial clast of A-type granite has a uranium-lead zircon age of ~1440 million years, an epsilon-hafnium initial value of +7, and an epsilon-neodymium initial value of +4. These tracers indicate the presence of granites in East Antarctica having the same age, geochemical properties, and isotopic signatures as the distinctive granites in Laurentia.

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answers: Precambrian

answers: NDQ_005572

answers: Laurentia

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Laurentia

answers: NDQ_005575

answers: 1.4 billion year old

answers: NDQ_005576

answers: Precambrian

answers: NDQ_005577

answers: Yes

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Exiting Bobcaygeon, the former highway serves cottages along the northern shore of Pigeon Lake and Little Bald Lake. After passing Nogies Creek, the highway descends a hill and encounters the Canadian Shield for the first time. The road runs along the border of the Precambrian shield and the Ordovician limestone plateau en route to Burleigh Falls. The shield lies to the north and is overlain by the plateau to the south.The highway turns south at Flynns Corner, intersecting former Highway 507. It enters the town of Buckhorn from the north, then drivers must turn to remain on the route, which exits the town to the east. Between Buckhorn and Burleigh Falls, the highway serves the cottages that line the northern shore of Lower Buckhorn Lake.

text: Exiting Bobcaygeon, the former highway serves cottages along the northern shore of

text: Pigeon Lake

text: and

text: Little Bald Lake

text: . After passing

text: Nogies Creek

text: , the highway descends a hill and encounters the

text: Canadian Shield

text: for the first time. The road runs along the border of the

text: Precambrian

text: shield and the

text: Ordovician

text: limestone plateau en route to Burleigh Falls. The shield lies to the north and is overlain by the plateau to the south.The highway turns south at Flynns Corner, intersecting former

text: Highway 507

text: . It enters the town of

text: Buckhorn

text: from the north, then drivers must turn to remain on the route, which exits the town to the east. Between Buckhorn and Burleigh Falls, the highway serves the cottages that line the northern shore of

text: Lower Buckhorn Lake

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answers: Ordovician limestone

answers: NDQ_005572

answers: the Canadian Shield

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Canadian Shield

answers: NDQ_005575

answers: Canadian Shield

answers: NDQ_005576

answers: Canadian Shield

answers: NDQ_005577

answers: Lake

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Precambrian bedrock of the Duluth Complex and the North Shore Volcanics are not buried beneath layers of later sedimentary rock, as is common further south; much of this bedrock is close to or at the surface.  Glaciers scoured away earlier soils, and as is typical of the Canadian Shield, the new topsoils are thin and poor, being derived from the rock beneath or nearby rather than from deep layers of glacial till, which is intermittent and relatively shallow over most of the region.  Consequently, much of the bedrock is exposed, except for the sediments and glacial till in the watershed of the Saint Louis and Cloquet Rivers inland on the west.

text: The Precambrian bedrock of the Duluth Complex and the North Shore Volcanics are not buried beneath layers of later sedimentary rock, as is common further south; much of this bedrock is close to or at the surface.  Glaciers scoured away earlier soils, and as is typical of the Canadian Shield, the new topsoils are thin and poor, being derived from the rock beneath or nearby rather than from deep layers of

text: glacial till

text: , which is intermittent and relatively shallow over most of the region.  Consequently, much of the bedrock is exposed, except for the sediments and glacial till in the watershed of the

text: Saint Louis

text: and

text: Cloquet River

text: s inland on the west.

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answers: close to or at the surface

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answers: 0

answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Volcanics

answers: NDQ_005575

answers: Canadian Shield

answers: NDQ_005576

answers: Duluth Complex

answers: NDQ_005577

answers: the Saint Louis and Cloquet Rivers

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Convective heat transfer is one of the major types of heat transfer, and convection is also a major mode of mass transfer in fluids. Convective heat and mass transfer take place both by diffusion – the random Brownian motion of individual particles in the fluid – and by advection, in which matter or heat is transported by the larger-scale motion of currents in the fluid. In the context of heat and mass transfer, the term "convection" is used to refer to the sum of advective and diffusive transfer. In common use the term "convection" may refer loosely to heat transfer by convection, as opposed to mass transfer by convection, or the convection process in general. Sometimes "convection" is even used to refer specifically to "free heat convection" (natural heat convection) as opposed to forced heat convection. However, in mechanics the correct use of the word is the general sense, and different types of convection should be qualified for clarity.

text: Convective heat transfer

text: is one of the major types of

text: heat transfer

text: , and convection is also a major mode of

text: mass transfer

text: in fluids. Convective heat and mass transfer take place both by

text: diffusion

text: – the random

text: Brownian motion

text: of individual particles in the fluid – and by

text: advection

text: , in which matter or heat is transported by the larger-scale motion of currents in the fluid. In the context of heat and mass transfer, the term "convection" is used to refer to the sum of

text: advective

text: and diffusive transfer. In common use the term "convection" may refer loosely to heat transfer by convection, as opposed to mass transfer by convection, or the convection process in general. Sometimes "convection" is even used to refer specifically to "free heat convection" (natural heat convection) as opposed to forced heat convection. However, in mechanics the correct use of the word is the general sense, and different types of convection should be qualified for clarity.

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text: The first officially recognized tropical disturbance developed early on October 10. The disturbance featured persistent convection around an elongated low level circulation located about  west-northwest of Diego Garcia. With marginally favorable. conditions for further development, the JTWC assessed the chances of the low developing into a tropical cyclone as "poor". Further development took place later that day, with banding features developing and deepening convection as it traveled towards the south-southwest. In response to the increased development, the JTWC increased the chances of a tropical cyclone developing to "fair". On October 12 Météo-France designated the system as Tropical Disturbance 01-20072008. However, little or no further development was expected.

text: The first officially recognized tropical disturbance developed early on October 10. The disturbance featured persistent

text: convection

text: around an elongated

text: low level circulation

text: located about  west-northwest of

text: Diego Garcia

text: . With marginally favorable. conditions for further development, the JTWC assessed the chances of the low developing into a

text: tropical cyclone

text: as "poor". Further development took place later that day, with

text: banding features

text: developing and deepening convection as it traveled towards the south-southwest. In response to the increased development, the JTWC increased the chances of a tropical cyclone developing to "fair". On October 12

text: Météo-France

text: designated the system as Tropical Disturbance 01-20072008. However, little or no further development was expected.

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answers: It indicates that there was water in the environment.

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text: While in his early years Craton often performed on violin, piano, recorder, and other instruments, he abandoned public performance after a hand injury and has since devoted himself completely to teaching and composing. He currently operates a private music studio in Bedford, Indiana.

text: While in his early years Craton often performed on

text: violin

text: piano

text: recorder

text: , and other instruments, he abandoned public performance after a hand injury and has since devoted himself completely to teaching and composing. He currently operates a private music studio in

text: Bedford, Indiana

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answers: in his early years

answer: No

answer: No

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text: East Antarctica is geologically varied, dating from the Precambrian era, with some rocks formed more than 3 billion years ago. It is composed of a metamorphic and igneous platform which is the basis of the continental shield. On top of this base are coal and various modern rocks, such as sandstones, limestones and shales laid down during the Devonian and Jurassic periods to form the Transantarctic Mountains. In coastal areas such as Shackleton Range and Victoria Land some faulting has occurred.

text: East Antarctica is geologically varied, dating from the

text: Precambrian

text: era, with some rocks formed more than 3 billion years ago. It is composed of a

text: metamorphic

text: and

text: igneous

text: platform which is the basis of the

text: continental shield

text: . On top of this base are coal and various modern rocks, such as

text: sandstone

text: s,

text: limestone

text: s and

text: shale

text: s laid down during the Devonian and Jurassic periods to form the

text: Transantarctic Mountains

text: . In coastal areas such as

text: Shackleton Range

text: and

text: Victoria Land

text: some

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text: has occurred.

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answers: Precambrian

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answers: Devonian

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answers: Devonian

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answers: Transantarctic Mountains

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answers: continental shield

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answers: continental shield

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The geologic history of the region began with the deposition of late Precambrian to early Cambrian sandstones collectively known as the Tillman metasedimentary group.  These sediments were intruded by a coarse mafic layered complex about 575 million years ago as the region began to rift apart in an aulacogen during breakup of the Neoproterozoic continent, Pannotia.  The exposed portion of this unit, named the Glen Mountains Layered Complex, consists of gabbro, anorthosite and troctolite.  These are the dark gray rocks found throughout the Raggedy Mountains, the central region of the wildlife refuge, and to the immediate north of the refuge.

text: The

text: geologic

text: history of the region began with the deposition of late

text: Precambrian

text: to early

text: Cambrian

text: sandstone

text: s collectively known as the Tillman metasedimentary group.  These sediments were

text: intruded

text: by a coarse

text: mafic

text: layered complex

text: about 575 million years ago as the region began to

text: rift

text: apart in an

text: aulacogen

text: during breakup of the

text: Neoproterozoic

text: continent,

text: Pannotia

text: .  The exposed portion of this unit, named the Glen Mountains Layered Complex, consists of

text: gabbro

text: anorthosite

text: and

text: troctolite

text: .  These are the dark gray rocks found throughout the Raggedy Mountains, the central region of the wildlife refuge, and to the immediate north of the refuge.

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answers: Neoproterozoic

answers: NDQ_005572

answers: Pannotia

answers: NDQ_005573

answers: breakup

answers: NDQ_005574

answers: Pannotia

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answers: 575 million years ago

answers: NDQ_005576

answers: aulacogen

answers: NDQ_005577

answers: zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The oldest form of shield was a protection device designed to block attacks by hand weapons, such as swords, axes and maces, or ranged weapons like sling-stones and arrows. Shields have varied greatly in construction over time and place. Sometimes shields were made of metal, but wood or animal hide construction was much more common; wicker and even turtle shells have been used. Many surviving examples of metal shields are generally felt to be ceremonial rather than practical, for example the Yetholm-type shields of the Bronze Age, or the Iron Age Battersea shield.

text: The oldest form of shield was a protection device designed to block attacks by

text: hand weapon

text: s, such as swords, axes and maces, or ranged weapons like sling-stones and arrows. Shields have varied greatly in construction over time and place. Sometimes shields were made of metal, but

text: wood

text: or

text: animal hide

text: construction was much more common;

text: wicker

text: and even turtle shells have been used. Many surviving examples of metal shields are generally felt to be ceremonial rather than practical, for example the

text: Yetholm-type shields

text: of the

text: Bronze Age

text: , or the

text: Iron Age

text: Battersea shield

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Africa is suffering deforestation at twice the world rate, according to the United Nations Environment Programme (UNEP). Some sources claim that deforestation has already wiped out roughly 90% of West Africa's original forests. Deforestation is accelerating in Central Africa. According to the FAO, Africa lost the highest percentage of tropical forests of any continent during the 1980s, 1990s, and early 2000s. According to the figures from the FAO (1997), only 22.8% of West Africa's moist forests remain, much of this degraded. Nigeria has lost 81% of its old-growth forests in just 15 years (1990–2005).  Massive deforestation threatens food security in some African countries.  One factor contributing to the continent's high rates of deforestation is the dependence of 90% of its population on wood as fuel for heating and cooking.

text: Africa is suffering deforestation at twice the world rate, according to the United Nations Environment Programme (

text: UNEP

text: ). Some sources claim that deforestation has already wiped out roughly 90% of

text: West Africa

text: 's original forests. Deforestation is accelerating in

text: Central Africa

text: . According to the

text: FAO

text: , Africa lost the highest percentage of tropical forests of any continent during the 1980s, 1990s, and early 2000s. According to the figures from the FAO (1997), only 22.8% of West Africa's

entity_name: Tropical and subtropical moist broadleaf forests

text: moist forest

text: s remain, much of this degraded. Nigeria has lost 81% of its old-growth forests in just 15 years (1990–2005).  Massive deforestation threatens

text: food security

text: in some African countries.  One factor contributing to the continent's high rates of deforestation is the dependence of 90% of its population on wood as fuel for heating and cooking.

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answers: tropical forests

answers: NDQ_005572

answers: Africa

answers: NDQ_005573

answers: Africa is suffering deforestation at twice the world rate

answers: NDQ_005574

answers: Africa

answers: NDQ_005575

answers: deforestation

answers: NDQ_005576

answers: deforestation

answers: NDQ_005577

answers: 22.8% of West Africa's moist forests remain

answers: NDQ_005579

answers: tropical forests

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A typical subway station has waiting platforms ranging from  long, though some IND platforms may be as long as  long. Platforms of former commuter rail stations, such as those on the IND Rockaway Line, are even longer. Due to the large number of transit lines, one platform or set of platforms often serves more than one service (unlike other rapid transit systems including the Paris Metro, but like some lines on the London Underground). A passenger needs to look at the signs hung at the platform entrance steps and over each track to see which trains stop there and when, and at the arriving train to see which train it is.

text: A typical subway station has waiting platforms ranging from  long, though some IND platforms may be as long as  long. Platforms of former commuter rail stations, such as those on the

text: IND Rockaway Line

text: , are even longer. Due to the large number of transit lines, one platform or set of platforms often serves more than one service (unlike other rapid transit systems including the

text: Paris Metro

text: , but like some lines on the

text: London Underground

text: ). A passenger needs to look at the signs hung at the platform entrance steps and over each track to see which trains stop there and when, and at the arriving train to see which train it is.

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answers: NDQ_005571

answers: IND

answers: NDQ_005572

answers: IND

answers: NDQ_005573

answers: long

answers: NDQ_005574

answers: IND Rockaway Line

answers: NDQ_005575

answers: long

answers: NDQ_005576

answers: platform or set of platforms often serves more than one service

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: commuter rail stations

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Ontario, owing to its size, has diverse geology that varies in structure, age, and lithology. About 61% of the province is covered by the Canadian Shield, mostly with Precambrian rock. These rocks contain large mineral deposits that are vital to the economy of northern Ontario. The shield can further be divided into three sections. The northwestern parts of the Shield, located roughly north and west of Sudbury, are known as the Superior Province;  this is the largest of the three sections, covering about 70% of the Shield portion in Ontario. This region is more than 2.5 billion years old and is composed of felsic intrusive rocks. In the northernmost parts of the Superior Province, the geology of the region is dominated by granite and gneiss rocks. The central region of the Shield, known as the Grenville Province and located south of Sudbury, is 1.0 to 1.6 billion years old and is dominated by sedimentary rocks showing evidence of being subjected to metamorphism. It makes up about 20% of the Canadian Shield in Ontario. These rocks were metamorphosed between 990 million years ago and 1.08 billion years ago. The third region, known as the Southern province which is a narrow region from Sault Ste. Marie to Kirkland Lake, is made of rocks dating 1.8 to 2.4 billion years ago.  The Hudson Bay lowlands, located north of the Canadian Shield, are mainly made of sedimentary rocks from the Silurian Period, although some parts date from the Ordovician and Devonian periods. This area covers 25% of the province. Most of the bedrock in the Hudson Bay lowlands is composed of limestone and carbonate-dominated sedimentary rock.

text: Ontario, owing to its size, has diverse geology that varies in structure, age, and lithology. About 61% of the province is covered by the

text: Canadian Shield

text: , mostly with

text: Precambrian

text: rock. These rocks contain large mineral deposits that are vital to the economy of northern Ontario. The shield can further be divided into three sections. The northwestern parts of the Shield, located roughly north and west of Sudbury, are known as the Superior Province;  this is the largest of the three sections, covering about 70% of the Shield portion in Ontario. This region is more than 2.5 billion years old and is composed of

text: felsic

text: intrusive rocks. In the northernmost parts of the Superior Province, the geology of the region is dominated by granite and gneiss rocks. The central region of the Shield, known as the Grenville Province and located south of Sudbury, is 1.0 to 1.6 billion years old and is dominated by sedimentary rocks showing evidence of being subjected to metamorphism. It makes up about 20% of the Canadian Shield in Ontario. These rocks were metamorphosed between 990 million years ago and 1.08 billion years ago. The third region, known as the Southern province which is a narrow region from Sault Ste. Marie to Kirkland Lake, is made of rocks dating 1.8 to 2.4 billion years ago.  The Hudson Bay lowlands, located north of the Canadian Shield, are mainly made of sedimentary rocks from the

text: Silurian Period

text: , although some parts date from the

text: Ordovician

text: and

text: Devonian

text: periods. This area covers 25% of the province. Most of the bedrock in the Hudson Bay lowlands is composed of limestone and carbonate-dominated sedimentary rock.

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answers: 4

answers: NDQ_005576

answers: 0

answers: NDQ_005577

answers: 0

answers: NDQ_005579

answers: 0

answers: NDQ_005571

answers: Silurian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: these rocks were metamorphosed

answers: NDQ_005574

answers: The shield can further be divided into three sections

answers: NDQ_005575

answers: Canadian Shield

answers: NDQ_005576

answers: Silurian Period

answers: NDQ_005577

answers: Hudson Bay lowlands

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There are many microcontinents, or continental fragments, that are built of continental crust but do not contain a craton. Some of these are fragments of Gondwana or other ancient cratonic continents: Zealandia, which includes New Zealand and New Caledonia; Madagascar; the northern Mascarene Plateau, which includes the Seychelles. Other islands, such as several in the Caribbean Sea, are composed largely of granitic rock as well, but all continents contain both granitic and basaltic crust, and there is no clear boundary as to which islands would be considered microcontinents under such a definition. The Kerguelen Plateau, for example, is largely volcanic, but is associated with the breakup of Gondwanaland and is considered a microcontinent, whereas volcanic Iceland and Hawaii are not. The British Isles, Sri Lanka, Borneo, and Newfoundland are margins of the Laurasian continent—only separated by inland seas flooding its margins.

text: There are many

text: microcontinents, or continental fragments

text: , that are built of continental crust but do not contain a craton. Some of these are fragments of

text: Gondwana

text: or other ancient cratonic continents:

text: Zealandia

text: , which includes

text: New Zealand

text: and

text: New Caledonia

text: Madagascar

text: ; the northern

text: Mascarene Plateau

text: , which includes the

text: Seychelles

text: . Other islands, such as several in the

text: Caribbean Sea

text: , are composed largely of granitic rock as well, but all continents contain both granitic and basaltic crust, and there is no clear boundary as to which islands would be considered microcontinents under such a definition. The

text: Kerguelen Plateau

text: , for example, is largely volcanic, but is associated with the breakup of Gondwanaland and is considered a microcontinent, whereas volcanic

text: Iceland

text: and

text: Hawaii

text: are not. The

text: British Isles

text: Sri Lanka

text: Borneo

text: , and

text: Newfoundland

text: are margins of the

text: Laurasia

text: n continent—only separated by inland seas flooding its margins.

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answers: basaltic

answers: NDQ_005572

answers: Gondwana

answers: NDQ_005573

answers: ancient

answers: NDQ_005574

answers: are built of continental crust but do not contain a craton

answers: NDQ_005575

answers: cratonic continents

answers: NDQ_005576

answers: craton

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Gondwana

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: When passenger car doors are located only at the ends of each car (a common design for commuter rail and long-distance trains), platform access from a concave platform is preferred, since this brings the car ends in closest proximity to the platform edge.  By contrast, a convex platform would leave the largest possible gaps between the car ends and the platform edge, making this design undesirable and thus rarely implemented. An example of platforms designed for access from the concave side is at Yawkey station in Boston, where side platforms for both the inbound and outbound directions are located to reduce platform gaps to commuter rail trains of the Framingham/Worcester Line. Concave and convex gaps also exist in several MTR stations in Hong Kong, particularly on the East Rail Line, which was built on the historic Kowloon-Canton Railway line.

text: When passenger car doors are located only at the ends of each car (a common design for

text: commuter rail

text: and long-distance trains), platform access from a

text: concave

text: platform is preferred, since this brings the car ends in closest proximity to the platform edge.  By contrast, a

text: convex

text: platform would leave the largest possible gaps between the car ends and the platform edge, making this design undesirable and thus rarely implemented. An example of platforms designed for access from the concave side is at

text: Yawkey

text: station in

text: Boston

text: , where

text: side platform

text: s for both the inbound and outbound directions are located to reduce platform gaps to commuter rail trains of the

text: Framingham/Worcester Line

text: . Concave and convex gaps also exist in several

text: MTR

text: stations in Hong Kong, particularly on the

text: East Rail Line

text: , which was built on the historic

text: Kowloon-Canton Railway

text: line.

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text: A shield always accompanied a sword as part of the swordsman's equipment. Carried on the left arm, or when out of use, slung over the shoulder, shields were made of steel or hide and were generally from  in diameter. If made of steel they were often highly ornamented with patterns in gold damascening while hide shields bore silver or gold bosses, crescents, or stars. Shields were made of sambar deer, buffalo, nilgai, elephant, or rhinoceros hide, the last being the most highly prized. Brahmans, who objected to leather, had shields made from forty or fifty folds of silk painted red and ornamented, lined with velvet or snakeskin. While shields can be used to block sword attacks, in South Asia they are more often used offensively as an impact weapon or pushed against the opponent to prevent them from attacking, in addition to deflecting projectiles. A dagger is often held in the same hand, protruding from under the shield.

text: A shield always accompanied a sword as part of the swordsman's equipment. Carried on the left arm, or when out of use, slung over the shoulder, shields were made of steel or hide and were generally from  in diameter. If made of steel they were often highly ornamented with patterns in gold

text: damascening

text: while hide shields bore silver or gold bosses, crescents, or stars. Shields were made of

text: sambar deer

text: , buffalo,

text: nilgai

text: elephant

text: , or

text: rhinoceros

text: hide, the last being the most highly prized. Brahmans, who objected to leather, had shields made from forty or fifty folds of silk painted red and ornamented, lined with velvet or snakeskin. While shields can be used to block sword attacks, in South Asia they are more often used offensively as an impact weapon or pushed against the opponent to prevent them from attacking, in addition to deflecting projectiles. A dagger is often held in the same hand, protruding from under the shield.

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answers: steel

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answer: No

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answer: 1

text: The New Caledonian archipelago is a microcontinental island chain which originated as a fragment of Zealandia, a nearly submerged continent or microcontinent which was part of the southern supercontinent of  Gondwana during the time of the dinosaurs. The Grande Terre group of New Caledonia, with Mont Panié at  as its highest point, is the most elevated part of the Norfolk Ridge, a long and mostly underwater arm of the continent.  While they were still one landmass, Zealandia and Australia combined broke away from Antarctica between 85 and 130 million years ago. Australia and Zealandia split apart 60–85 million years ago. Although biologists consider it contrary to the evidence of surviving Gondwanan lineages, geologists consider the logical possibility that Zealandia may have been completely submerged about 23 million years ago. While a continent like Australia consists of a large body of land surrounded by a fringe of continental shelf, Zealandia consists almost entirely of continental shelf, with the vast majority, some 93%, submerged beneath the Pacific Ocean.  This viewpoint is not universal. Bernard Pelletier argues that Grande Terre was completely submerged for millions of years, and hence the origin of the flora may not be local in nature, but due to long distance-dispersal.

text: The New Caledonian archipelago is a

text: microcontinental island chain

text: which originated as a fragment of

text: Zealandia

text: , a nearly submerged

text: continent

text: or

text: microcontinent

text: which was part of the southern

text: supercontinent

text: of

text: Gondwana

text: during the

text: time of the dinosaurs

text: . The Grande Terre group of New Caledonia, with

text: Mont Panié

text: at  as its highest point, is the most elevated part of the

text: Norfolk Ridge

text: , a long and mostly underwater arm of the continent.  While they were still one landmass, Zealandia and Australia combined broke away from

text: Antarctica

text: between 85 and 130

text: million years ago

text: . Australia and Zealandia split apart 60–85 million years ago. Although biologists consider it contrary to the evidence of surviving Gondwanan lineages, geologists consider the logical possibility that Zealandia may have been completely submerged about 23 million years ago. While a continent like Australia consists of a large body of land surrounded by a fringe of continental shelf, Zealandia consists almost entirely of continental shelf, with the vast majority, some 93%, submerged beneath the

text: Pacific Ocean

text: .  This viewpoint is not universal. Bernard Pelletier argues that Grande Terre was completely submerged for millions of years, and hence the origin of the flora may not be local in nature, but due to long distance-dispersal.

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text: A shield is held in the hand or arm. Its purpose is to intercept attacks, either by stopping projectiles such as arrows or by glancing a blow to the side of the shield-user. Shields vary greatly in size, ranging from large shields that protect the user's entire body to small shields that are mostly for use in hand-to-hand combat. Shields also vary a great deal in thickness; whereas some shields were made of thick wooden planking, to protect soldiers from spears and crossbow bolts, other shields were thinner and designed mainly for glancing blows away (such as a sword blow). In prehistory, shields were made of wood, animal hide, or wicker. In antiquity and in the Middle Ages, shields were used by foot soldiers and mounted soldiers. Even after the invention of gunpowder and firearms, shields continued to be used. In the 18th century, Scottish clans continued to use small shields, and in the 19th century, some non-industrialized peoples continued to use shields. In the 20th and 21st century, shields are used by military and police units that specialize in anti-terrorist action, hostage rescue, and siege-breaching.

text: A

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text: The U.S. Route shield is the highway marker used for United States Numbered Highways. Since the first U.S. Route signs were installed in 1926, the general idea has remained the same, but many changes have been made in the details. Originally, the shield included the name of the state in which the sign was erected and the letters "U S" on a shield-shaped sign. Over time, the shield has been simplified to consist of a white shield outline on a black square background, containing only a black route number. However, because each state is responsible for the production and maintenance of U.S. route shields, several variants of the shield have existed over the years.

text: The U.S. Route shield is the

text: highway marker

text: used for

text: United States Numbered Highways

text: . Since the first U.S. Route signs were installed in 1926, the general idea has remained the same, but many changes have been made in the details. Originally, the shield included the name of the state in which the sign was erected and the letters "U S" on a shield-shaped sign. Over time, the shield has been simplified to consist of a white shield outline on a black square background, containing only a black route number. However, because each state is responsible for the production and maintenance of U.S. route shields, several variants of the shield have existed over the years.

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answer: No

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text: The Withoutabox website offers filmmakers a platform to search over 3000 film festivals on five continents and to submit their films to over 850 film festivals worldwide, including festivals such as Sundance and the Toronto International Film Festival.

text: The Withoutabox website offers filmmakers a platform to search over 3000 film festivals on five continents and to submit their films to over 850 film festivals worldwide, including festivals such as

text: Sundance

text: and the

text: Toronto International Film Festival

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text: The northern plain contains the old geological continent of Baltica, and so may be regarded geologically as the "main continent", while peripheral highlands and mountainous regions in the south and west constitute fragments from various other geological continents. Most of the older geology of western Europe existed as part of the ancient microcontinent Avalonia.

text: The northern plain contains the old geological continent of

text: Baltica

text: , and so may be regarded geologically as the "main continent", while peripheral highlands and mountainous regions in the south and west constitute fragments from various other geological continents. Most of the older geology of western Europe existed as part of the ancient

text: microcontinent

text: Avalonia

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answers: Avalonia

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answers: Baltica

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answers: Avalonia

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answers: Baltica

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answers: mountainous regions

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answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: ancient microcontinent Avalonia

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Granites and detrital zircons have notably similar and episodic appearances in the rock record. Their fluctuations correlate with Precambrian supercontinent cycles. The U–Pb zircon dates from orogenic granites are of the most reliable aging determinants. Some issues exist with relying on granite sourced zircons, such as a lack of evenly globally sourced data and the loss of granite zircons by sedimentary coverage or plutonic consumption. Where granite zircons are less adequate, detrital zircons from sandstones appear and make up for the gaps. These detrital zircons are taken from the sands of major modern rivers and their drainage basins. Oceanic magnetic anomalies and paleomagnetic data are the primary resources used for reconstructing continent and supercontinent locations back to roughly 150 Ma.

text: Granites

text: and detrital

text: zircon

text: s have notably similar and episodic appearances in the rock record. Their fluctuations correlate with Precambrian supercontinent cycles. The U–Pb

text: zircon

text: dates from orogenic granites are of the most reliable aging determinants. Some issues exist with relying on granite sourced zircons, such as a lack of evenly globally sourced data and the loss of granite zircons by sedimentary coverage or

text: pluton

text: ic consumption. Where granite zircons are less adequate, detrital zircons from

text: sandstone

text: s appear and make up for the gaps. These detrital zircons are taken from the sands of major modern rivers and their drainage basins. Oceanic magnetic anomalies and paleomagnetic data are the primary resources used for reconstructing continent and supercontinent locations back to roughly 150 Ma.

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answers: Precambrian

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answers: supercontinents

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answers: 150 Ma

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answers: supercontinent

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answers: detrital zircons are taken from the sands of major modern rivers and their drainage basins

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: During September 17, both TCWC Jakarta and the JTWC reported that an area of convection had persisted about , to the south east of Sumatra in Indonesia. Satellite imagery was showing that the convection was slowly starting to consolidate with a well defined low level circulation centre off the western coast of Sumatra. However it was not expected to develop any further due to being in area of high vertical wind shear in excess of . Despite this it was designated as a tropical low early the next day by TCWC Perth. The JTWC then declared early the next day that the disturbance had dissipated as it crossed 90E and moved into RSMC La Reunion's area of responsibility. TCWC Perth continued to monitor the tropical low as it slowly developed further until early on September 20 when RSMC La Reunion designated it as the second Zone of Disturbed Weather of the 2009–10 as convection had developed over the system and the amount of vertical wind shear over the system had dropped. However they released their final advisory later that day as convection had dissipated in the northern quadrants of the system.

text: During September 17, both TCWC Jakarta and the JTWC reported that an area of convection had persisted about , to the south east of

text: Sumatra

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answers: volcanic

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answers: low level circulation centre

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answers: The presence of zircons in ancient rocks indicates that there was water in the environment

answers: NDQ_005579

answers: 2009–10

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: The rocks in the Rocky Mountains were formed before the mountains were raised by tectonic forces. The oldest rock is Precambrian metamorphic rock that forms the core of the North American continent. There is also Precambrian sedimentary argillite, dating back to 1.7 billion years ago. During the Paleozoic, western North America lay underneath a shallow sea, which deposited many kilometers of limestone and dolomite.

text: The rocks in the Rocky Mountains were formed before the mountains were raised by tectonic forces. The oldest rock is

text: Precambrian

text: metamorphic rock

text: that forms the core of the North American continent. There is also Precambrian sedimentary

text: argillite

text: , dating back to 1.7 billion years ago. During the

text: Paleozoic

text: , western North America lay underneath a shallow sea, which deposited many kilometers of

text: limestone

text: and

text: dolomite

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answers: Precambrian

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answers: Precambrian

answers: NDQ_005573

answers: a shallow sea

answers: NDQ_005574

answers: tectonic forces

answers: NDQ_005575

answers: 1.7 billion years ago

answers: NDQ_005576

answers: argillite

answers: NDQ_005577

answers: During the Paleozoic

answers: NDQ_005579

answers: Paleozoic

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: There are five global platforms and four regional platforms. The regional platforms are only sold in some continents and not others. These platforms are:

text: There are five global platforms and four regional platforms. The regional platforms are only sold in some continents and not others. These platforms are:

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text: According to the Fellowship, the Lemurian Philosophy was revealed to Stelle by highly advanced men and women, called Masters or Elder Brothers. The Philosophy is said to have formed the foundation of the so-called Mukulian civilization on the legendary continent of Mu (also known as Lemuria) now covered by the Pacific Ocean. This lost continent is considered incompatible with the theory of plate tectonics, the standard theory describing movement of the earth's lithosphere accepted by most, but not all, earth scientists. Nonetheless, the Lemurian Philosophy points to various megalithic structures and other features on various Pacific Islands, and in South America and Asia, as indications that the continent and an advanced civilization did at one time exist.

text: According to the Fellowship, the Lemurian Philosophy was revealed to Stelle by highly advanced men and women, called Masters or Elder Brothers. The Philosophy is said to have formed the foundation of the so-called Mukulian

text: civilization

text: on the legendary

text: continent

text: of Mu (also known as

text: Lemuria

text: ) now covered by the Pacific Ocean. This

text: lost continent

text: is considered incompatible with the

text: theory

text: of

text: plate tectonics

text: , the standard theory describing movement of the

text: earth

text: 's

text: lithosphere

text: accepted by most, but not all,

text: earth scientists

text: . Nonetheless, the Lemurian Philosophy points to various

text: megalith

text: ic structures and other features on various

text: Pacific Islands

text: , and in South America and Asia, as indications that the continent and an advanced civilization did at one time exist.

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answers: advanced civilization did at one time exist

answers: NDQ_005574

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answers: continent

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answers: Zircons indicate that there was water in the environment

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answers: Lemurian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The common side of the €0.01, €0.02 and €0.05 coins depict the denomination, the words 'EURO CENT' beside it, twelve stars and Europe highlighted on a globe in relation to Asia and Africa in the world. The common side of the €0.10, €0.20 and €0.50 coins currently depict the denomination on the right, the words 'EURO CENT' underneath it, with twelve stars and the European continent on the left. Coins minted from 1999 to 2006 depicted only the EU15, rather than the entire European continent, which is on coins minted after 2007. The common side of the €1 and €2 coins depict the denomination on the left, the currency, map of Europe and twelve stars on the right. Similarly, coins minted from 1999 to 2006 depicted the EU15, rather than the whole European continent, which is on coins minted from 2007.

text: The common side of the €0.01, €0.02 and €0.05 coins depict the denomination, the words 'EURO CENT' beside it, twelve stars and Europe highlighted on a globe in relation to

text: Asia

text: and

text: Africa

text: in the world. The common side of the €0.10, €0.20 and €0.50 coins currently depict the denomination on the right, the words 'EURO CENT' underneath it, with twelve stars and the

text: European continent

text: on the left. Coins minted from 1999 to 2006 depicted only the EU15, rather than the entire European continent, which is on coins minted after 2007. The common side of the €1 and €2 coins depict the denomination on the left, the currency, map of Europe and twelve stars on the right. Similarly, coins minted from 1999 to 2006 depicted the EU15, rather than the whole European continent, which is on coins minted from 2007.

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answers: NDQ_005571

answers: igneous

answers: NDQ_005572

answers: Europe

answers: NDQ_005573

answers: European continent

answers: NDQ_005574

answers: Euro CENT

answers: NDQ_005575

answers: European continent

answers: NDQ_005576

answers: Coins minted from 1999 to 2006 depicted the EU15, rather than the whole European continent, which is on coins minted from 2007.

answers: NDQ_005577

answers: The presence of zircons in ancient rocks indicates that there was water in the environment.

answers: NDQ_005579

answers: 2006

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: It is generally agreed that two of the terranes, the Meguma and Avalon were once part of Gondwana. Proof of Avalon being part of Gondwana exists because of trilobite fossils of the same species that have been found both in Massachusetts and Africa. This means that Avalon must have broken away from Gondwana during the end of the Precambrian, around 550 million years ago. At the very latest, it broke away by the Ordovician, around 490 million years ago. Fossils of the Meguma terrane also indicate a relation to the northwest Africa margin. The Avalon also originated as a volcanic island chain near the South Pole, on the fringe of the Gondwanan supercontinent. It is possible that late Precambrian quartzites of the eastern part of the state were deposited as beach sands on the continental shelf of Gondwana. These deposits were eventually caught in the Avalonian mountain building event, the same deformation which helped to form the Avalonian island chain.

text: It is generally agreed that two of the terranes, the Meguma and Avalon were once part of

text: Gondwana

text: . Proof of Avalon being part of Gondwana exists because of

text: trilobite

text: fossils of the same species that have been found both in

text: Massachusetts

text: and

text: Africa

text: . This means that Avalon must have broken away from Gondwana during the end of the

text: Precambrian

text: , around 550 million years ago. At the very latest, it broke away by the

text: Ordovician

text: , around 490 million years ago. Fossils of the Meguma terrane also indicate a relation to the northwest Africa margin. The Avalon also originated as a volcanic island chain near the

text: South Pole

text: , on the fringe of the Gondwanan supercontinent. It is possible that late

text: Precambrian

text: quartzites of the eastern part of the state were deposited as beach sands on the continental shelf of Gondwana. These deposits were eventually caught in the Avalonian mountain building event, the same deformation which helped to form the Avalonian island chain.

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answers: Gondwanan

answers: NDQ_005572

answers: Gondwana

answers: NDQ_005573

answers: Gondwana

answers: NDQ_005574

answers: Avalon

answers: NDQ_005575

answers: 550 million years ago

answers: NDQ_005576

answers: terranes

answers: NDQ_005577

answers: trilobite fossils

answers: NDQ_005579

answers: the end of the Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Kenneth originated from an area full of unsettled weather that developed off the coast of Guatemala on November 16. A low-pressure area formed shortly thereafter, and organization of the system began to improve on November 17 as it moved westward. The low remained over an area with favorable conditions for formation on November 18, although convective activity tapered slightly later during the day as it began to curve west-northwestward. The system continued to coalesce overnight, and the circulation of the low was more prominent by the following morning. By November 19, the disturbance had gained enough organization to be declared as a tropical depression, the thirteenth of the season. The following day, the depression continued to intensify, and was upgraded to a tropical storm, receiving the name Kenneth. Rapid strengthening began on November 21, and Kenneth was upgraded to a hurricane. As rapid intensification continued, Kenneth strengthened into a Category 3 major hurricane with sustained winds of 125 mph on November 22. Rapid intensification continued and the storm was upgraded to a Category 4 hurricane with sustained winds of 145 mph, just a few hours later, as Kenneth reached its peak intensity. The cause for this rapid intensification just days before the end of the season was unclimatologically low wind shear as well as unusually warm waters directly in the storm's path. However, Kenneth's intensification was short-lived; immediately it moved into an environment of colder waters and stronger wind shear, and started to rapidly deteriorate. Just 24 hours after the cyclone reached its peak, it dropped below hurricane strength and lost most of its central convection. Afterwards, Kenneth weakened at a slower rate, but by November 25, had weakened to a tropical depression, losing almost all of its convection. Early on November 25, Kenneth weakened to a remnant low, with its circulation void of any strong convection. But for the next 3 days, the remnant of the storm continued moving northwestward rapidly as a convectionless vortex, before dissipating completely early on November 28.

text: Kenneth originated from an area full of unsettled weather that developed off the coast of

text: Guatemala

text: on November 16. A

text: low-pressure area

text: formed shortly thereafter, and organization of the system began to improve on November 17 as it moved westward. The low remained over an area with favorable conditions for formation on November 18, although

text: convective activity

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

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answers: limestone

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answers: unclimatologically low

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answers: Category 4 hurricane

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answers: Category 4 hurricane

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answers: Category 4 hurricane with sustained winds of 145 mph

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answers: warm waters directly in the storm's path

answers: NDQ_005579

answers: unclimatologically

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Earth of the early Archean () may have had a different tectonic style. During this time, the Earth's crust cooled enough that rocks and continental plates began to form. Some scientists think because the Earth was hotter, that plate tectonic activity was more vigorous than it is today, resulting in a much greater rate of recycling of crustal material. This may have prevented cratonisation and continent formation until the mantle cooled and convection slowed down. Others argue that the subcontinental lithospheric mantle is too buoyant to subduct and that the lack of Archean rocks is a function of erosion and subsequent tectonic events.

text: The Earth of the early Archean () may have had a different tectonic style. During this time, the Earth's

text: crust

text: cooled enough that rocks and continental plates began to form. Some scientists think because the Earth was hotter, that plate tectonic activity was more vigorous than it is today, resulting in a much greater rate of recycling of crustal material. This may have prevented cratonisation and continent formation until the

text: mantle

text: cooled and convection slowed down. Others argue that the subcontinental lithospheric mantle is too buoyant to

text: subduct

text: and that the lack of Archean rocks is a function of

text: erosion

text: and subsequent

text: tectonic

text: events.

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answers: mantle

answers: NDQ_005572

answers: early Archean

answers: NDQ_005573

answers: The Earth of the early Archean

answers: NDQ_005574

answers: continental plates

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answers: Archean

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answers: continental plates

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answers: Zircons in ancient rocks indicate that there was water in the environment

answers: NDQ_005579

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answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Bruni d'Entrecasteaux, Jean-Michel Huon de Kermadec, Louis Antoine de Bougainville, Jules Dumont d'Urville, Nicolas Baudin, François Péron and Marc-Joseph Marion du Fresne were some of the early European explorers to reach the continent.

text: Bruni d'Entrecasteaux

text: Jean-Michel Huon de Kermadec

text: Louis Antoine de Bougainville

text: Jules Dumont d'Urville

text: Nicolas Baudin

text: François Péron

text: and

text: Marc-Joseph Marion du Fresne

text: were some of the early European explorers to reach the continent.

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answers: NDQ_005577

answers: Zircons

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answers: early European explorers

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: During the Precambrian, when life on land was precluded by a very thin or nonexistent ozone layer, soils were subject to much more rapid erosion and most fossils from this period are of undeveloped entisols or inceptisols. Vertisols and aridisols have a continuous fossil record from Paleoproterozoic continents onwards (though little is known about when they were first vegetated), whilst a few andisol fossils are known from the Mesoproterozoic and more abundantly from the Ordovician just before land vegetation began to emerge. Other major andisol fossils can be found in the middle Jurassic of Siberia.

text: During the

text: Precambrian

text: , when life on land was precluded by a very thin or nonexistent

text: ozone layer

text: , soils were subject to much more rapid erosion and most fossils from this period are of undeveloped

text: entisol

text: s or

text: inceptisols

text: Vertisol

text: s and

text: aridisols

text: have a continuous fossil record from

text: Paleoproterozoic

text: continent

text: s onwards (though little is known about when they were first vegetated), whilst a few

text: andisol

text: fossils are known from the

text: Mesoproterozoic

text: and more abundantly from the

text: Ordovician

text: just before land vegetation began to emerge. Other major andisol fossils can be found in the middle

text: Jurassic

text: of

text: Siberia

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answers: NDQ_005571

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answers: 0

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answers: 0

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answers: 0

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answers: Ordovician

answers: NDQ_005572

answers: Ordovician

answers: NDQ_005573

answers: a very thin or nonexistent ozone layer

answers: NDQ_005574

answers: Siberia

answers: NDQ_005575

answers: life on land

answers: NDQ_005576

answers: ozone layer

answers: NDQ_005577

answers: Vertisols

answers: NDQ_005579

answers: the Precambrian

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: LSW properties experience seasonal and interannual variations.  In late spring and summer, large amounts of cold freshwater accumulate from melting ice and are mixed downward during convection.  The source for heat in the Labrador Sea is modified North Atlantic Current water after circulating the subpolar gyre.   In winter the sea becomes more saline as freshwater freezes to form sea ice.  The greatest seasonal variability is largely confined to the surface waters, however an annual cycle of convective mixing and re-stratification is observed throughout the water column.  Warming and increased salinity in the lower level and freshening at the surface is associated with re-stratification (May–December), whereas a convective mixing period (January–April) leads to cooling and a decrease in salt content in intermediate and deep waters and an increase in salt content at the surface.  Interannual variations in the intermediate LSW are due largely to changes in convectivity throughout these periods.  Weak convective periods are associated with more heat in the water column and deep convective periods are characterized by cold water.  In the early 1990s, several consecutive severe winters contributed towards deep convection in the Labrador Sea.  These winters were also associated with strong positive fluctuations in the North Atlantic Oscillation.  LSW became very cold, fresh, and dense during this period, and the layer extended to depths of 2300m in the spring of 1994.  Due to weakened convection, LSW began warming significantly and increased in salinity over the following decade.  This trend continued through 2010 and 2011 when weak convection was observed in relation with negative NAO.  Deep convection was observed again in 2012 with the LSW reaching 1400m, corresponding with a positive NAO similar to those seen in the early 1990s.

text: LSW properties experience seasonal and interannual variations.  In late spring and summer, large amounts of cold freshwater accumulate from melting ice and are mixed downward during convection.  The source for heat in the Labrador Sea is modified North Atlantic Current water after circulating the

text: subpolar gyre

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answers: NDQ_005571

answers: gneiss

answers: NDQ_005572

answers: North Atlantic Oscillation

answers: NDQ_005573

answers: convection

answers: NDQ_005574

answers: North Atlantic Oscillation

answers: NDQ_005575

answers: Labrador Sea

answers: NDQ_005576

answers: Labrador Sea

answers: NDQ_005577

answers: water

answers: NDQ_005579

answers: the early 1990s

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: As with the rest of Madagascar, the rocks of Marojejy National Park were once part of the supercontinent of Gondwana, which began to break up 160 million years ago to form the southern continents.  However, the bedrock of Marojejy formed over 500 million years ago during the Precambrian beneath an ancient mountain range that has since eroded away completely.  The bedrock is composed mostly of granitic rocks, although it also contains a significant amount of gneiss, a high-grade metamorphic rock that formed under high pressure and temperature deep beneath the ancient mountain range.  In places where heat and pressure were highest, the rock melted completely and eventually recrystallized at depth as granite, an igneous rock.  Later, veins of quartz formed in cracks in the bedrock; these are the source of the quartz and amethyst crystals mined in the region today.  In more recent geological times, the area's abundant quartzite formed when quartz-rich sands were deposited on the bedrock, and were then buried and recrystallized (metamorphosed).  The soil pH is expected to be acidic to neutral.

text: As with the rest of Madagascar, the rocks of Marojejy National Park were once part of the

text: supercontinent

text: of

text: Gondwana

text: , which began to break up 160 million years ago to form the southern continents.  However, the

text: bedrock

text: of Marojejy formed over 500 million years ago during the

text: Precambrian

text: beneath an ancient mountain range that has since eroded away completely.  The bedrock is composed mostly of

text: granitic

text: rocks, although it also contains a significant amount of

text: gneiss

text: , a

text: high-grade

text: metamorphic rock

text: that formed under high pressure and temperature deep beneath the ancient mountain range.  In places where heat and pressure were highest, the rock melted completely and eventually recrystallized at depth as granite, an

text: igneous rock

text: .  Later,

text: veins

text: of

text: quartz

text: formed in cracks in the bedrock; these are the source of the quartz and

text: amethyst

text: crystals mined in the region today.  In more recent geological times, the area's abundant

text: quartzite

text: formed when quartz-rich sands were deposited on the bedrock, and were then buried and recrystallized (

text: metamorphosed

text: ).  The

text: soil pH

text: is expected to be acidic to neutral.

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answers: granitic

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answers: Gondwana

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answers: high pressure and temperature

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answers: mountain range

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answers: 500 million years ago

answers: NDQ_005576

answers: mountain range

answers: NDQ_005577

answers: quartz-rich sands

answers: NDQ_005579

answers: the Precambrian

answer: No

answer: No

answer: Yes

answer: No

answer: Yes

answer: 1

text: Much of the East Antarctic craton was formed in the Precambrian period by a series of tectonothermal orogenic events. Napier orogeny formed the cratonic nucleus approximately 4 billion years ago. Mount Elkins is a classic example of Napier orogeny. Napier orogeny is characterized by high-grade metamorphism and plate tectonics. The orogenic events which resulted in the formation of the Napier Complex (including Mount Elkins) have been dated to the Archean Eon. Radiometrically dated to as old as 3.8 billion years, some of the zircons collected from the orthogneisses of the Napier Complex are among the oldest rock specimens found on Earth. Billions of years of erosion and tectonic deformation have exposed the metamorphic rock core of these ancient mountains.

text: Much of the

text: East Antarctic craton

text: was formed in the

text: Precambrian

text: period by a series of tectonothermal

text: orogenic

text: events. Napier orogeny formed the cratonic nucleus approximately 4 billion years ago. Mount Elkins is a classic example of Napier orogeny. Napier orogeny is characterized by high-grade

text: metamorphism

text: and

text: plate tectonics

text: . The orogenic events which resulted in the formation of the Napier Complex (including Mount Elkins) have been dated to the

text: Archean

text: Eon

text: Radiometrically dated

text: to as old as 3.8 billion years, some of the

text: zircon

text: s collected from the

text: orthogneisses

text: of the Napier Complex are among the

text: oldest rock specimens

text: found on Earth. Billions of years of

text: erosion

text: and

text: tectonic deformation

text: have exposed the

text: metamorphic rock

text: core of these ancient mountains.

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answers: NDQ_005571

answers: orthogneisses

answers: NDQ_005572

answers: Napier orogeny

answers: NDQ_005573

answers: radiometrically dated

answers: NDQ_005574

answers: mountains

answers: NDQ_005575

answers: 4 billion years ago

answers: NDQ_005576

answers: Napier Complex

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: the Precambrian period

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: The Great Falls tectonic zone was first identified in 1985. Geologists originally believed the zone was part of the Wyoming craton, but now conclude that it is distinct from it. There is continuing controversy over whether the region is a shear zone or suture, and the role the zone played in the formation of the North American continent. At one time, both the Great Falls Tectonic Zone and the Vulcan structure were both considered sutures, but debate remains open on the point. At least one group of geologists has concluded the zone represents the closure of an ocean basin. The zone lacks gravity anomalies or electromagnetic signatures which would allow scientists to conclude that it was generated by subduction. There is significant evidence that the zone has been periodically remineralized since Precambrian times. Square Butte, Shaw Butte, Crown Butte and the other structures of the Adel Mountains Volcanic Field lie astride the tectonic zone near the city of Great Falls.

text: The Great Falls tectonic zone was first identified in 1985. Geologists originally believed the zone was part of the Wyoming craton, but now conclude that it is distinct from it. There is continuing controversy over whether the region is a shear zone or

text: suture

text: , and the role the zone played in the formation of the North American continent. At one time, both the Great Falls Tectonic Zone and the

text: Vulcan structure

text: were both considered sutures, but debate remains open on the point. At least one group of geologists has concluded the zone represents the closure of an ocean basin. The zone lacks

text: gravity anomalies

text: or electromagnetic signatures which would allow scientists to conclude that it was generated by

text: subduction

text: . There is significant evidence that the zone has been periodically

text: remineralized

text: since

text: Precambrian

text: times. Square Butte, Shaw Butte, Crown Butte and the other structures of the

text: Adel Mountains Volcanic Field

text: lie astride the tectonic zone near the city of

text: Great Falls

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answers: Wyoming craton

answers: NDQ_005572

answers: Wyoming craton

answers: NDQ_005573

answers: precambrian times

answers: NDQ_005574

answers: Wyoming craton

answers: NDQ_005575

answers: the zone has been periodically remineralized

answers: NDQ_005576

answers: tectonic zone

answers: NDQ_005577

answers: The zone lacks gravity anomalies or electromagnetic signatures

answers: NDQ_005579

answers: Precambrian times

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Between 1998 and 2006 Shields became a frequent collaborator and semi-permanent touring member of Primal Scream. He contributed guitar, produced and mixed tracks on two of the band's studio albums: XTRMNTR (2000), and Evil Heat (2002). Primal Scream frontman Bobby Gillespie has said that "[Shields] brings something that nobody else in the world can bring. He plays guitar the way that nobody else in the world plays guitar," adding that Primal Scream considered Shields to be "part of the family, very much so." Shields has remained close to the band following his departure in 2006, remastering Primal Scream's third studio album Screamadelica (1991) in 2010 and contributing guitar to "2013", the lead single from More Light (2013). Gillespie has since commented on Shields' absence, noting that "there's always room for Kevin Shields—always."

text: Between 1998 and 2006 Shields became a frequent collaborator and semi-permanent touring member of

text: Primal Scream

text: . He contributed guitar, produced and mixed tracks on two of the band's studio albums:

text: XTRMNTR

text: (2000), and

text: Evil Heat

text: (2002). Primal Scream frontman

text: Bobby Gillespie

text: has said that "[Shields] brings something that nobody else in the world can bring. He plays guitar the way that nobody else in the world plays guitar," adding that Primal Scream considered Shields to be "part of the family, very much so." Shields has remained close to the band following his departure in 2006, remastering Primal Scream's third studio album

text: Screamadelica

text: (1991) in 2010 and contributing guitar to "2013", the lead single from

text: More Light

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text: General elections were held in Namibia on 28 November 2014, although early voting took place in foreign polling stations and for seagoing personnel on 14 November. The elections were the first on the African continent to use electronic voting.

text: General elections were held in

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text: on 28 November 2014, although early voting took place in

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text: The conditions for diamond formation to happen in the lithospheric mantle occur at considerable depth corresponding to the requirements of temperature and pressure. These depths are estimated between  though occasionally diamonds have crystallized at depths about . The rate at which temperature changes with increasing depth into the Earth varies greatly in different parts of the Earth. In particular, under oceanic plates the temperature rises more quickly with depth, beyond the range required for diamond formation at the depth required. The correct combination of temperature and pressure is only found in the thick, ancient, and stable parts of continental plates where regions of lithosphere known as cratons exist. Long residence in the cratonic lithosphere allows diamond crystals to grow larger.

text: The conditions for diamond formation to happen in the lithospheric mantle occur at considerable depth corresponding to the requirements of temperature and pressure. These depths are estimated between  though occasionally diamonds have crystallized at depths about . The rate at which

text: temperature changes with increasing depth

text: into the Earth varies greatly in different parts of the Earth. In particular, under oceanic plates the temperature rises more quickly with depth, beyond the range required for diamond formation at the depth required. The correct combination of temperature and pressure is only found in the thick, ancient, and stable parts of continental plates where regions of lithosphere known as

text: craton

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text: Situated on the Canadian Shield, the city is surrounded by dense forest, muskeg swamps, numerous lakes, winding rivers, and hills of Precambrian bedrock. The local forests are mixed deciduous and coniferous, with colourful displays in the autumn.

text: Situated on the

text: Canadian Shield

text: , the city is surrounded by dense forest, muskeg swamps, numerous lakes, winding rivers, and hills of Precambrian bedrock. The local forests are mixed deciduous and coniferous, with colourful displays in the autumn.

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answer: No

answer: No

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text: Nilpenia rossi is a Precambrian fossil genus.

text: Nilpenia rossi is a

text: Precambrian

text: fossil genus.

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answer: No

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text: The South American continent also includes various islands, most of which belong to countries on the continent. The Caribbean territories are grouped with North America. The South American nations that border the Caribbean Sea—including Colombia, Venezuela, Guyana, Suriname, and French Guiana—are also known as Caribbean South America.

text: The South American continent also includes various

text: island

text: s, most of which belong to countries on the continent. The

text: Caribbean

text: territories are grouped with North America. The South American nations that border the Caribbean Sea—including

text: Colombia

text: Venezuela

text: Guyana

text: Suriname

text: , and

text: French Guiana

text: —are also known as

text: Caribbean South America

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text: The program was established in early 1873 during the school's first academic year and played in the Ohio Athletic Conference (OAC) from 1954–1966, the Ohio Valley Conference from 1981 through 1987, and the Mid-Continent Conference for the 1990, 1991, and 1992 seasons. The Zips began competition in the MAC in 1993 and were placed in the East Division when it was created in 2000. The team had one appearance in the NCAA Division I Baseball Championship, which came in 1996 following their only MAC Tournament Championship. Additionally, the Zips won the 1954 OAC championship and the 1991 Mid-Continent Conference title.

text: The program was established in early 1873 during the school's first academic year and played in the

text: Ohio Athletic Conference

text: (OAC) from 1954–1966, the

text: Ohio Valley Conference

text: from 1981 through 1987, and the

text: Mid-Continent Conference

text: for the 1990, 1991, and 1992 seasons. The Zips began competition in the MAC in 1993 and were placed in the East Division when it was created in 2000. The team had one appearance in the

text: NCAA Division I Baseball Championship

text: , which came in

entity_name: 1996 NCAA Division I Baseball Tournament

text: following their only

entity_name: 1996 Mid-American Conference Baseball Tournament

text: MAC Tournament Championship

text: . Additionally, the Zips won the 1954 OAC championship and the 1991 Mid-Continent Conference title.

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text: The term basement is used mostly in disciplines of geology like basin geology, sedimentology and petroleum geology in which the (typically Precambrian) crystalline basement is not of interest as it rarely contains petroleum or natural gas.

text: The term basement is used mostly in disciplines of geology like

text: basin geology

text: sedimentology

text: and

text: petroleum geology

text: in which the (typically

text: Precambrian

text: ) crystalline basement is not of interest as it rarely contains

text: petroleum

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text: natural gas

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answers: crystalline basement

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answers: Precambrian

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answers: Precambrian

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answers: Precambrian

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answers: petroleum or natural gas

answers: NDQ_005576

answers: basement

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Hearne Craton is a craton in northern Canada which, together with the Rae Craton, forms the Western Churchill Province.  Hearne is one of the six Archaean cratons of the Canadian Shield (the other being Slave, Rae, Wyoming, Superior, Nain) that are bound together by Palaeoproterozoic orogenic belts.  Before being merged these six cratons formed independent microcontinents.

text: The Hearne Craton is a

text: craton

text: in northern Canada which, together with the

text: Rae Craton

text: , forms the Western

text: Churchill Province

text: .  Hearne is one of the six Archaean cratons of the

text: Canadian Shield

text: (the other being

text: Slave

text: Rae

text: Wyoming

text: Superior

text: Nain

text: ) that are bound together by Palaeoproterozoic

text: orogenic belt

text: s.  Before being merged these six cratons formed independent

text: microcontinent

text: s.

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answers: NDQ_005571

answers: Archaean

answers: NDQ_005572

answers: Archaean

answers: NDQ_005573

answers: independent microcontinents

answers: NDQ_005574

answers: Hearne Craton

answers: NDQ_005575

answers: Archaean

answers: NDQ_005576

answers: craton

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Archaean

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: The Barberton greenstone belt (BGB) is located in the Kapvaal craton of southeastern Africa. It characterizes one of the most well-preserved and oldest pieces of continental crust today by containing rocks in the Barberton Granite Greenstone Terrain (3.55–3.22 Ga). The BGB is a small, cusp-shaped succession of volcanic and sedimentary rocks, surrounded on all sides by granitoid plutons which range in age from >3547 to <3225 Ma.  It is commonly known as the type locality of the ultramafic, extrusive volcanic rock, the komatiite. Greenstone belts are geologic regions generally composed of mafic to ultramafic volcanic sequences that have undergone metamorphism. These belts are associated with sedimentary rocks that occur within Archean and Proterozoic cratons between granitic bodies. Their name is derived from the green hue that comes from the metamorphic minerals associated with the mafic rocks. These regions are theorized to have formed at ancient oceanic spreading centers and island arcs.  In simple terms, greenstone belts are described as metamorphosed volcanic belts. Being one of the few most well-preserved Archean portions of the crust, the BGB is well studied. It provides present geologic evidence of  Earth during the Archean (pre-3.0 Ga). Despite the BGB being a well studied area, its tectonic evolution has been the cause of much debate.

text: The

text: Barberton greenstone belt

text: (BGB) is located in the

text: Kapvaal craton

text: of southeastern Africa. It characterizes one of the most well-preserved and oldest pieces of

text: continental crust

text: today by containing rocks in the Barberton Granite Greenstone Terrain (3.55–3.22

text: Ga

text: ). The BGB is a small, cusp-shaped succession of volcanic and sedimentary rocks, surrounded on all sides by

text: granitoid

text: pluton

text: s which range in age from >3547 to <3225

text: Ma

text: .  It is commonly known as the type locality of the

text: ultramafic

text: , extrusive volcanic rock, the

text: komatiite

text: Greenstone belts

text: are geologic regions generally composed of

text: mafic

text: to ultramafic volcanic sequences that have undergone

text: metamorphism

text: . These belts are associated with

text: sedimentary rock

text: s that occur within

text: Archean

text: and

text: Proterozoic

text: cratons

text: between granitic bodies. Their name is derived from the green hue that comes from the metamorphic minerals associated with the mafic rocks. These regions are theorized to have formed at ancient

text: oceanic spreading centers

text: and

text: island arcs

text: .  In simple terms, greenstone belts are described as

text: metamorphosed

text: volcanic belt

text: s. Being one of the few most well-preserved Archean portions of the crust, the BGB is well studied. It provides present geologic evidence of  Earth during the Archean (pre-3.0 Ga). Despite the BGB being a well studied area, its tectonic evolution has been the cause of much debate.

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

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answers: 0

answers: NDQ_005571

answers: granitic bodies

answers: NDQ_005572

answers: Archean

answers: NDQ_005573

answers: Earth during the Archean

answers: NDQ_005574

answers: Archean and Proterozoic

answers: NDQ_005575

answers: Archean and Proterozoic cratons

answers: NDQ_005576

answers: Greenstone belts

answers: NDQ_005577

answers: It provides present geologic evidence of Earth during the Archean

answers: NDQ_005579

answers: the Archean

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: Almost all of Northern Australia is a huge ancient craton that has not experienced geological upheaval since the end of the Precambrian. The only exception to this generalisation is the Wet Tropics of northern Queensland, where active volcanoes have been present as recently as the Pleistocene.

text: Almost all of Northern Australia is a huge ancient

text: craton

text: that has not experienced geological upheaval since the end of the

text: Precambrian

text: . The only exception to this generalisation is the

text: Wet Tropics

text: of northern Queensland, where active

text: volcano

text: es have been present as recently as the

text: Pleistocene

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answers: Precambrian

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answers: Precambrian

answers: NDQ_005573

answers: active volcanoes

answers: NDQ_005574

answers: ancient

answers: NDQ_005575

answers: ancient craton

answers: NDQ_005576

answers: craton

answers: NDQ_005577

answers: Wet Tropics

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: The Canadian Shield, also called the Laurentian Plateau, or Bouclier canadien (French), is a large area of exposed Precambrian igneous and high-grade metamorphic rocks (geological shield) that forms the ancient geological core of the North American continent (North American or Laurentia craton). Composed of igneous rock resulting from its long volcanic history, the area is covered by a thin layer of soil. With a deep, common, joined bedrock region in eastern and central Canada, it stretches north from the Great Lakes to the Arctic Ocean, covering over half of Canada; it also extends south into the northern reaches of the United States. Human population is sparse, and industrial development is minimal, while mining is prevalent.

text: The Canadian Shield, also called the Laurentian Plateau, or Bouclier canadien (French), is a large area of exposed

text: Precambrian

text: igneous

text: and

text: high-grade metamorphic rock

text: s (

text: geological shield

text: ) that forms the ancient geological core of the North American continent (

text: North American or Laurentia craton

text: ). Composed of

text: igneous rock

text: resulting from its long volcanic history, the area is covered by a thin layer of

text: soil

text: . With a deep, common, joined

text: bedrock

text: region in eastern and central

text: Canada

text: , it stretches north from the

text: Great Lakes

text: to the

text: Arctic Ocean

text: , covering over half of Canada; it also extends south into the northern reaches of the United States. Human population is sparse, and industrial development is minimal, while mining is prevalent.

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: long volcanic history

answers: NDQ_005574

answers: Laurentia

answers: NDQ_005575

answers: ancient geological core of the North American continent

answers: NDQ_005576

answers: Laurentian Plateau

answers: NDQ_005577

answers: the Great Lakes to the Arctic Ocean

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: The Scotia Plate originated about  (Ma), during the late Mesozoic at the Panthalassic margins of the Gondwana supercontinent between two Precambrian cratons, the Kalahari and East Antarctic Cratons, now located in Africa and Antarctica.  Its development was also influenced by the Río de la Plata Craton in South America.  The initial cause for its formation was the break-up of Gondwana in what became the south-west Indian Ocean.

text: The Scotia Plate originated about  (Ma), during the late

text: Mesozoic

text: at the

text: Panthalassic

text: margins of the

text: Gondwana

text: supercontinent between two Precambrian cratons, the

text: Kalahari

text: and

text: East Antarctic Craton

text: s, now located in Africa and Antarctica.  Its development was also influenced by the

text: Río de la Plata Craton

text: in South America.  The initial cause for its formation was the break-up of Gondwana in what became the south-west Indian Ocean.

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text: , nevertheless, found a three-fold stratigraphic similarity and proposed that the two cratons once formed a continent which he named Vaalbara.  This model is supported by the palaeomagnetic data of .Reconstructions of the palaeolatitudes of the two cratons at 2.78–2.77 Ga are ambiguous however.  In the reconstruction of  they fail to overlap, but they do in more recent reconstructions, for example .

text: , nevertheless, found a three-fold stratigraphic similarity and proposed that the two cratons once formed a continent which he named Vaalbara.  This model is supported by the palaeomagnetic data of .Reconstructions of the palaeolatitudes of the two cratons at 2.78–2.77 Ga are ambiguous however.  In the reconstruction of  they fail to overlap, but they do in more recent reconstructions, for example .

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text: Final Fantasy IX takes place primarily on the four continents of a world named Gaia. Most of Gaia's population reside on the Mist Continent, named so because the entire continent is blanketed in thick Mist. Lands outside the Mist Continent—the Outer, Lost and Forgotten continents—are uncharted territories not explored until midway through the game. Several locations on the parallel world of Terra and the dream land of Memoria round out the game's areas. The Mist Continent features four nations: Alexandria, Lindblum, Burmecia, and Cleyra. Alexandria is a kingdom to the northeast of the Mist Continent ruled by a monarchy located in Alexandria Castle. The technologically advanced Lindblum, ruled by a regent, is nestled on a plateau to the southwest where airships regularly fly by. The Kingdom of Burmecia, whose capital is showered by eternal rain is to the northwest and nearby to the isolated Cleyran civilisation, which is nestled in a giant tree in the desert, protected by a powerful sandstorm. Treno, a large, perpetually dark city, heavily populated by both aristocrats and paupers, is located on the southeast part of the continent. The Mist Continent is extremely mountainous resulting in a natural barrier between many of the ruling nations.

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answers: The Mist Continent is extremely mountainous

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answers: The Mist Continent

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text: The process by which cratons are formed from early rock is called cratonization. The first large cratonic landmasses formed during the Archean eon. During the early Archean, Earth's heat flow was nearly three times higher than it is today because of the greater concentration of radioactive isotopes and the residual heat from the Earth's accretion. There was considerably greater tectonic and volcanic activity; the mantle was less viscous and the crust thinner. This resulted in rapid formation of oceanic crust at ridges and hot spots, and rapid recycling of oceanic crust at subduction zones. There are at least three hypotheses of how cratons have been formed:  1) surface crust was thickened by a rising plume of deep molten material, 2) successive subducting plates of oceanic lithosphere became lodged beneath a proto-craton in an under-plating process, 3) accretion from island arcs or continental fragments rafting together to thicken into a craton.

text: The process by which cratons are formed from early rock is called cratonization. The first large cratonic landmasses formed during the

text: Archean

text: eon. During the early Archean, Earth's heat flow was nearly three times higher than it is today because of the greater concentration of radioactive isotopes and the residual heat from the Earth's

text: accretion

text: . There was considerably greater

text: tectonic

text: and

text: volcanic

text: activity; the

text: mantle

text: was less viscous and the crust thinner. This resulted in rapid formation of

text: oceanic crust

text: at ridges and

text: hot spots

text: , and rapid

text: recycling of oceanic crust

text: at

text: subduction

text: zones. There are at least three hypotheses of how cratons have been formed:  1) surface crust was thickened by a rising plume of deep molten material, 2) successive subducting plates of oceanic lithosphere became lodged beneath a proto-craton in an under-plating process, 3) accretion from island arcs or continental fragments rafting together to thicken into a craton.

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answers: 4

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answers: 4

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answers: early rock

answers: NDQ_005572

answers: Archean

answers: NDQ_005573

answers: There was considerably greater tectonic and volcanic activity

answers: NDQ_005574

answers: are formed from early rock

answers: NDQ_005575

answers: Archean

answers: NDQ_005576

answers: subduction zones

answers: NDQ_005577

answers: rapid formation of oceanic crust at ridges and hot spots

answers: NDQ_005579

answers: early Archean

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: The earthquake's epicenter lay near Manhattan, Kansas, a town just off the connection of the Kansas River and the Big Blue River. Nearby is the anticline Nemaha Ridge, which has been associated with at least a few earthquakes of Kansas. A 300‑million-year-old Precambrian granite range bounded by faults, it hosts the Humboldt Fault Zone, which, in addition to serving as the range's easternmost boundary, has produced a large portion of the state's earthquakes. Each year, it is responsible for at least several small tremors less than magnitude 2.7. It cuts through Permian rock, and according to the Geological Society of America, may actually be a complex fault. Previously, it was believed to be a simple, Precambrian structure.

text: The earthquake's epicenter lay near

text: Manhattan

text: , Kansas, a town just off the connection of the

text: Kansas River

text: and the

text: Big Blue River

text: . Nearby is the

text: anticline

text: Nemaha Ridge

text: , which has been associated with at least a few earthquakes of Kansas. A 300‑million-year-old

text: Precambrian

text: granite range bounded by faults, it hosts the Humboldt Fault Zone, which, in addition to serving as the range's easternmost boundary, has produced a large portion of the state's earthquakes. Each year, it is responsible for at least several small tremors less than magnitude 2.7. It cuts through

text: Permian

text: rock, and according to the Geological Society of America, may actually be a complex

text: fault

text: . Previously, it was believed to be a simple,

text: Precambrian

text: structure.

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Nemaha Ridge

answers: NDQ_005575

answers: 300 million-year

answers: NDQ_005576

answers: Nemaha Ridge

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Paleodictyon is a pattern, usually interpreted to be a burrow, which appears in the geologic marine record beginning in the Precambrian/Early Cambrian and in modern ocean environments. Paleodictyon were first described by Giuseppe Meneghini in 1850.

text: Paleodictyon is a pattern, usually interpreted to be a burrow, which appears in the geologic marine record beginning in the Precambrian/Early Cambrian and in modern ocean environments. Paleodictyon were first described by

text: Giuseppe Meneghini

text: in 1850.

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answers: Precambrian

answers: NDQ_005572

answers: the Precambrian

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answers: Paleodictyon

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answers: paleodictyon

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answers: paleodictyon

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answers: Paleodictyon

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answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: According to J.D.A. Piper, Rodinia is one of two models for the configuration and history of the continental crust in the latter part of Precambrian times. The other is Paleopangea, Piper's own concept.  Piper proposes an alternative hypothesis for this era and the previous ones. This idea rejects that Rodinia ever existed as a transient supercontinent subject to progressive break-up in the latter part of Proterozoic times and instead that this time and earlier times were dominated by a single, persistent "Paleopangaea" supercontinent. As evidence, he suggests an observation that the palaeomagnetic poles from the continental crust assigned to this time conform to a single path between 800 and 600 million years ago and latterly to a near-static position between 750 and 600 million years. This latter solution predicts that break-up was confined to the Ediacaran Period and produced the dramatic environmental changes that characterised the transition between Precambrian and Phanerozoic times.

text: According to J.D.A. Piper, Rodinia is one of two models for the configuration and history of the continental crust in the latter part of

text: Precambrian

text: times. The other is

text: Paleopangea

text: , Piper's own concept.  Piper proposes an alternative hypothesis for this era and the previous ones. This idea rejects that Rodinia ever existed as a transient supercontinent subject to progressive break-up in the latter part of

text: Proterozoic

text: times and instead that this time and earlier times were dominated by a single, persistent "

text: Paleopangaea

text: " supercontinent. As evidence, he suggests an observation that the palaeomagnetic poles from the continental crust assigned to this time conform to a single path between 800 and 600 million years ago and latterly to a near-static position between 750 and 600 million years. This latter solution predicts that break-up was confined to the

text: Ediacaran

text: Period and produced the dramatic environmental changes that characterised the transition between Precambrian and

text: Phanerozoic

text: times.

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answers: Proterozoic

answers: NDQ_005572

answers: Rodinia

answers: NDQ_005573

answers: a near-static position

answers: NDQ_005574

answers: Rodinia

answers: NDQ_005575

answers: Rodinia

answers: NDQ_005576

answers: precambrian

answers: NDQ_005577

answers: Zircons in ancient rocks indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The falls have a drop of , cascading into a gorge carved out of the Precambrian Shield by meltwater following the last glacial maximum. Because of its size and ease of access, it has been consequently nicknamed "the Niagara of the North".

text: The falls have a drop of , cascading into a gorge carved out of the

text: Precambrian Shield

text: by

text: meltwater

text: following the

text: last glacial maximum

text: . Because of its size and ease of access, it has been consequently nicknamed "the Niagara of the North".

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answers: NDQ_005577

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answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Precambrian Shield

answers: NDQ_005575

answers: last glacial maximum

answers: NDQ_005576

answers: gorge

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: last glacial maximum

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: To the east the Sub-Cambrian peneplain continues as an unconformity beneath the East European Platform. The island Blå Jungfrun in the Baltic Sea is an ancient inselberg belonging to the Sub-Cambrian peneplain. Being a inselberg formed in Precambrian time it was buried in sandstone after its formation and remained buried until erosion of the East European Platform freed it in geologically recent times.

text: To the east the Sub-Cambrian peneplain continues as an

text: unconformity

text: beneath the

text: East European Platform

text: . The island

text: Blå Jungfrun

text: in the

text: Baltic Sea

text: is an ancient

text: inselberg

text: belonging to the Sub-Cambrian peneplain. Being a inselberg formed in

text: Precambrian

text: time it was

text: buried

text: in

text: sandstone

text: after its formation and remained buried until

text: erosion

text: of the East European Platform freed it in geologically recent times.

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answers: sandstone

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answers: Precambrian

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answers: sandstone

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answers: Sub-Cambrian

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answers: Sub-Cambrian

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answers: inselberg

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answers: Zircons indicate that there was water in the environment

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answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Interaction with another vigorous tropical low and eastern wind shear weakened the storm on September 9. The interaction and weak steering currents brought the storm almost to a halt, meandering around the Cape Verde islands before weakening to a tropical depression as it absorbed the secondary low. The storm regained tropical storm status on September 10, and began to organize again. It rapidly deepened and briefly developed an eye-like feature early on September 11, which persisted for two hours. As Igor absorbed dry air, a process called entrainment, convection decreased, and much of the convection was displaced south of Igor. The storm strengthened into a hurricane, though, late on September 11.

text: Interaction with another vigorous tropical low and eastern

text: wind shear

text: weakened the storm on September 9. The interaction and weak steering currents brought the storm almost to a halt, meandering around the Cape Verde islands before weakening to a tropical depression as it absorbed the secondary low. The storm regained tropical storm status on September 10, and began to organize again. It rapidly deepened and briefly developed an eye-like feature early on September 11, which persisted for two hours. As Igor absorbed dry air, a process called entrainment,

text: convection

text: decreased, and much of the convection was displaced south of Igor. The storm strengthened into a hurricane, though, late on September 11.

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answers: limestone

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answers: eastern wind shear

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answers: greenstones in cratons indicate that at the time they formed

answers: NDQ_005574

answers: Igor

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answers: Precambrian shields are about

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answers: tropical depression

answers: NDQ_005577

answers: It rapidly deepened and briefly developed an eye-like feature early on September 11

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answers: tropical depression

answer: No

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text: The foundation of Florida was located in the continent of Gondwana at the South Pole 650 Mya. When Gondwana collided with the continent of Laurentia 300 Mya, it had moved further north. 200 Mya, the merged continents containing what would be Florida, had moved north of the equator. By then, Florida was surrounded by desert, in the middle of a new continent, Pangaea. When Pangaea broke up 115 mya, Florida assumed a shape as a peninsula.The emergent landmass of Florida was Orange Island, a low-relief island sitting atop the carbonate Florida Platform which emerged about 34 to 28 million years ago.

text: The foundation of Florida was located in the continent of

text: Gondwana

text: at the

text: South Pole

text: 650 Mya. When Gondwana collided with the continent of

text: Laurentia

text: 300 Mya, it had moved further north. 200 Mya, the merged continents containing what would be Florida, had moved north of the equator. By then, Florida was surrounded by desert, in the middle of a new continent,

text: Pangaea

text: . When Pangaea broke up 115 mya, Florida assumed a shape as a peninsula.The emergent

text: landmass

text: of Florida was

text: Orange Island

text: , a low-relief island sitting atop the carbonate

text: Florida Platform

text: which emerged about 34 to 28 million years ago.

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answers: the carbonate Florida Platform

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answers: Florida Platform

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answers: 34 to 28 million years ago

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answers: Florida Platform

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answers: By then, Florida was surrounded by desert

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answers: 650 Mya

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: In geology, a supercontinent is the assembly of most or all of Earth's continental blocks or cratons to form a single large landmass.  However, the definition of a supercontinent can be ambiguous. Many earth scientists, such as P.F. Hoffman (1999), use the term "supercontinent" to mean "a clustering of nearly all continents". This definition leaves room for interpretation when labeling a continental body and is easier to apply to Precambrian times.  Using the first definition provided here, Gondwana (aka Gondwanaland) is not considered a supercontinent, because the landmasses of Baltica, Laurentia and Siberia also existed at the same time but physically separate from each other. The landmass of Pangaea is the collective name describing all of these continental masses when they were in proximity to one another. This would classify Pangaea as a supercontinent. According to the definition by Rogers and Santosh (2004), a supercontinent does not exist today. Supercontinents have assembled and dispersed multiple times in the geologic past (see table). The positions of continents have been accurately determined back to the early Jurassic. However, beyond , continental positions are much less certain.

text: In

text: geology

text: , a supercontinent is the assembly of most or all of

text: Earth

text: 's

text: continental blocks

text: or

text: craton

text: s to form a single large landmass.  However, the definition of a supercontinent can be ambiguous. Many earth scientists, such as P.F. Hoffman (1999), use the term "supercontinent" to mean "a clustering of nearly all continents". This definition leaves room for interpretation when labeling a continental body and is easier to apply to

text: Precambrian

text: times.  Using the first definition provided here,

text: Gondwana

text: (aka Gondwanaland) is not considered a supercontinent, because the landmasses of

text: Baltica

text: Laurentia

text: and

text: Siberia

text: also existed at the same time but physically separate from each other. The landmass of

text: Pangaea

text: is the collective name describing all of these continental masses when they were in proximity to one another. This would classify

text: Pangaea

text: as a supercontinent. According to the definition by Rogers and Santosh (2004), a supercontinent does not exist today. Supercontinents have assembled and dispersed multiple times in the geologic past (see table). The positions of continents have been accurately determined back to the early

text: Jurassic

text: . However, beyond , continental positions are much less certain.

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answers: cratons

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answers: Jurassic

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answers: a supercontinent does not exist today

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answers: Zircons in ancient rocks indicates that there was water in the environment

answers: NDQ_005579

answers: Precambrian times

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: The Trans Brazilian Lineament (TBL), or Transbrasiliano Lineament, is a major shear zone that developed in the Precambrian period, and that has been reactivated several times since then, mostly recently during the Mesozoic. Movement along the shear zone helps explain how the South American continent could have fitted tightly to the African continent before the breakup of Gondwana.

text: The Trans Brazilian Lineament (TBL), or Transbrasiliano Lineament, is a major

text: shear zone

text: that developed in the

text: Precambrian

text: period, and that has been reactivated several times since then, mostly recently during the

text: Mesozoic

text: . Movement along the shear zone helps explain how the

text: South America

text: n continent could have fitted tightly to the

text: Africa

text: n continent before the breakup of

text: Gondwana

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answers: Precambrian

answers: NDQ_005572

answers: the Precambrian period

answers: NDQ_005573

answers: the Precambrian period

answers: NDQ_005574

answers: Gondwana

answers: NDQ_005575

answers: major shear zone

answers: NDQ_005576

answers: shear zone

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: the Precambrian period

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Platform 1 is serves arrivals and departures to Liverpool Lime Street with this service terminating at the platform, and occasionally for North Wales services. Platform 2 is generally used for North Wales services, and southbound intercity services to Birmingham New Street and London Euston.  Platform 3 serves northbound intercity trains to Edinburgh and Glasgow Central. Platform 4 for services from North Wales to Manchester. The platforms are not bi-directional, except that the slow line between the station and Winwick Junction, some  to the north. This allows northbound departures from platform 1. The present platform 4 was numbered 5 for many years, because there was to be a north-facing bay platform in the west island which was numbered 4, but this saw no passenger use after electrification in 1972 being removed later.

text: Platform 1 is serves arrivals and departures to

text: Liverpool Lime Street

text: with this service terminating at the platform, and occasionally for North Wales services. Platform 2 is generally used for North Wales services, and southbound intercity services to Birmingham New Street and London Euston.  Platform 3 serves northbound intercity trains to Edinburgh and Glasgow Central. Platform 4 for services from North Wales to Manchester. The platforms are not bi-directional, except that the slow line between the station and Winwick Junction, some  to the north. This allows northbound departures from platform 1. The present platform 4 was numbered 5 for many years, because there was to be a north-facing bay platform in the west island which was numbered 4, but this saw no passenger use after electrification in 1972 being removed later.

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answers: limestone

answers: NDQ_005572

answers: North Wales

answers: NDQ_005573

answers: the present platform 4 was numbered 5

answers: NDQ_005574

answers: platforms are not bi-directional

answers: NDQ_005575

answers: North Wales

answers: NDQ_005576

answers: platform 4

answers: NDQ_005577

answers: This allows northbound departures from platform 1

answers: NDQ_005579

answers: eons ago

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Basement rocks in the Northeastern region of the Gulf of Mexico basin are fragments of the African plate which remained behind during the breakup of Pangaea and date back to the late Precambrian through the Cambrian. It is atop these Precambrian plate fragments that the mainly carbonate and evaporite sediments deposited after the opening of the Gulf of Mexico would become the Florida Platform.

text: Basement rocks in the Northeastern region of the Gulf of Mexico basin are fragments of the

text: African plate

text: which remained behind during the breakup of Pangaea and date back to the late

text: Precambrian

text: through the

text: Cambrian

text: . It is atop these Precambrian plate fragments that the mainly carbonate and evaporite sediments deposited after the opening of the Gulf of Mexico would become the Florida Platform.

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answers: Precambrian

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answers: Pangaea

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answers: Precambrian

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answers: Pangaea

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answers: Pangaea

answers: NDQ_005576

answers: Florida Platform

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: The NAASP remains an important and potential forum of cooperation among countries in the two continents. In a changing world, certainly the NAASP, like any other international forum, is called upon to address the challenges of today. Undoubtedly in the case of Palestine, the cause of freedom and independence remains a top priority for NAASP. For others, the issue of stability, as well as welfare of Asian and African peoples is the main theme of cooperation that brings the two continents together. Indonesia is of the view that only by working together can the two continents create peace, stability, and prosperity for their peoples.

text: The NAASP remains an important and potential forum of cooperation among countries in the two continents. In a changing world, certainly the NAASP, like any other international forum, is called upon to address the challenges of today. Undoubtedly in the case of Palestine, the cause of freedom and independence remains a top priority for NAASP. For others, the issue of stability, as well as welfare of Asian and African peoples is the main theme of cooperation that brings the two continents together. Indonesia is of the view that only by working together can the two continents create peace, stability, and prosperity for their peoples.

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answers: Asia

answers: NDQ_005572

answers: Asia

answers: NDQ_005573

answers: greenstones in cratons indicate that at the time they formed

answers: NDQ_005574

answers: two continents

answers: NDQ_005575

answers: peace, stability, and prosperity for their peoples

answers: NDQ_005576

answers: NAASP

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: In a changing world

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Zimbabwe Craton is an area in Southern Africa of ancient continental crust, being a part of the ancient continent of Western Gondwana, with rocks dating back to the early Archean Eon, possibly as early as 3.46 billion years ago (Ga.). The craton is named after the country of Zimbabwe where the majority of the craton is located. The rocks of the Zimbabwe Craton are separated from the rocks of the Kaapvaal Craton to the southeast by the 250 km wide Limpopo Belt of granulite facies tectonites.  The Limpopo belt formed contemporaneously with the Zimbabwe and Kaapvaal cratons, but remained geologically active until much later. It was only in the late Archean, ca. 2.8-2.5 Ga., that the two cratons were stabilized together and that high-grade metamorphism ceased in the Limpopo Belt. North of the Zimbabwe Craton is the Zambezi Belt.

text: The Zimbabwe Craton is an area in Southern Africa of ancient continental crust, being a part of the ancient continent of Western

text: Gondwana

text: , with rocks dating back to the early

text: Archean

text: Eon, possibly as early as 3.46 billion years ago (

text: Ga.

text: ). The

text: craton

text: is named after the country of

text: Zimbabwe

text: where the majority of the craton is located. The rocks of the Zimbabwe Craton are separated from the rocks of the

text: Kaapvaal Craton

text: to the southeast by the 250 km wide

text: Limpopo Belt

text: of

text: granulite

text: facies

text: tectonite

text: s.  The Limpopo belt formed contemporaneously with the Zimbabwe and Kaapvaal cratons, but remained geologically active until much later. It was only in the late Archean, ca. 2.8-2.5 Ga., that the two cratons were stabilized together and that high-grade

text: metamorphism

text: ceased in the Limpopo Belt. North of the Zimbabwe Craton is the

text: Zambezi Belt

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answers: tectonites

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answers: Western Gondwana

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answers: The Limpopo Belt

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answers: The Zimbabwe Craton

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answers: 3.46 billion years ago

answers: NDQ_005576

answers: craton

answers: NDQ_005577

answers: The Zimbabwe Craton

answers: NDQ_005579

answers: Archean Eon

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: A shield always accompanied a sword as part of the swordsman's equipment. Carried on the left arm, or when out of use, slung over the shoulder, shields were made of steel or hide and were generally from  in diameter. If made of steel they were often highly ornamented with patterns in gold damascening while hide shields bore silver or gold bosses, crescents, or stars. Shields were made of sambar deer, buffalo, nilgau, elephant, or rhinoceros hide, the last being the most highly prized. Brahmans, who objected to leather, had shields made from forty or fifty folds of silk painted red and ornamented. The curious snakeskin (nagphanl) shield is not a Mughal weapon.

text: A shield always accompanied a sword as part of the swordsman's equipment. Carried on the left arm, or when out of use, slung over the shoulder, shields were made of steel or hide and were generally from  in diameter. If made of steel they were often highly ornamented with patterns in gold

text: damascening

text: while hide shields bore silver or gold bosses, crescents, or stars. Shields were made of

text: sambar deer

text: , buffalo,

text: nilgau

text: elephant

text: , or

text: rhinoceros

text: hide, the last being the most highly prized. Brahmans, who objected to leather, had shields made from forty or fifty folds of silk painted red and ornamented. The curious snakeskin (nagphanl) shield is not a Mughal weapon.

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answers: shields were made of steel or hide and were generally from in diameter

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answers: in diameter

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answers: made of steel or hide

answers: NDQ_005577

answers: It's impossible to say

answers: NDQ_005579

answers: in diameter

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Prior to the breakup of the Precambrian supercontinent and the formation of the modern Permian Basin geometry, shallow marine sedimentation onto to the ancestral Tobosa Basin characterized the passive margin, shallow marine environment.

text: Prior to the breakup of the

text: Precambrian

text: supercontinent

text: and the formation of the modern Permian Basin geometry, shallow marine sedimentation onto to the ancestral

text: Tobosa Basin

text: characterized the

text: passive margin

text: , shallow marine environment.

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answers: 4

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answers: 0

answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: the Precambrian supercontinent

answers: NDQ_005573

answers: shallow marine environment

answers: NDQ_005574

answers: Tobosa Basin

answers: NDQ_005575

answers: Precambrian supercontinent

answers: NDQ_005576

answers: passive margin

answers: NDQ_005577

answers: shallow marine environment

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The most restricted meaning of continent is that of a continuous area of land or mainland, with the coastline and any land boundaries forming the edge of the continent. In this sense the term continental Europe (sometimes referred to in Britain as "the Continent") is used to refer to mainland Europe, excluding islands such as Great Britain, Ireland, Malta and Iceland, and the term continent of Australia may refer to the mainland of Australia, excluding Tasmania and New Guinea. Similarly, the continental United States refers to the 48 contiguous states in central North America and may include Alaska in the northwest of the continent (the two being separated by Canada), while excluding Hawaii in the middle of the Pacific Ocean.

text: The most restricted meaning of continent is that of a continuous area of land or mainland, with the coastline and any land boundaries forming the edge of the continent. In this sense the term

text: continental Europe

text: (sometimes referred to in Britain as "the Continent") is used to refer to mainland Europe, excluding

text: island

text: s such as

text: Great Britain

text: Ireland

text: Malta

text: and

text: Iceland

text: , and the term continent of Australia may refer to the

text: mainland of Australia

text: , excluding

text: Tasmania

text: and

text: New Guinea

text: . Similarly, the

text: continental United States

text: refers to the 48 contiguous states in central North America and may include

text: Alaska

text: in the northwest of the continent (the two being separated by

text: Canada

text: ), while excluding

text: Hawaii

text: in the middle of the

text: Pacific Ocean

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answers: continental

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answers: Australia

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answers: continent

answers: NDQ_005574

answers: Iceland

answers: NDQ_005575

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answers: NDQ_005576

answers: continental

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: continental Europe

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The geology of Uruguay combines areas of Precambrian-aged shield units with a region of volcanic rock erupted during the Cretaceous and copious sedimentary facies the oldest of which date from the Devonian. Big events that have shaped the geology of Uruguay include the Transamazonian orogeny (2000 million years ago (mya)), the breakup of Rodinia (700–500 mya) and the opening of the South Atlantic (~145 mya).

text: The geology of Uruguay combines areas of

text: Precambrian

text: -aged

text: shield

text: unit

text: s with a region of

text: volcanic rock

text: erupted during the

text: Cretaceous

text: and copious

text: sedimentary

text: facies

text: the oldest of which date from the

text: Devonian

text: . Big events that have shaped the geology of

text: Uruguay

text: include the

text: Transamazonian orogeny

text: million years ago

text: (mya)), the breakup of

text: Rodinia

text: mya

text: ) and the

text: opening of the South Atlantic

text: (~145 mya).

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answer: Yes

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text: The convection section is located above the radiant section where it is cooler to recover additional heat. Heat transfer takes place by convection here, and the tubes are finned to increase heat transfer. The first two tube rows in the bottom of the convection section and at the top of the radiant section is an area of bare tubes (without fins) and are known as the shield section ("shock tubes"), so named because they are still exposed to plenty of radiation from the firebox and they also act to shield the convection section tubes, which are normally of less resistant material from the high temperatures in the firebox.

text: The convection section is located above the radiant section where it is cooler to recover additional heat.

text: Heat transfer

text: takes place by

text: convection

text: here, and the tubes are finned to increase heat transfer. The first two tube rows in the bottom of the convection section and at the top of the radiant section is an area of bare tubes (without fins) and are known as the shield section ("shock tubes"), so named because they are still exposed to plenty of radiation from the firebox and they also act to shield the convection section tubes, which are normally of less resistant material from the high temperatures in the firebox.

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answers: are still exposed to plenty of radiation

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answers: Zircons indicate that there was water in the environment

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text: The Australian Shield, also called the Western Australian Shield or Western Plateau, occupies more than half of the continent of Australia. The word shield is used because it refers to ancient, molten rock which has cooled and solidified. The Australian Shield has a characteristic depth of 4.5 km and an estimated age of 2.8 to 3.5 billion years. In places younger sedimentary rock covers the shield's Precambrian surface.

text: The Australian Shield, also called the Western Australian

text: Shield

text: or

text: Western Plateau

text: , occupies more than half of the continent of Australia. The word shield is used because it refers to ancient, molten rock which has cooled and solidified. The Australian Shield has a characteristic depth of 4.5 km and an estimated age of 2.8 to 3.5 billion years. In places younger

text: sedimentary rock

text: covers the shield's

text: Precambrian

text: surface.

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answers: Precambrian

answers: NDQ_005572

answers: The Australian Shield

answers: NDQ_005573

answers: 2.8 to 3.5 billion years

answers: NDQ_005574

answers: molten rock which has cooled and solidified

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answers: molten rock which has cooled and solidified

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answers: Australian Shield

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Early on July 8, another brief burst in convection near the center of Blanca occurred. In this area, satellites found sustained winds around 40 mph (65 km/h). However, the convection quickly dissipated and the winds were not considered to be representative of the storm's true intensity. By later that day, convection had not reformed around the center of circulation and Blanca degenerated into a non-convective remnant low pressure system, corresponding with the final public advisory from the NHC. Although no longer a tropical cyclone, the remnants of Blanca maintained a well-defined low pressure center as it continued its northwesterly movement. Early on July 11, the system turned northward and gradually weakened. The following day, the remnants of Blanca dissipated over open waters.

text: Early on July 8, another brief burst in convection near the center of Blanca occurred. In this area, satellites found sustained winds around 40 mph (65 km/h). However, the convection quickly dissipated and the winds were not considered to be representative of the storm's true intensity. By later that day, convection had not reformed around the center of circulation and Blanca degenerated into a non-convective remnant low pressure system, corresponding with the final public advisory from the NHC. Although no longer a tropical cyclone, the remnants of Blanca maintained a well-defined low pressure center as it continued its northwesterly movement. Early on July 11, the system turned northward and gradually weakened. The following day, the remnants of Blanca dissipated over open waters.

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answers: limestone

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answers: Blanca

answers: NDQ_005573

answers: no longer a tropical cyclone

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answers: Blanca

answers: NDQ_005575

answers: 40 mph (65 km/h

answers: NDQ_005576

answers: low pressure system

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

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answers: tropical

answer: No

answer: No

answer: No

answer: No

answer: No

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text: In recent times, spin bowling has been a forte of the bowlers from the South Asian sub-continent. The primary reason for that is that the pitches in the sub-continent provide more help to the spin bowlers. The faster the pitch degenerates, the earlier the spinners come into the picture. Australian and South African pitches are usually very hard and bouncy, helping the fast bowlers more. They do not break up very much during the duration of the match. In contrast, pitches in the sub-continent are not that hard. They are not usually held together by the grass as much; hence they break up more quickly and help spin bowlers. In general, leg-spinis considered to be one of the toughest types of bowling in which to keep control of the ball, but it is very effective in picking off wickets.

text: In recent times, spin bowling has been a forte of the bowlers from the South Asian sub-continent. The primary reason for that is that the pitches in the sub-continent provide more help to the spin bowlers. The faster the pitch degenerates, the earlier the spinners come into the picture. Australian and South African pitches are usually very hard and bouncy, helping the fast bowlers more. They do not break up very much during the duration of the match. In contrast, pitches in the sub-continent are not that hard. They are not usually held together by the grass as much; hence they break up more quickly and help spin bowlers. In general, leg-spinis considered to be one of the toughest types of bowling in which to keep control of the ball, but it is very effective in picking off wickets.

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answers: Australian and South African

answers: NDQ_005572

answers: South Asian

answers: NDQ_005573

answers: Australian and South African pitches are usually very hard and bouncy

answers: NDQ_005574

answers: South Asian sub-continent

answers: NDQ_005575

answers: They are not usually held together by the grass as much

answers: NDQ_005576

answers: pitches in the sub-continent are not that hard

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: sub-continent

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Slave Craton is an Archaean craton in the north-western Canadian Shield, in Northwest Territories and Nunavut.  The Slave Craton includes the 4.03 Ga-old Acasta Gneiss which is one of the oldest dated rocks on Earth.Covering about , it is a relatively small but well-exposed craton dominated by about 2.73-2.63 Ga (billion years-old) greenstones and turbidite sequences and ca. 2.72-2.58 Ga plutonic rock, with large parts of the craton underlain by older gneiss and granitoid units.The Slave Craton is one of the blocks that compose the Precambrian core of North America, also known as the palaeocontinent Laurentia.

text: The Slave Craton is an

text: Archaean

text: craton

text: in the north-western

text: Canadian Shield

text: , in

text: Northwest Territories

text: and

text: Nunavut

text: .  The Slave Craton includes the 4.03 Ga-old

text: Acasta Gneiss

text: which is one of the

text: oldest dated rocks

text: on Earth.Covering about , it is a relatively small but well-exposed craton dominated by about 2.73-2.63 Ga (billion years-old)

text: greenstones

text: and

text: turbidite

text: sequences

text: and ca. 2.72-2.58 Ga

text: plutonic

text: rock, with large parts of the craton underlain by older

text: gneiss

text: and

text: granitoid

text: units.The Slave Craton is one of the blocks that compose the Precambrian core of North America, also known as the palaeocontinent

text: Laurentia

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answers: plutonic rock

answers: NDQ_005572

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answers: billion years-old

answers: NDQ_005574

answers: The Slave Craton

answers: NDQ_005575

answers: Canadian Shield

answers: NDQ_005576

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answers: Zircons

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: In the north and east of Santa Cruz Department the crystalline and Precambrian Guaporé Shield (also called Central Brazil Shield) makes up most of the bedrock but is mostly covered by Tertiary laterites  and Quaternary alluvial basins. The shield expresses itself topographically as a large elevated hinterland located north of Serranías Chiquitanas towards the Brazilian border. High grade metamorphic rocks occur in the Bolivian part of the Guaporé Shiled partly due to the 2000 millions years old "Transamazonian Tectono-Thermal Event" that affected parts of South America. Low grade metamorphic rocks occur as well. The Guaporé Shield is believed to extend beneath the Phanerozoic Tarija-Chaco and Beni Basin sediments into the Andes. Weakenesses in the Guaporé Shield have been suggested to be responsible for the formation of the Arica Elbow. The East-West Río Mercedes Line in the Guaporé Shield host several Proterozoic diabase intrusions. As of 1985 the rocks of Guaporé Shiled were considered to be poorly known. Near the Brazilian border the iron deposit of El Mutún stands out as the world's largest iron ore deposit. It is located in the Serranía de El Mutún, also called Cerro Mutún or Serranía de Jacadigo in Brazil. The shield also underlies Serrania Caparuch or Huanchaca which is the inspiration for the Lost World of Conan Doyle.

text: In the north and east of

text: Santa Cruz Department

text: the crystalline and

text: Precambrian

text: Guaporé Shield (also called Central Brazil Shield) makes up most of the

text: bedrock

text: but is mostly covered by

text: Tertiary

text: laterite

text: s  and

text: Quaternary

text: alluvial

text: basins. The shield expresses itself topographically as a large elevated

text: hinterland

text: located north of

text: Serranías Chiquitanas

text: towards the Brazilian border. High grade metamorphic rocks occur in the Bolivian part of the Guaporé Shiled partly due to the 2000 millions years old "Transamazonian Tectono-Thermal Event" that affected parts of South America. Low grade metamorphic rocks occur as well. The Guaporé Shield is believed to extend beneath the

text: Phanerozoic

text: Tarija-Chaco and

text: Beni Basin

text: sediments into the Andes. Weakenesses in the Guaporé Shield have been suggested to be responsible for the formation of the

text: Arica Elbow

text: . The East-West Río Mercedes Line in the Guaporé Shield host several

text: Proterozoic

text: diabase

text: intrusion

text: s. As of 1985 the rocks of Guaporé Shiled were considered to be poorly known. Near the Brazilian border the iron deposit of

text: El Mutún

text: stands out as the world's largest

text: iron ore

text: deposit. It is located in the Serranía de El Mutún, also called Cerro Mutún or Serranía de Jacadigo in Brazil. The shield also underlies Serrania Caparuch or Huanchaca which is the inspiration for the

text: Lost World

text: of

text: Conan Doyle

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Guaporé Shield

answers: NDQ_005575

answers: Guaporé Shield

answers: NDQ_005576

answers: Guaporé Shield

answers: NDQ_005577

answers: alluvial basins

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A tropical wave moved off the western coast of Africa on June 22 and entered the East Pacific eight days later. On July 4, convection increased with the aid of a convectively-coupled kelvin wave, and two days later, a broad area of low pressure formed along the wave axis well south-southwest of Baja California. After further organization, the disturbance was declared a tropical depression at 12:00 UTC on July 7. Steered westward around a subtropical ridge, the depression intensified into Tropical Storm Fausto six hours later and simultaneously attained peak winds of 45 mph (75 km/h). By early on July 9, Fausto weakened to a tropical depression as dry air became entrained into the circulation. The low-level center opened up into a trough by 12:00 UTC, marking the demise of the cyclone.

text: A tropical wave moved off the western coast of Africa on June 22 and entered the East Pacific eight days later. On July 4, convection increased with the aid of a convectively-coupled kelvin wave, and two days later, a broad area of low pressure formed along the wave axis well south-southwest of Baja California. After further organization, the disturbance was declared a tropical depression at 12:00 UTC on July 7. Steered westward around a subtropical ridge, the depression intensified into Tropical Storm Fausto six hours later and simultaneously attained peak winds of 45 mph (75 km/h). By early on July 9, Fausto weakened to a tropical depression as dry air became entrained into the circulation. The low-level center opened up into a trough by 12:00 UTC, marking the demise of the cyclone.

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text: s in Precambrian rocks would "completely blow evolution out of the water." Philosopher Peter Godfrey-Smith doubted that a single set of anachronistic fossils, however, even rabbits in the Precambrian, would disprove the theory of evolution outright. The first question raised by the assertion of such a discovery would be whether the alleged "Precambrian rabbits" really were fossilized rabbits. Alternative interpretations might include incorrect identification of the "fossils", incorrect dating of the rocks, and a hoax such as the Piltdown Man was shown to be. Even if the "Precambrian rabbits" turned out to be genuine, they would not instantly refute the theory of evolution, because that theory is a large package of ideas, including: that life on Earth has evolved over billions of years; that this evolution is driven by certain mechanisms; and that these mechanisms have produced a specific "family tree" that defines the relationships among species and the order in which they appeared. Hence, "Precambrian rabbits" would prove that there were one or more serious errors somewhere in this package, and the next task would be to identify those errors.

text: s in Precambrian rocks would "completely blow evolution out of the water." Philosopher

text: Peter Godfrey-Smith

text: doubted that a single set of

text: anachronistic

text: fossils, however, even rabbits in the Precambrian, would disprove the theory of evolution outright. The first question raised by the assertion of such a discovery would be whether the alleged "Precambrian rabbits" really were fossilized rabbits. Alternative interpretations might include incorrect identification of the "fossils", incorrect dating of the rocks, and a

text: hoax

text: such as the

text: Piltdown Man

text: was shown to be. Even if the "Precambrian rabbits" turned out to be genuine, they would not instantly refute the theory of evolution, because that theory is a large package of ideas, including: that life on Earth has evolved over billions of years; that this evolution is driven by certain mechanisms; and that these mechanisms have produced a specific "family tree" that defines the relationships among species and the order in which they appeared. Hence, "Precambrian rabbits" would prove that there were one or more serious errors somewhere in this package, and the next task would be to identify those errors.

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text: The Gawler Craton covers approximately 440,000 square kilometres of central South Australia. Its Precambrian crystalline basement crustal block was cratonised ca. 1550-1450 Ma. Prior to 1550 Ma the craton comprised a number of active Proterozoic orogenic belts extending back in time to at least 2450 Ma.

text: The Gawler Craton covers approximately 440,000 square kilometres of central South Australia. Its

text: Precambrian

text: crystalline

text: basement

text: crust

text: al

text: block

text: was

text: craton

text: ised ca. 1550-1450 Ma. Prior to 1550 Ma the craton comprised a number of active

text: Proterozoic

text: orogenic

text: belts extending back in time to at least 2450 Ma.

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answer: No

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answer: No

answer: No

answer: 1

text: Although the country's volcanic activity dates back to the Precambrian eon, volcanism continues to occur in Western and Northern Canada where it forms part of an encircling chain of volcanoes and frequent earthquakes around the Pacific Ocean called the Pacific Ring of Fire. But because volcanoes in Western and Northern Canada are in remote rugged areas and the level of volcanic activity is less frequent than with other volcanoes around the Pacific Ocean, Canada is commonly thought to occupy a gap in the Pacific Ring of Fire between the volcanoes of western United States to the south and the Aleutian volcanoes of Alaska to the north. However, the mountainous landscape of Western and Northern Canada includes more than 100 volcanoes that have been active during the past two million years and have claimed many lives. Volcanic activity has been responsible for many of Canada's geological and geographical features and mineralization, including the nucleus of North America called the Canadian Shield.

text: Although the country's volcanic activity dates back to the Precambrian eon,

text: volcanism

text: continues to occur in

text: Western

text: and

text: Northern Canada

text: where it forms part of an encircling chain of volcanoes and frequent

text: earthquake

text: s around the

text: Pacific Ocean

text: called the

text: Pacific Ring of Fire

text: . But because volcanoes in Western and Northern Canada are in remote rugged areas and the level of volcanic activity is less frequent than with other volcanoes around the Pacific Ocean, Canada is commonly thought to occupy a gap in the Pacific Ring of Fire between the volcanoes of western

text: United States

text: to the south and the

text: Aleutian volcanoes

text: of

text: Alaska

text: to the north. However, the mountainous landscape of Western and Northern Canada includes more than 100 volcanoes that have been active during the past two million years and have claimed many lives. Volcanic activity has been responsible for many of Canada's geological and geographical features and

text: mineralization

text: , including the nucleus of

text: North America

text: called the

text: Canadian Shield

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answers: Precambrian

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answers: Precambrian

answers: NDQ_005573

answers: volcanoes

answers: NDQ_005574

answers: Pacific Ring of Fire

answers: NDQ_005575

answers: the nucleus of North America

answers: NDQ_005576

answers: Grand Canyon

answers: NDQ_005577

answers: Precambrian eon

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: It is often studied by geologists due to the extreme old age of the Precambrian rocks exposed by the creek bed. The canyon's high walls are of three dominant rock types. The Cambrian to Ordovician Deadwood Shale at the bottom lies on an unconformity above Precambrian rock and can be identified by its brown color. It is multi-layered in appearance and ranges from 10 to 400 feet thick. Englewood Limestone in the middle is pink to red colored and is 30 to 60 feet thick. The Paleogene Paha Sapa Limestone, the top layer, is the thickest (300 to 600 feet) and is buff colored and weathered gray in appearance. Caves and fossils are frequently found in the Paha Sapa Limestone.

text: It is often studied by geologists due to the extreme old age of the Precambrian rocks exposed by the creek bed. The canyon's high walls are of three dominant rock types. The

text: Cambrian

text: to

text: Ordovician

text: Deadwood Shale

text: at the bottom lies on an

text: unconformity

text: above Precambrian rock and can be identified by its brown color. It is multi-layered in appearance and ranges from 10 to 400 feet thick.

text: Englewood Limestone

text: in the middle is pink to red colored and is 30 to 60 feet thick. The

text: Paleogene

text: Paha Sapa Limestone

text: , the top layer, is the thickest (300 to 600 feet) and is buff colored and weathered gray in appearance. Caves and fossils are frequently found in the Paha Sapa Limestone.

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answers: NDQ_005576

answers: unconformity

answers: NDQ_005577

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answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Deadwood Shale

answers: NDQ_005575

answers: old age

answers: NDQ_005576

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answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The dyke swarms of Tandil and Azul are groups of dykes of Proterozoic age located in Buenos Aires Province, Argentina. The dyke swarms consists of two groups: 2000 million year old dykes of calc-alkaline type and 1600 million year old dykes of tholeiitic type.The tholeiitic dykes are made up of diabase and titanium-rich basalt, in contrast the calc-alkaline dykes are made up of andesite and rhyolite. The dyke swarms intrude the southern part of the Río de la Plata Craton, much the same way the Uruguayan dyke swarms intrude the northeastern part of the craton. The calc-alkaline dykes intruded during a period of transtensional tectonics during the Transamazonian Orogeny while the tholeiitic dykes intruded during the period of extensional tectonics that succeeded the orogeny.

text: The dyke swarms of Tandil and Azul are

text: groups of dykes

text: of

text: Proterozoic

text: age located in

text: Buenos Aires Province

text: , Argentina. The dyke swarms consists of two groups: 2000 million year old dykes of

text: calc-alkaline

text: type and 1600 million year old dykes of

text: tholeiitic

text: type.The tholeiitic dykes are made up of

text: diabase

text: and

text: titanium-rich

text: basalt

text: , in contrast the calc-alkaline dykes are made up of

text: andesite

text: and

text: rhyolite

text: . The dyke swarms

text: intrude

text: the southern part of the

text: Río de la Plata Craton

text: , much the same way the

text: Uruguayan dyke swarms

text: intrude the northeastern part of the craton. The calc-alkaline dykes intruded during a period of

text: transtensional tectonics

text: during the

text: Transamazonian Orogeny

text: while the tholeiitic dykes intruded during the period of

text: extensional tectonics

text: that succeeded the orogeny.

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answer: No

answer: No

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answer: 1

text: Platform 1 is rarely used except for peak-hour services to and from London Liverpool Street starting or terminating at Witham; a limited number of through-trains towards London use this platform as well. Platform 1 was formerly used by trains on the now disused Witham-Maldon branch line. Platform 2 is typically for services towards London and platform 3 is for country-bound services. Platform 4 is the Braintree platform, where services start from or terminate here on Sundays, or run on to and from London from Monday to Saturday. This platform is also used by through eastbound services stopping during peak times to allow non-stopping express trains to pass through unhindered. Some evening peak services terminating at Witham also use this platform. Before the lengthening of the Braintree line platforms through-trains to Braintree would divide here with only the front four coaches going forward.

text: Platform 1 is rarely used except for peak-hour services to and from

text: London Liverpool Street

text: starting or terminating at Witham; a limited number of through-trains towards London use this platform as well. Platform 1 was formerly used by trains on the now disused

text: Witham-Maldon branch line

text: . Platform 2 is typically for services towards London and platform 3 is for country-bound services. Platform 4 is the Braintree platform, where services start from or terminate here on Sundays, or run on to and from London from Monday to Saturday. This platform is also used by through eastbound services stopping during peak times to allow non-stopping express trains to pass through unhindered. Some evening peak services terminating at Witham also use this platform. Before the lengthening of the Braintree line platforms through-trains to Braintree would divide here with only the front four coaches going forward.

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answers: igneous

answers: NDQ_005572

answers: London Liverpool Street

answers: NDQ_005573

answers: platform 4 is the Braintree platform

answers: NDQ_005574

answers: platform 4 is the Braintree platform

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answers: platform 4 is the Braintree platform

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answers: platform 4 is the Braintree platform

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answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: the lengthening of the Braintree line

answer: No

answer: No

answer: No

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text: During late November, an area of convection persisted about 625 kilometers (390 mi) east-southeast of Pohnpei. Satellite imagery indicated broad cyclonic turning in the lower levels of the atmosphere, and a trough was located near the surface. The disturbance developed rainbands and gradually became better organized. By December 2, the system had an elongated low-level circulation, located to the south of the convection. At 0600 UTC that day, the Japan Meteorological Agency (JMA) classified the system as a tropical depression about 735 km (450 mi) east-northeast of Pohnpei. Shortly thereafter, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert, and at 1800 UTC on December 2 the agency classified the system as Tropical Depression 31W. Initially the depression moved to the west-northwest, and early on December 3 the JTWC classified the system as a tropical storm.

text: During late November, an area of

text: convection

text: persisted about 625 kilometers (390 mi) east-southeast of

text: Pohnpei

text: . Satellite imagery indicated broad cyclonic turning in the lower levels of the atmosphere, and a

text: trough

text: was located near the surface. The disturbance developed

text: rainbands

text: and gradually became better organized. By December 2, the system had an elongated low-level

text: circulation

text: , located to the south of the convection. At 0600

text: UTC

text: that day, the

text: Japan Meteorological Agency

text: (JMA) classified the system as a tropical depression about 735 km (450 mi) east-northeast of Pohnpei. Shortly thereafter, the

text: Joint Typhoon Warning Center

text: (JTWC) issued a

text: Tropical Cyclone Formation Alert

text: , and at 1800 UTC on December 2 the agency classified the system as Tropical Depression 31W. Initially the depression moved to the west-northwest, and early on December 3 the JTWC classified the system as a tropical storm.

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answers: Tropical Cyclone Formation

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answers: late November

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: The area was originally characterized by Precambrian and Paleozoic northeast-southwest fold and thrust belts. Volcanism began in the late Cretaceous in limited areas, but is mostly limited to the Miocene. It is also the age of sedimentary rocks in some basins, and the same series lasted into the Eocene. Rifting resumed beginning in the Oligocene, and is commonly held to have increased since the middle Pliocene, causing the formation of basins in the form of grabens. The new rift structure may follow the Precambrian and Paleozoic faults. Magmatic activity and rifting may also be independent events. Outside of the grabens basalt volcanics erupted from either end of the rift system during the uplift. The grabens mostly spread without releasing magma, except the Tunka depression.

text: The area was originally characterized by Precambrian and Paleozoic northeast-southwest fold and thrust belts. Volcanism began in the late Cretaceous in limited areas, but is mostly limited to the

text: Miocene

text: . It is also the age of sedimentary rocks in some basins, and the same series lasted into the

text: Eocene

text: . Rifting resumed beginning in the

text: Oligocene

text: , and is commonly held to have increased since the middle

text: Pliocene

text: , causing the formation of basins in the form of grabens. The new rift structure may follow the Precambrian and Paleozoic faults. Magmatic activity and rifting may also be independent events. Outside of the grabens

text: basalt

text: volcanics erupted from either end of the rift system during the uplift. The grabens mostly spread without releasing magma, except the Tunka depression.

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answers: Paleozoic

answers: NDQ_005572

answers: Paleozoic

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answers: magma

answers: NDQ_005574

answers: basins in the form of grabens

answers: NDQ_005575

answers: northeast-southwest fold

answers: NDQ_005576

answers: grabens

answers: NDQ_005577

answers: Precambrian and Paleozoic

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: A terminology has evolved covering the early years of the Earth's existence, as radiometric dating has allowed real dates to be assigned to specific formations and features. The Precambrian Supereon is divided into three eons: the Hadean (4500–3950 Ma), Archean (- Ma) and Proterozoic (- Ma). See Timetable of the Precambrian.

text: A terminology has evolved covering the early years of the Earth's existence, as

text: radiometric dating

text: has allowed real dates to be assigned to specific formations and features. The Precambrian Supereon is divided into three eons: the

text: Hadean

text: (4500–3950 Ma),

text: Archean

text: (- Ma) and

text: Proterozoic

text: (- Ma). See

text: Timetable of the Precambrian

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answers: NDQ_005571

answers: Archean

answers: NDQ_005572

answers: The Precambrian

answers: NDQ_005573

answers: radiometric dating

answers: NDQ_005574

answers: eons

answers: NDQ_005575

answers: 4500–3950 Ma

answers: NDQ_005576

answers: formations

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: The Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: As noted by Digby and numerous later publications, this archipelago consists of a mixture of folded and faulted sedimentary and igneous rocks ranging in age from Precambrian to Pliocene. The Lyakhovsky Islands consist of a folded and faulted assemblage of Precambrian metamorphic rocks; upper Paleozoic to Triassic sandstones and shales; Jurassic to lower Cretaceous turbidites; Cretaceous granites; and ophiolites. The Anzhu Islands consist of a highly faulted and folded assemblage of Ordovician to Devonian limestones, dolomites, sandstones, shales, volcanoclastic strata, and igneous rocks; upper Paleozoic to Triassic sandstones and shales; Jurassic to lower Cretaceous turbidites; and upper Cretaceous to Pliocene sandstones and shales. The De Long Islands consist of early Paleozoic, middle Paleozoic, Cretaceous, and Neogene sedimentary and igneous (mostly basalt) rocks. These sedimentary, metamorphic, and igneous rocks are mantled by loose Pleistocene and Holocene sediments that range in thickness from a fraction of a meter to about .

text: As noted by Digby and numerous later publications, this archipelago consists of a mixture of

text: folded

text: and

text: faulted

text: sedimentary

text: and

text: igneous rock

text: s ranging in age from

text: Precambrian

text: to

text: Pliocene

text: . The Lyakhovsky Islands consist of a folded and faulted assemblage of Precambrian

text: metamorphic rock

text: s; upper

text: Paleozoic

text: to

text: Triassic

text: sandstone

text: s and

text: shale

text: s;

text: Jurassic

text: to lower

text: Cretaceous

text: turbidite

text: s; Cretaceous

text: granite

text: s; and

text: ophiolite

text: s. The Anzhu Islands consist of a highly faulted and folded assemblage of

text: Ordovician

text: to

text: Devonian

text: limestone

text: s,

text: dolomite

text: s, sandstones, shales, volcanoclastic strata, and igneous rocks; upper Paleozoic to Triassic sandstones and shales; Jurassic to lower Cretaceous turbidites; and upper Cretaceous to Pliocene sandstones and shales. The De Long Islands consist of early Paleozoic, middle Paleozoic, Cretaceous, and Neogene sedimentary and igneous (mostly

text: basalt

text: ) rocks. These sedimentary, metamorphic, and igneous rocks are mantled by loose

text: Pleistocene

text: and

text: Holocene

text: sediment

text: s that range in thickness from a fraction of a meter to about .

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answer: No

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answer: 1

text: For example, the Ural Mountains, to the west of the Angaran Shield, are atop the mobile zone that separates the shield from the Baltic Shield.  Similarly, the Himalayas are on the mobile boundary between the Angaran and Indian shields. Shield margins have been subject to geotectonic forces that have both destroyed and rebuilt the margins and the cratons that they partially comprise. In fact, the growth of continents has occurred as a result of the accretion of younger rocks that underwent deformations during series of mountain building processes. In a sense, these belts of folded rocks have been welded onto the borders of the preexisting shields, thus increasing the size of the proto-continents that they make up.

text: For example, the

text: Ural Mountains

text: , to the west of the Angaran Shield, are atop the mobile zone that separates the shield from the Baltic Shield.  Similarly, the

text: Himalayas

text: are on the mobile boundary between the

text: Angaran

text: and

text: Indian

text: shields. Shield margins have been subject to

text: geotectonic

text: forces that have both destroyed and rebuilt the margins and the cratons that they partially comprise. In fact, the growth of continents has occurred as a result of the accretion of younger rocks that underwent

text: deformation

text: s during series of mountain building processes. In a sense, these belts of folded rocks have been welded onto the borders of the preexisting shields, thus increasing the size of the proto-continents that they make up.

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answers: Angaran

answers: NDQ_005572

answers: Angaran Shield

answers: NDQ_005573

answers: Shield margins have been subject to geotectonic forces

answers: NDQ_005574

answers: Shield

answers: NDQ_005575

answers: the Baltic Shield

answers: NDQ_005576

answers: Shield

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: the Baltic Shield

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Although Laurasia is known as a Mesozoic phenomenon, today it is believed that the same continents that formed the later Laurasia also existed as a coherent supercontinent after the breakup of Rodinia around 1 billion years ago. To avoid confusion with the Mesozoic continent, this is referred to as Proto-Laurasia. It is believed that Laurasia did not break up again before it recombined with the southern continents to form the late Precambrian supercontinent of Pannotia, which remained until the early Cambrian.  Laurasia was assembled, then broken up, due to the actions of plate tectonics, continental drift, and seafloor spreading.

text: Although Laurasia is known as a

text: Mesozoic

text: phenomenon, today it is believed that the same continents that formed the later Laurasia also existed as a coherent supercontinent after the breakup of

text: Rodinia

text: around 1 billion years ago. To avoid confusion with the Mesozoic continent, this is referred to as Proto-Laurasia. It is believed that Laurasia did not break up again before it recombined with the southern continents to form the late

text: Precambrian

text: supercontinent of

text: Pannotia

text: , which remained until the early

text: Cambrian

text: .  Laurasia was assembled, then broken up, due to the actions of

text: plate tectonics

text: continental drift

text: , and

text: seafloor spreading

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text: The platform dreams to interconnect the African people to contribute to the development of the continent. The platform claims 250 000 accounts registered in three years. Its promoters hope to mobilize investments in the order of $1 million to $10 million to accelerate the growth of Mivasocial.

text: The platform dreams to interconnect the African people to contribute to the development of the continent. The platform claims 250 000 accounts registered in three years. Its promoters hope to mobilize investments in the order of $1 million to $10 million to accelerate the growth of Mivasocial.

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text: The convective season for the Plains ranges between May and September.  Organized systems of thunderstorms known as mesoscale convective systems develop over the region during this period, with a bulk of the activity occurring between midnight and 6 a.m. local time.  The time of maximum precipitation during the day gradually varies from late afternoon near the slopes of the Rockies to early morning near the Ohio River valley, in part reflecting the west-to-east propagation of mesoscale convective systems.  Mesoscale convective systems bring 30 to 70 percent of the annual warm season rainfall to the Plains.  An especially long-lived and well-organized type of mesoscale convective system called a mesoscale convective complex produces on average 8% to 18% of the annual warm season rainfall across the Plains and Midwest.  Squall lines account for 30% of the large thunderstorm complexes which move through the region.

text: The convective season for the Plains ranges between May and September.  Organized systems of thunderstorms known as

text: mesoscale convective system

text: s develop over the region during this period, with a bulk of the activity occurring between midnight and 6 a.m. local time.  The time of maximum precipitation during the day gradually varies from late afternoon near the slopes of the Rockies to early morning near the Ohio River valley, in part reflecting the west-to-east propagation of mesoscale convective systems.  Mesoscale convective systems bring 30 to 70 percent of the annual warm season rainfall to the Plains.  An especially long-lived and well-organized type of mesoscale convective system called a

text: mesoscale convective complex

text: produces on average 8% to 18% of the annual warm season rainfall across the Plains and Midwest.

text: Squall line

text: s account for 30% of the large thunderstorm complexes which move through the region.

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answers: Rockies

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answer: No

answer: No

answer: No

answer: No

answer: 0

text: The topography of the biosphere reserve is rugged, consisting of steep, rocky slopes and ridges, typical of the Precambrian Shield. These alternate with moist forest or wetland valleys inland, and rocky promontories in the Saint Lawrence River known as the Thousand Islands.

text: The topography of the biosphere reserve is rugged, consisting of steep, rocky slopes and ridges, typical of the Precambrian Shield. These alternate with moist

text: forest

text: or wetland valleys inland, and rocky promontories in the Saint Lawrence River known as the Thousand Islands.

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

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answers: Precambrian

answers: NDQ_005575

answers: biosphere reserve

answers: NDQ_005576

answers: Shield

answers: NDQ_005577

answers: Saint Lawrence River

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Archaean greenstones are found in the Slave craton, northern Canada, Pilbara craton and Yilgarn Craton, Western Australia, Gawler Craton in South Australia, and in the Wyoming Craton in the US. Examples are found in South and Eastern Africa, namely the Kaapvaal craton and also in the cratonic core of Madagascar, as well as West Africa and Brazil, northern Scandinavia and the Kola Peninsula (see Baltic Shield).

text: Archaean greenstones are found in the

text: Slave craton

text: , northern

text: Canada

text: Pilbara craton

text: and

text: Yilgarn Craton

text: Western Australia

text: Gawler Craton

text: in

text: South Australia

text: , and in the

text: Wyoming Craton

text: in the US. Examples are found in South and Eastern Africa, namely the

text: Kaapvaal craton

text: and also in the cratonic core of

text: Madagascar

text: , as well as

text: West Africa

text: and

text: Brazil

text: , northern

text: Scandinavia

text: and the

text: Kola Peninsula

text: (see

text: Baltic Shield

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answers: NDQ_005571

answers: Archaean

answers: NDQ_005572

answers: Slave craton

answers: NDQ_005573

answers: Archaean

answers: NDQ_005574

answers: cratonic core of Madagascar

answers: NDQ_005575

answers: Baltic Shield

answers: NDQ_005576

answers: craton

answers: NDQ_005577

answers: Archaean greenstones

answers: NDQ_005579

answers: Archaean

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The Taiga Shield Ecozone, as defined by the Commission for Environmental Cooperation (CEC), is an ecozone which stretches across Canada's subarctic region. Some regions exhibit exposed Precambrian bedrock of the Canadian Shield, the oldest of the world's geological formations. The world's oldest rocks, dating to four billion years, are found in the Canadian Shield north of Great Slave Lake.

text: The Taiga Shield Ecozone, as defined by the

entity_name: Commission for Environmental Cooperation

text: Commission for Environmental Cooperation

text: (CEC), is an

text: ecozone

text: which stretches across

text: Canada's

text: subarctic region. Some regions exhibit exposed

text: Precambrian

text: bedrock

text: of the

text: Canadian Shield

text: , the oldest of the world's geological formations. The world's oldest rocks, dating to four billion years, are found in the Canadian Shield north of

text: Great Slave Lake

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answers: Precambrian

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answers: Precambrian

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answers: Precambrian

answers: NDQ_005574

answers: The world's oldest rocks

answers: NDQ_005575

answers: Canada's subarctic region

answers: NDQ_005576

answers: Canadian Shield

answers: NDQ_005577

answers: Great Slave Lake

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In addition, subduction zones present due to the adjoining of Gondwana continents further influence the convection of mantle. Therefore, inhomogeneous mantle is formed and cause crustal thinning. Various igneous structures formed by magma intrusion from mantle to crust and extrusion to the land surface.

text: In addition, subduction zones present due to the adjoining of Gondwana continents further influence the convection of mantle. Therefore, inhomogeneous mantle is formed and cause crustal thinning. Various igneous structures formed by magma intrusion from mantle to crust and extrusion to the land surface.

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answers: 0

answers: NDQ_005571

answers: mantle

answers: NDQ_005572

answers: Gondwana

answers: NDQ_005573

answers: subduction zones present

answers: NDQ_005574

answers: Gondwana

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answers: Gondwana

answers: NDQ_005576

answers: subduction zones

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Gondwana

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Younger metamorphic dates (1.81–1.71 Ga) also typify the eastern and northern Wyoming province peripheries in the western Dakotas and southeastern Montana. The final assembly of the eastern Wyoming Craton as part of the continent Laurentia began during the ca. 1.78–1.74 Ga interval of island-arc accretion along the southern margin of the growing craton.<ref name=Dahl>

text: Younger

text: metamorphic

text: dates (1.81–1.71 Ga) also typify the eastern and northern Wyoming province peripheries in the western

text: Dakotas

text: and southeastern

text: Montana

text: . The final assembly of the eastern Wyoming Craton as part of the continent

text: Laurentia

text: began during the ca. 1.78–1.74 Ga interval of

text: island-arc

text: accretion

text: along the southern margin of the growing craton.<ref name=Dahl>

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answers: Laurentia

answers: NDQ_005572

answers: Laurentia

answers: NDQ_005573

answers: accretion

answers: NDQ_005574

answers: Wyoming Craton

answers: NDQ_005575

answers: 1.78–1.74 Ga

answers: NDQ_005576

answers: Wyoming Craton

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment.

answers: NDQ_005579

answers: 1.78–1.74 Ga

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: A long time ago an emperor called Muuru was having problems with the empire which was in a civil war, so he tried to summon a god named アルカイ「arukai」 (which was translated as Yorae) to unify the empire through its divinity. The summoning was imperfect, which made the god to be split both in time and bodies. The summoned god was called Fou-lu. After ten years he was able to unify the western continent into the Fou empire. Meanwhile, the western continent was repeatedly attacked by the eastern continent, so Fou-lu decided to create a bridge that would transport people and things to the other continent. Carrying the ambitions of Muuru, Fou-lu wanted to unify both continents and cease the war. But due to the imperfect summoning Fou-lu entered a sleeping state (sealed) and the empire lost its strike on the eastern continent keeping the war in a deadlock. Without Fou-lu's presence the war kept going on for many years of truces and war. Several years later, the second half of the god came into the world, waking up Fou-lu that was sealed in a long sleep recovering his powers. And so the game begins...

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text: A typical subway station has waiting platforms ranging from  long, though some IND platforms may be as long as  long. Platforms of former commuter rail stations, such as those on the IND Rockaway Line, are even longer. Due to the large number of transit lines, one platform or set of platforms often serve more than one service. Passengers need to look at the overhead signs at the platform entrance steps and over each track to see which trains stop there and when, and at the arriving train to see which one it is.

text: A typical subway station has waiting platforms ranging from  long, though some IND platforms may be as long as  long. Platforms of former commuter rail stations, such as those on the

text: IND Rockaway Line

text: , are even longer. Due to the large number of transit lines, one platform or set of platforms often serve more than one service. Passengers need to look at the overhead signs at the platform entrance steps and over each track to see which trains stop there and when, and at the arriving train to see which one it is.

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answers: IND

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answers: IND

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answers: long

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answers: Rockaway Line

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answers: long

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answers: platform or set of platforms often serve more than one service

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answers: former

answer: No

answer: No

answer: No

answer: No

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text: The Isua Greenstone Belt is an anomaly in terms of the other greenstone belts in the world. It is the only greenstone belt that has preserved deformational events from greater than 3.2 Ga and contains peridotites (indicating an obducted ophiolite sequence). However, as compared to the Pilbara Craton and the Barberton Greenstone Belts, which have alternate evolution theories, there are a few similarities.

text: The Isua Greenstone Belt is an anomaly in terms of the other

text: greenstone belt

text: s in the world. It is the only greenstone belt that has preserved deformational events from greater than 3.2 Ga and contains

text: peridotite

text: s (indicating an obducted

text: ophiolite

text: sequence). However, as compared to the

text: Pilbara Craton

text: and the

text: Barberton Greenstone Belt

text: s, which have alternate evolution theories, there are a few similarities.

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text: The Jericho pipe is a diamondiferous diatreme in the Slave craton of the Northwest Territories, Canada, located  northeast of Yellowknife near the northern end of Contwoyto Lake. It is home to the Jericho Diamond Mine.

text: The Jericho pipe is a

text: diamond

text: iferous

text: diatreme

text: in the

text: Slave craton

text: of the

text: Northwest Territories

text: Canada

text: , located  northeast of

text: Yellowknife

text: near the northern end of

text: Contwoyto Lake

text: . It is home to the

text: Jericho Diamond Mine

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answer: No

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text: The craton is one of the distinct physiographic provinces of the West Australian Shield physiographic division, which comprises the Stirling-Mount Barren Block, Darling Hills, and Recherche Shelf sections.

text: The craton is one of the distinct physiographic provinces of the

text: West Australian Shield

text: physiographic division, which comprises the Stirling-Mount Barren Block, Darling Hills, and Recherche Shelf sections.

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text: Dr. Stockwell was also an explorer.  In July/August 1932, he canoed through the unexplored region north of Great Slave Lake. This work delineated the basic features and problems of the geology of this large part of the Precambrian Shield, and laid the foundation for the many studies that followed.

text: Dr. Stockwell was also an explorer.  In July/August 1932, he

text: canoed

text: through the unexplored region north of

text: Great Slave Lake

text: . This work delineated the basic features and problems of the geology of this large part of the

text: Precambrian Shield

text: , and laid the foundation for the many studies that followed.

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answers: Precambrian

answers: NDQ_005572

answers: Great Slave Lake

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answers: Precambrian

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answers: geology

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answers: NDQ_005577

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answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Depositional age of the Mount Barren Group on the southern margin of the Yilgarn Craton and zircon provenance analysis support the hypothesis that collisions between the Pilbara–Yilgarn and Yilgarn–Gawler Cratons assembled a proto-Australian continent approximately  (Dawson et al. 2002).

text: Depositional age of the

text: Mount Barren Group

text: on the southern margin of the

text: Yilgarn Craton

text: and

text: zircon

text: provenance analysis support the hypothesis that collisions between the

text: Pilbara

text: Yilgarn

text: and

text: Yilgarn

text: Gawler

text: Craton

text: s assembled a proto-Australian continent approximately  (Dawson et al. 2002).

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answers: NDQ_005571

answers: Mount Barren Group

answers: NDQ_005572

answers: Yilgarn Craton

answers: NDQ_005573

answers: Depositional age

answers: NDQ_005574

answers: Yilgarn–Gawler

answers: NDQ_005575

answers: Mount Barren Group

answers: NDQ_005576

answers: Craton

answers: NDQ_005577

answers: Zircon provenance analysis

answers: NDQ_005579

answers: proto-Australian continent

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Reconstructions of the supercontinent Vaalbara places two cratons, Kaapvaal in southern Africa and Pilbara in western Australia next to each other based on stratigraphic similarities.  In Roger's configuration of Ur these cratons are placed far apart in their Gondwana configuration.  This configuration is contradicted by widespread Precambrian collisional events between Australia and Africa.

text: Reconstructions of the supercontinent

text: Vaalbara

text: places two cratons,

text: Kaapvaal

text: in southern Africa and

text: Pilbara

text: in western Australia next to each other based on stratigraphic similarities.  In Roger's configuration of Ur these cratons are placed far apart in their Gondwana configuration.  This configuration is contradicted by widespread Precambrian collisional events between Australia and Africa.

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answers: cratons

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answers: Zircons

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The story begins when the father of the protagonist brings home a map fragment from a fishing trip; this map suggests to the protagonist and his friend that the world had, at some point in its past, many continents, though now there is only the small island of . The two of them find a way to travel back to the past, when the continents still existed. The continents are facing serious problems that threaten their existence; the protagonist and his growing party work to resolve the problems, and when they do, the continents reappear in the present. When all the continents are finally restored, the Demon Lord, who is responsible for the loss of many of the continents, appears and seals away many of the continents again. He then raises up his Dark Palace, where the party face the Demon Lord in a final showdown.

text: The story begins when the father of the protagonist brings home a map fragment from a fishing trip; this map suggests to the protagonist and his friend that the world had, at some point in its past, many continents, though now there is

text: only the small island

text: of . The two of them find a way to

text: travel

text: back to the past, when the continents still existed. The continents are facing serious problems that threaten their existence; the protagonist and his growing party work to resolve the problems, and when they do, the continents reappear in the present. When all the continents are finally restored, the Demon Lord, who is responsible for the loss of many of the continents, appears and seals away many of the continents again. He then raises up his Dark Palace, where the party face the Demon Lord in a final showdown.

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answers: continents

answers: NDQ_005572

answers: a fishing trip

answers: NDQ_005573

answers: continents still existed

answers: NDQ_005574

answers: are facing serious problems that threaten their existence

answers: NDQ_005575

answers: The continents are facing serious problems that threaten their existence

answers: NDQ_005576

answers: continents

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: continents still existed

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Great Bear Lake lies between two major physiographic regions: the Kazan Uplands portion of the Canadian Shield and the Interior Plains. It was part of Glacial Lake McConnell in the pre-glacial valleys reshaped by erosional ice during the Pleistocene. Since, the lake has changed from post-glacial rebound following the ice melting. Precambrian rocks of the Canadian Shield form the eastern margin of the McTavish Arm. These rocks of the Precambrian are sedimentary and metamorphic deposits supplemented by igneous intrusions forming dikes and sills.

text: Great Bear Lake lies between two major

text: physiographic regions

text: : the

text: Kazan Uplands

text: portion of the

text: Canadian Shield

text: and the

text: Interior Plains

text: . It was part of

text: Glacial Lake McConnell

text: in the pre-glacial valleys reshaped by

text: erosion

text: al ice during the

text: Pleistocene

text: . Since, the lake has changed from

text: post-glacial rebound

text: following the ice melting.

text: Precambrian

text: rocks of the Canadian Shield form the eastern margin of the McTavish Arm. These rocks of the Precambrian are

text: sediment

text: ary and

text: metamorphic

text: deposits supplemented by

text: igneous

text: intrusion

text: s forming

text: dike

text: s and

text: sill

text: s.

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answers: 4

answers: NDQ_005576

answers: 0

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answers: 0

answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Canadian Shield

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: igneous intrusions

answers: NDQ_005575

answers: Canadian Shield

answers: NDQ_005576

answers: glacial valleys

answers: NDQ_005577

answers: Glacial Lake McConnell

answers: NDQ_005579

answers: Pleistocene

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: He was the elder brother of the Masonic author Albert Churchward (1852–1925.) He was a tea planter in Sri Lanka before coming to the US in the 1890s. In James' biography entitled My Friend Churchey and His Sunken Continent, he discussed Mu with Augustus Le Plongeon and his wife in the 1890s. He patented NCV Steel, armor plating to protect ships during World War I, and other steel alloys. After a patent-infringement settlement in 1914, James retired to his 7+ acre estate on Lake Wononskopomuc in Lakeville, Connecticut, to answer the questions from his Pacific travels.  In 1926, at the age of 75, he published The Lost Continent of Mu: Motherland of Man, which he claimed proved the existence of a lost continent, called Mu, in the Pacific Ocean.

text: He was the elder brother of the Masonic author Albert Churchward (1852–1925.) He was a tea planter in

text: Sri Lanka

text: before coming to the US in the 1890s. In James' biography entitled My Friend Churchey and His Sunken Continent, he discussed Mu with

text: Augustus Le Plongeon

text: and his wife in the 1890s. He patented NCV Steel, armor plating to protect ships during

text: World War I

text: , and other steel alloys. After a patent-infringement settlement in 1914, James retired to his 7+ acre estate on Lake Wononskopomuc in

text: Lakeville, Connecticut

text: , to answer the questions from his Pacific travels.  In 1926, at the age of 75, he published The Lost Continent of Mu: Motherland of Man, which he claimed proved the existence of a

text: lost continent

text: , called

text: Mu

text: , in the

text: Pacific Ocean

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answer: No

answer: No

answer: No

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answer: No

answer: 1

text: Proponents of the Snowball Earth theory claim that sometime before 650 million years ago the Earth was going through an extremely cold period. The oceans were frozen to great depths, and their snow covering reflected the heat from the sun through cloudless skies. Only simple forms of life could survive in locations such as deep oceanic hydrothermal vents. At the end of this period the edges of the West African craton became highly active, throwing up a ring of volcanoes. The thermal activity was caused by excessive mantle heat that had built up below the craton, insulated by the lithosphere. The volcanic eruptions created a greenhouse effect on massive scale, melting the ice and releasing CO into the atmosphere. The climate quickly switched to one much warmer than today, resulting in the Cambrian explosion of life forms.

text: Proponents of the

text: Snowball Earth

text: theory claim that sometime before 650 million years ago the Earth was going through an extremely cold period. The oceans were frozen to great depths, and their snow covering reflected the heat from the sun through cloudless skies. Only simple forms of life could survive in locations such as deep oceanic

text: hydrothermal vents

text: . At the end of this period the edges of the West African craton became highly active, throwing up a ring of

text: volcanoes

text: . The thermal activity was caused by excessive

text: mantle

text: heat that had built up below the craton, insulated by the

text: lithosphere

text: . The volcanic eruptions created a

text: greenhouse effect

text: on massive scale, melting the ice and releasing CO into the atmosphere. The climate quickly switched to one much warmer than today, resulting in the

text: Cambrian explosion

text: of life forms.

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answers: mantle

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answers: West African craton

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answers: lithosphere

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answers: 650 million years ago

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In other languages, however, there is no possibility for confusion. For example, the Chinese word for "U.S. national" is  () is derived from a word for the United States, , where  is an abbreviation for Yàměilìjiā ("America") and  is "country". The name for the American continents is , from  plus  ("continent"). Thus, a  is an American in the continent sense, and a  is an American in the U.S. sense.

text: In other languages, however, there is no possibility for confusion. For example, the

text: Chinese

text: word for "U.S. national" is  () is derived from a word for the United States, , where  is an abbreviation for Yàměilìjiā ("America") and  is "country". The name for the American continents is , from  plus  ("continent"). Thus, a  is an American in the continent sense, and a  is an American in the U.S. sense.

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answers: Zircons indicate that there was water

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answer: No

answer: No

answer: No

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text: 1982, he started his political activities from the platform of student union. In this tenure, he also participated in left-wing movement. In 1986, he joined trade union being as an activist. He is working in trade union movement since 1986. He has honour to work with the founder of Labour Movement in Sub-Continent Mr. Mirza Mohammad Ibrahim (Late).

text: 1982, he started his political activities from the platform of student union. In this tenure, he also participated in left-wing movement. In 1986, he joined

text: trade union

text: being as an activist. He is working in trade union movement since 1986. He has honour to work with the founder of Labour Movement in Sub-Continent Mr. Mirza Mohammad Ibrahim (Late).

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answers: He is working in trade union movement since 1986

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answers: Sub-Continent

answer: No

answer: No

answer: No

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text: A shield is that part of the continental crust in which these usually Precambrian basement rocks crop out extensively at the surface. Shields themselves can be very complex: they consist of vast areas of granitic or granodioritic gneisses, usually of tonalitic composition, and they also contain belts of sedimentary rocks, often surrounded by low-grade volcano-sedimentary sequences, or greenstone belts. These rocks are frequently metamorphosed greenschist, amphibolite, and granulite facies.

text: A shield is that part of the

text: continental

text: crust in which these usually

text: Precambrian

text: basement rock

text: s crop out extensively at the surface. Shields themselves can be very complex: they consist of vast areas of

text: granitic

text: or

text: granodioritic

text: gneiss

text: es, usually of

text: tonalitic

text: composition, and they also contain belts of

text: sedimentary

text: rocks, often surrounded by low-grade volcano-sedimentary sequences, or

text: greenstone belts

text: . These rocks are frequently

text: metamorphose

text: d

text: greenschist

text: amphibolite

text: , and

text: granulite

text: facies

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answers: Precambrian

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answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: In the Cambrian period, the continent of Laurentia, which would later become North America, sat on the equator, with three bordering oceans: the Panthalassic Ocean to the north and west, the Iapetus Ocean to the south and the Khanty Ocean to the east. In the Earliest Ordovician, around 480 Ma, the microcontinent of Avalonia – a landmass incorporating fragments of what would become eastern Newfoundland, the southern British Isles, and parts of Belgium, northern France, Nova Scotia, New England, Iberia and northwest Africa – broke free from Gondwana and began its journey to Laurentia. Baltica, Laurentia, and Avalonia all came together by the end of the Ordovician to form a minor supercontinent called Euramerica or Laurussia, closing the Iapetus Ocean. The collision also resulted in the formation of the northern Appalachians. Siberia sat near Euramerica, with the Khanty Ocean between the two continents. While all this was happening, Gondwana drifted slowly towards the South Pole. This was the first step of the formation of Pangaea.

text: In the

text: Cambrian

text: period, the continent of

text: Laurentia

text: , which would later become

text: North America

text: , sat on the

text: equator

text: , with three bordering oceans: the

text: Panthalassic Ocean

text: to the north and west, the

text: Iapetus Ocean

text: to the south and the

text: Khanty Ocean

text: to the east. In the Earliest

text: Ordovician

text: , around 480 Ma, the microcontinent of

text: Avalonia

text: – a landmass incorporating fragments of what would become eastern

text: Newfoundland

text: , the southern

text: British Isles

text: , and parts of

text: Belgium

text: , northern

text: France

text: Nova Scotia

text: New England

text: Iberia

text: and northwest Africa – broke free from Gondwana and began its journey to

text: Laurentia

text: . Baltica, Laurentia, and Avalonia all came together by the end of the Ordovician to form a minor supercontinent called

text: Euramerica

text: or Laurussia, closing the Iapetus Ocean. The collision also resulted in the formation of the northern

text: Appalachians

text: Siberia

text: sat near Euramerica, with the

text: Khanty Ocean

text: between the two continents. While all this was happening, Gondwana drifted slowly towards the South Pole. This was the first step of the formation of Pangaea.

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answer: Yes

answer: Yes

answer: No

answer: No

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answer: 1

text: Physiologist Jared Diamond was inspired to write his Pulitzer Prize-winning work Guns, Germs, and Steel by a question posed by Yali, a New Guinean politician: why were Europeans so much wealthier than his people? In this book, Diamond argues that the Europe-Asia land mass is particularly favorable for the transition of societies from hunter-gatherer to farming communities. This continent stretches much further along the same lines of latitude than any of the other continents. Since it is much easier to transfer a domesticated species along the same latitude than it is to move it to a warmer or colder climate, any species developed at a particular latitude will be transferred across the continent in a relatively short amount of time. Thus the inhabitants of the Eurasian continent have had a built-in advantage in terms of earlier development of farming, and a greater range of plants and animals from which to choose.

text: Physiologist

text: Jared Diamond

text: was inspired to write his

text: Pulitzer Prize

text: -winning work

text: Guns, Germs, and Steel

text: by a question posed by

text: Yali

text: , a

text: New Guinea

text: n politician: why were Europeans so much wealthier than his people? In this book, Diamond argues that the

text: Europe

text: Asia

text: land mass is particularly favorable for the transition of societies from

text: hunter-gatherer

text: to farming communities. This continent stretches much further along the same lines of latitude than any of the other continents. Since it is much easier to transfer a domesticated species along the same latitude than it is to move it to a warmer or colder climate, any species developed at a particular latitude will be transferred across the continent in a relatively short amount of time. Thus the inhabitants of the Eurasian continent have had a built-in advantage in terms of earlier development of farming, and a greater range of plants and animals from which to choose.

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answers: Eurasian

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answers: Zircons indicate that there was water in the environment

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answers: earlier development of farming

answer: No

answer: No

answer: No

answer: No

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answer: 1

text: It is unclear whether Craton and the work credited to him by Pseudo-Abdias actually existed, or whether this Craton was invented to lend the pseudepigrapha greater legitimacy.

text: It is unclear whether Craton and the work credited to him by Pseudo-Abdias actually existed, or whether this Craton was invented to lend the

text: pseudepigrapha

text: greater legitimacy.

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answers: Zircons indicate that there was water in the environment

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answer: No

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answer: No

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text: Originally the Earth (Arda) was flat, the continents were surrounded by a mighty ocean (or perhaps by space), Ekkaia or Vaiya, the Encircling Sea. The central and western continents - respectively Middle-earth and Aman - were separated by Belegaer, also called the Great Sea and the Sundering Seas. In the First Age, the area in the northwest of Middle-earth was occupied by the large region of Beleriand, but this was mostly destroyed and submerged in the War of Wrath at the end of that Age.

text: Originally the Earth (Arda) was flat, the continents were surrounded by a mighty

text: ocean

text: (or perhaps by

text: space

text: Ekkaia

text: or Vaiya, the Encircling Sea. The central and western continents - respectively

text: Middle-earth

text: and

text: Aman

text: - were separated by

text: Belegaer

text: , also called the Great Sea and the Sundering Seas. In the

text: First Age

text: , the area in the northwest of Middle-earth was occupied by the large region of

text: Beleriand

text: , but this was mostly destroyed and submerged in the

text: War of Wrath

text: at the end of that Age.

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answers: are surrounded by a mighty ocean

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answers: sedimentary rock

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answers: Originally

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: The paleogeography was dominated by the supercontinent of Gondwana to the south, the continent of Siberia to the north, and the early formation of the small continent of Euramerica in between.

text: The

text: paleogeography

text: was dominated by the

text: supercontinent

text: of

text: Gondwana

text: to the south, the

text: continent

text: of

text: Siberia

text: to the north, and the early formation of the small continent of

text: Euramerica

text: in between.

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answers: Siberia

answers: NDQ_005572

answers: Gondwana

answers: NDQ_005573

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answers: NDQ_005575

answers: Gondwana

answers: NDQ_005576

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answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: paleogeography

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Also, many continents can consist of several continental cratons - blocks of crust built around an initial original core of continents, that gradually grew and expanded as additional newly created terranes were added to their edges. For instance, Pangea consisted of most of the Earth's continents being accreted into one giant supercontinent. Most continents indeed have several continental cratons, in other words they are made up of the accretion of many smaller continents, such as Asia, Africa, and Europe.

text: Also, many continents can consist of several continental

text: craton

text: s - blocks of crust built around an initial original core of continents, that gradually grew and expanded as additional newly created terranes were added to their edges. For instance,

text: Pangea

text: consisted of most of the Earth's continents being accreted into one giant

text: supercontinent

text: . Most continents indeed have several continental cratons, in other words they are made up of the accretion of many smaller continents, such as

text: Asia

text: Africa

text: , and

text: Europe

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answers: NDQ_005571

answers: core of continents

answers: NDQ_005572

answers: Pangea

answers: NDQ_005573

answers: accretion of many smaller continents

answers: NDQ_005574

answers: blocks of crust

answers: NDQ_005575

answers: blocks of crust built around an initial original core

answers: NDQ_005576

answers: continental cratons

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Pangea

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: About 1 billion years ago, the earth was producing massive amounts of molten rock that would one day amalgamate, drift together and combine, to ultimately form the continents we live on today. In the Colorado region, this molten rock spewed and cooled, forming what we now know as the Precambrian Pikes Peak Granite. Over the next 500 million years, little is known about changes in the sedimentation (sediment deposition) after the granite was produced.  However, at about 500 – 300 million years ago, the region began to sink and sediments began to deposit in the newly formed accommodation space. Eroded granite produced sand particles that began to form strata, layers of sediment, in the sinking basin. Sedimentation would continue to take place until about 300 million years ago.

text: About 1 billion years ago, the earth was producing massive amounts of molten rock that would one day

text: amalgamate

text: , drift together and combine, to ultimately form the continents we live on today. In the Colorado region, this molten rock spewed and cooled, forming what we now know as the

text: Precambrian

text: Pikes Peak

text: Granite. Over the next 500 million years, little is known about changes in the

text: sedimentation

text: (sediment deposition) after the granite was produced.  However, at about 500 – 300 million years ago, the region began to sink and sediments began to deposit in the newly formed accommodation space. Eroded granite produced sand particles that began to form strata, layers of sediment, in the sinking basin. Sedimentation would continue to take place until about 300 million years ago.

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answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Pikes Peak Granite

answers: NDQ_005573

answers: the earth was producing massive amounts of molten rock

answers: NDQ_005574

answers: continents

answers: NDQ_005575

answers: 1 billion years ago

answers: NDQ_005576

answers: strata

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: 1 billion years ago

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: Early in the Ordovician, the continents of Laurentia (in present-day North America), Siberia, and Baltica (present-day northern Europe) were still independent continents (since the break-up of the supercontinent Pannotia earlier), but Baltica began to move towards Laurentia later in the period, causing the Iapetus Ocean between them to shrink. The small continent Avalonia separated from Gondwana and began to move north towards Baltica and Laurentia, opening the Rheic Ocean between Gondwana and Avalonia.

text: Early in the Ordovician, the continents of

text: Laurentia

text: (in present-day

text: North America

text: Siberia

text: , and

text: Baltica

text: (present-day northern Europe) were still independent continents (since the break-up of the

text: supercontinent

text: Pannotia

text: earlier), but Baltica began to move towards Laurentia later in the period, causing the

text: Iapetus Ocean

text: between them to shrink. The small continent

text: Avalonia

text: separated from Gondwana and began to move north towards Baltica and Laurentia, opening the

text: Rheic Ocean

text: between Gondwana and Avalonia.

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answers: Pannotia

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answers: supercontinent Pannotia

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answers: the break-up of the supercontinent Pannotia

answers: NDQ_005576

answers: Iapetus Ocean

answers: NDQ_005577

answers: Iapetus Ocean

answers: NDQ_005579

answers: Ordovician

answer: No

answer: No

answer: Yes

answer: No

answer: Yes

answer: 1

text: The initial crust, formed when the Earth's surface first solidified, totally disappeared from a combination of this fast Hadean plate tectonics and the intense impacts of the Late Heavy Bombardment. However, it is thought that it was basaltic in composition, like today's oceanic crust, because little crustal differentiation had yet taken place. The first larger pieces of continental crust, which is a product of differentiation of lighter elements during partial melting in the lower crust, appeared at the end of the Hadean, about 4.0 Ga. What is left of these first small continents are called cratons. These pieces of late Hadean and early Archean crust form the cores around which today's continents grew.

text: The initial crust, formed when the Earth's surface first solidified, totally disappeared from a combination of this fast Hadean plate tectonics and the intense impacts of the Late Heavy Bombardment. However, it is thought that it was

text: basalt

text: ic in composition, like today's

text: oceanic crust

text: , because little crustal differentiation had yet taken place. The first larger pieces of

text: continental crust

text: , which is a product of differentiation of lighter elements during

text: partial melting

text: in the lower crust, appeared at the end of the Hadean, about 4.0 Ga. What is left of these first small continents are called

text: craton

text: s. These pieces of late Hadean and early Archean crust form the cores around which today's continents grew.

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answers: basaltic

answers: NDQ_005572

answers: the end of the Hadean

answers: NDQ_005573

answers: partial melting in the lower crust

answers: NDQ_005574

answers: What is left of these first small continents

answers: NDQ_005575

answers: 4.0 Ga

answers: NDQ_005576

answers: cratons

answers: NDQ_005577

answers: It is thought that it was basaltic in composition

answers: NDQ_005579

answers: Hadean

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The African Plate includes several cratons, stable blocks of old crust with deep roots in the subcontinental lithospheric mantle, and less stable terranes, which came together to form the African continent during the assembly of the supercontinent Pangea around 550 million years ago. The cratons are, from south to north, the Kalahari craton, Congo craton, Tanzania craton and West African craton. The cratons were widely separated in the past, but came together during the Pan-African orogeny and stayed together when Gondwana split up.The cratons are connected by orogenic belts, regions of highly deformed rock where the tectonic plates have engaged.The Saharan Metacraton has been tentatively identified as the remains of a craton that has become detached from the subcontinental lithospheric mantle, but alternatively may consist of a collection of unrelated crustal fragments swept together during the Pan-African orogeny.

text: The African Plate includes several

text: craton

text: s, stable blocks of old crust with deep roots in the

text: subcontinental lithospheric mantle

text: , and less stable

text: terranes

text: , which came together to form the African continent during the assembly of the

text: supercontinent

text: Pangea

text: around 550 million years ago. The cratons are, from south to north, the

text: Kalahari craton

text: Congo craton

text: Tanzania craton

text: and

text: West African craton

text: . The cratons were widely separated in the past, but came together during the

text: Pan-African orogeny

text: and stayed together when Gondwana split up.The cratons are connected by

text: orogenic belts

text: , regions of highly deformed rock where the

text: tectonic plates

text: have engaged.The

text: Saharan Metacraton

text: has been tentatively identified as the remains of a craton that has become detached from the subcontinental lithospheric mantle, but alternatively may consist of a collection of unrelated crustal fragments swept together during the Pan-African orogeny.

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answers: lithospheric mantle

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answers: Gondwana

answers: NDQ_005573

answers: stable blocks of old crust

answers: NDQ_005574

answers: The African Plate includes several cratons

answers: NDQ_005575

answers: 550 million years ago

answers: NDQ_005576

answers: orogenic belt

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: 550 million years ago

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: In the middle of December, twin monsoon troughs were established in the extreme western Pacific Ocean, which will later spawn storms Greg, and Fern itself in the northern hemisphere. The trough in the southern hemisphere spawned cyclones Ophelia, Phil, and Fergus. Around that time, convection began to increase near the equator, and was associated with a westerly wind burst. A low level circulation center was noted by JTWC on December 19 at 0600 UTC. Two days later, convection consolidated near the circulation center, and JMA began tracking it at 0000 UTC as a tropical depression.

text: In the middle of December, twin

text: monsoon trough

text: s were established in the extreme western Pacific Ocean, which will later spawn storms

text: Greg

text: , and Fern itself in the northern hemisphere. The trough in the southern hemisphere spawned cyclones

entity_name: 1996–97 Australian region cyclone season

text: Ophelia

text: Phil

text: , and

text: Fergus

text: . Around that time, convection began to increase near the equator, and was associated with a

text: westerly wind burst

text: . A low level circulation center was noted by JTWC on December 19 at 0600

text: UTC

text: . Two days later, convection consolidated near the circulation center, and JMA began tracking it at 0000 UTC as a tropical depression.

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answers: 0

answers: NDQ_005571

answers: igneous

answers: NDQ_005572

answers: extreme western Pacific Ocean

answers: NDQ_005573

answers: troughs

answers: NDQ_005574

answers: Pacific Ocean

answers: NDQ_005575

answers: Pacific Ocean

answers: NDQ_005576

answers: tropical depression

answers: NDQ_005577

answers: yes

answers: NDQ_005579

answers: the equator

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Bolshoy Lyakhovsky Island consists of highly folded and faulted Precambrian metamorphic rocks and turbidites; Mesozoic turbidites and igneous rocks; and Cenozoic sediments. Exposed in southeastern part of this island, the older Precambrian. Early Proterozoic, metamorphic rocks consist of schists and amphibolites. Small exposures of Late Proterozoic schistose, quartzose sandstones and phyllitic, sericite-quartz schist (turbidites) also occur in the southeastern part of Bolshoy Lyakhovsky Island. The bulk of this island consists of Late Jurassic to Early Cretaceous turbidites composed of interbedded fine-grained sandstones, thinly bedded siltstones, and argillites. The Precambrian and Late Jurassic to Early Cretaceous rocks are intruded by Late Cretaceous granites and granodiorites.

text: Bolshoy Lyakhovsky Island consists of highly folded and faulted

text: Precambrian

text: metamorphic rock

text: s and

text: turbidites

text: Mesozoic

text: turbidites and

text: igneous

text: rocks; and

text: Cenozoic

text: sediments

text: . Exposed in southeastern part of this island, the older Precambrian. Early

text: Proterozoic

text: , metamorphic rocks consist of

text: schist

text: s and

text: amphibolite

text: s. Small exposures of Late Proterozoic schistose, quartzose

text: sandstone

text: s and phyllitic,

text: sericite

text: quartz

text: schist (turbidites) also occur in the southeastern part of Bolshoy Lyakhovsky Island. The bulk of this island consists of Late

text: Jurassic

text: to Early

text: Cretaceous

text: turbidites composed of interbedded fine-grained sandstones, thinly bedded

text: siltstone

text: s, and

text: argillite

text: s. The Precambrian and Late Jurassic to Early Cretaceous rocks are intruded by Late Cretaceous

text: granite

text: s and granodiorites.

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answers: Precambrian

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answers: Precambrian

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answers: Precambrian

answers: NDQ_005574

answers: Late Cretaceous granites

answers: NDQ_005575

answers: Bolshoy Lyakhovsky Island

answers: NDQ_005576

answers: turbidites

answers: NDQ_005577

answers: turbidites

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answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: As wind shear increased and convection became disorganized, Paul weakened. A trough briefly curved it to the northwest, before resuming its westward motion. Although the convection was becoming displaced from the low-level circulation, the National Hurricane Center continued to predict strengthening. However, the thunderstorms became minimal, and Paul weakened to a tropical depression early on October 28. The circulation center deteriorated, and although there were bursts in convection, Paul dissipated early on October 29, as it was becoming indistinguishable in the ITCZ. The remnants continued westward, and interacted with an upper-level low, affecting Hawaii with heavy rainfall in early November. The flooding caused $70 million in damage, and the highest rainfall total was  at Kapapala Ranch. That rainfall total makes Paul the second rainiest tropical cyclone in Hawaii, behind only Hurricane Hiki of 1950.

text: As wind shear increased and convection became disorganized, Paul weakened. A trough briefly curved it to the northwest, before resuming its westward motion. Although the convection was becoming displaced from the low-level circulation, the National Hurricane Center continued to predict strengthening. However, the thunderstorms became minimal, and Paul weakened to a tropical depression early on October 28. The circulation center deteriorated, and although there were bursts in convection, Paul dissipated early on October 29, as it was becoming indistinguishable in the ITCZ. The remnants continued westward, and interacted with an upper-level low, affecting Hawaii with heavy rainfall in early November. The flooding caused $70 million in damage, and the highest rainfall total was  at

text: Kapapala Ranch

text: . That rainfall total makes Paul the second rainiest tropical cyclone in Hawaii, behind only

text: Hurricane Hiki

text: of 1950.

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answers: It indicates that there was water in the environment

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answers: 1950

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: At about 2.5 and 1.8 billion years ago in Precambrian time, sand, mud, silt, and ash were laid down in a marine basin adjacent to an orogenic belt. From 1.8 to 1.6 billion years ago at least two island arcs collided with the proto-North American continent. This process of plate tectonics compressed and grafted the marine sediments in the basin onto the mainland and uplifted them out of the sea. Later, these rocks were buried  under the surface and pressure-cooked into metamorphic rock. The resulting Granite Gorge Metamorphic Suite, which is part of the Vishnu Basement Rocks, consists of the metasedimentary Vishnu Schist and the metavolcanic Brahma and Rama Schists that were formed 1.75 billion to 1.73 billion years ago. This is the resistant rock now exposed at the bottom of the canyon in the Inner Gorge.

text: At about 2.5 and 1.8 billion years ago in

text: Precambrian

text: time,

text: sand

text: mud

text: silt

text: , and

text: ash

text: were laid down in a marine basin adjacent to an

text: orogenic belt

text: . From 1.8 to 1.6 billion years ago at least two

text: island arc

text: s collided with the proto-North American

text: continent

text: . This process of

text: plate tectonics

text: compressed and grafted the marine sediments in the basin onto the mainland and uplifted them out of the sea. Later, these rocks were buried  under the surface and pressure-cooked into

text: metamorphic rock

text: . The resulting

text: Granite Gorge Metamorphic Suite

text: , which is part of the

text: Vishnu Basement Rocks

text: , consists of the metasedimentary Vishnu Schist and the metavolcanic Brahma and Rama Schists that were formed 1.75 billion to 1.73 billion years ago. This is the resistant rock now exposed at the bottom of the canyon in the Inner Gorge.

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answers: Precambrian

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answers: the proto-North American continent

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answers: plate tectonics

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answers: island arcs

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answers: 2.5 and 1.8 billion years

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answers: basement rocks

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answers: marine basin

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answers: 2.5 and 1.8 billion years ago

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: The current geological structure of the Arctic Region is the result of tectonic processes during the Mesozoic and Cenozoic (250 Ma to present) when the Amerasian and Eurasian basins formed, but the presence of Precambrian metamorphic complexes discovered in the 1980s indicated a continent once existed between Laurentia, Baltica, and Siberia.

text: The current geological structure of the Arctic Region is the result of tectonic processes during the Mesozoic and Cenozoic (250 Ma to present) when the

text: Amerasian

text: and

text: Eurasian

text: basins formed, but the presence of Precambrian metamorphic complexes discovered in the 1980s indicated a continent once existed between

text: Laurentia

text: Baltica

text: , and

text: Siberia

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answers: Precambrian

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answers: Precambrian

answers: NDQ_005573

answers: a continent once existed

answers: NDQ_005574

answers: tectonic processes

answers: NDQ_005575

answers: a continent once existed

answers: NDQ_005576

answers: complexes

answers: NDQ_005577

answers: Amerasian and Eurasian basins

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Micro-continent model is suggested by Thomas and Astini. Saying that Precordillera origins from Laurentia as the south-east of Ouachita Embayment. It was detached by Ouachita Rift since Early Cambrian. After that Precordillera acts as an independent continent traveling through the Iapetus Ocean along the Alabama-Oklahoma transform fault. Finally the continent collides to Gondwana continent at middle Ordovician, changing the environment from passive margin to extensive rifting. This model is strongly supported by the thick carbonate complex as well as matching faunas records.

text: Micro-continent model is suggested by Thomas and Astini. Saying that

text: Precordillera

text: origins from

text: Laurentia

text: as the south-east of Ouachita Embayment. It was detached by

text: Ouachita

text: Rift since Early

text: Cambrian

text: . After that

text: Precordillera

text: acts as an independent continent traveling through the Iapetus Ocean along the Alabama-Oklahoma transform fault. Finally the continent collides to

text: Gondwana

text: continent at middle

text: Ordovician

text: , changing the environment from

text: passive margin

text: to extensive

text: rift

text: ing. This model is strongly supported by the thick carbonate complex as well as matching faunas records.

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answers: 0

answers: NDQ_005571

answers: Carbonate

answers: NDQ_005572

answers: Laurentia

answers: NDQ_005573

answers: Late Cambrian

answers: NDQ_005574

answers: Precordillera

answers: NDQ_005575

answers: Early Cambrian

answers: NDQ_005576

answers: Rift

answers: NDQ_005577

answers: Iapetus Ocean

answers: NDQ_005579

answers: Early Cambrian

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Badilisha Poetry X-Change is a platform dedicated to showcasing poetry from Africa and the African Diaspora. The project came out of recognising the lack of documentation of African poets, on the African continent and in the rest of the world. Its aims are to fill this void as well as create a comprehensive global archive of Pan-African poets that can accessed internationally. First launched in 2008 as a poetry festival, the Spier Poetry Exchange. by nonprofit organisation Africa Centre in Cape Town, the festival centred on various aspects of developing, celebrating, archiving and documenting poetry and voices. In 2009, the Spier Poetry Exchange changed to the Badilisha Poetry X-Change (taking its name from the kiSwahili expression "Badilisha", which means to change, exchange and transform). Although different in name, Badilisha Poetry X-Change continues the "exchange" between poets, creating spaces and platforms for programmed poetry interventions, workshops and presentations. Its existence continues to provide new and established Pan-African voices a space of celebration, documentation, proliferation, and self-reflection.

text: Badilisha Poetry X-Change is a platform dedicated to showcasing poetry from Africa and the

text: African Diaspora

text: . The project came out of recognising the lack of documentation of African poets, on the African continent and in the rest of the world. Its aims are to fill this void as well as create a comprehensive global archive of Pan-African poets that can accessed internationally. First launched in 2008 as a poetry festival, the Spier Poetry Exchange. by nonprofit organisation

text: Africa Centre

text: in

text: Cape Town

text: , the festival centred on various aspects of developing, celebrating, archiving and documenting poetry and voices. In 2009, the Spier Poetry Exchange changed to the Badilisha Poetry X-Change (taking its name from the

text: kiSwahili

text: expression "Badilisha", which means to change, exchange and transform). Although different in name, Badilisha Poetry X-Change continues the "exchange" between poets, creating spaces and platforms for programmed poetry interventions, workshops and presentations. Its existence continues to provide new and established Pan-African voices a space of celebration, documentation, proliferation, and self-reflection.

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answer: No

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text: Natural convection has attracted a great deal of attention from researchers because of its presence both in nature and engineering applications. In nature, convection cells formed from air raising above sunlight-warmed land or water are a major feature of all weather systems. Convection is also seen in the rising plume of hot air from fire, oceanic currents, and sea-wind formation (where upward convection is also modified by Coriolis forces). In engineering applications, convection is commonly visualized in the formation of microstructures during the cooling of molten metals, and fluid flows around shrouded heat-dissipation fins, and solar ponds. A very common industrial application of natural convection is free air cooling without the aid of fans: this can happen on small scales (computer chips) to large scale process equipment.

text: Natural convection has attracted a great deal of attention from researchers because of its presence both in nature and engineering applications. In nature, convection cells formed from air raising above sunlight-warmed land or water are a major feature of all weather systems. Convection is also seen in the rising plume of hot air from

text: fire

text: , oceanic currents, and sea-wind formation (where upward convection is also modified by

text: Coriolis force

text: s). In engineering applications, convection is commonly visualized in the formation of microstructures during the cooling of molten metals, and fluid flows around shrouded heat-dissipation fins, and solar ponds. A very common industrial application of natural convection is free air cooling without the aid of fans: this can happen on small scales (computer chips) to large scale process equipment.

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text: In 1978 the public lane known as Victoria Street extending south from Gould was closed to vehicle traffic. The southeasterly corner of at this intersection was originally a parking lot. This space now forms part of Devonian Square and features a reflecting pond, which is used as a skating rink in the winter. Devonian Square is owned by Ryerson but is maintained by the City of Toronto Parks, Forestry and Recreation. The park was designed in 1978 by Toronto landscape architecture firm Richard Strong, Steven Moorhead Ltd. Design and construction of the square was partially funded by the Devonian Group of Charitable Foundations of Calgary — lending the park its name. The space features huge Precambrian igneous and metamorphic rocks that are approximately two billion years old. These were trucked in from the Canadian Shield.

text: In 1978 the public lane known as Victoria Street extending south from Gould was closed to vehicle traffic. The southeasterly corner of at this intersection was originally a parking lot. This space now forms part of Devonian Square and features a reflecting pond, which is used as a skating rink in the winter. Devonian Square is owned by Ryerson but is maintained by the

entity_name: Toronto Parks, Forestry and Recreation Division

text: City of Toronto Parks, Forestry and Recreation

text: . The park was designed in 1978 by Toronto landscape architecture firm

text: Richard Strong, Steven Moorhead Ltd

text: . Design and construction of the square was partially funded by the Devonian Group of Charitable Foundations of

text: Calgary

text: — lending the park its name. The space features huge

text: Precambrian

text: igneous

text: and

text: metamorphic

text: rocks that are approximately two billion years old. These were trucked in from the

text: Canadian Shield

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answers: Devonian

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answers: the Canadian Shield

answers: NDQ_005573

answers: two billion years old

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answers: two billion years old

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answers: Devonian

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answer: 1

text: Precambrian metamorphic rock formed the core of the North American continent during the Precambrian eon 4.5–1 billion years ago. During the Paleozoic era, western North America lay underneath a shallow sea, with many kilometers of limestone and dolomite deposits. Precambrian Pikes Peak Granite formed during Paleozoic era and the Precambrian eon, about 300 million–1 billion years ago, when mass quantities of molten rock flowed, amalgamated, and formed the continents. At about 500 – 300 million years ago, the region began to sink and lime and mud sediments deposited in the newly formed space. Eroded granite produced sand particles that formed strata, layers of sediment, in the sinking basin.

text: Precambrian

text: metamorphic rock

text: formed the core of the North American continent during the Precambrian eon 4.5–1 billion years ago. During the

text: Paleozoic

text: era, western North America lay underneath a shallow sea, with many kilometers of

text: limestone

text: and

text: dolomite

text: deposits. Precambrian Pikes Peak Granite formed during Paleozoic era and the Precambrian eon, about 300 million–1 billion years ago, when mass quantities of molten rock flowed, amalgamated, and formed the continents. At about 500 – 300 million years ago, the region began to sink and lime and mud sediments deposited in the newly formed space. Eroded granite produced sand particles that formed strata, layers of sediment, in the sinking basin.

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answers: Precambrian

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answers: Precambrian

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answers: mass quantities of molten rock

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answers: continents

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answers: 300 million–1 billion years ago

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answers: strata

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answers: During the Paleozoic era

answers: NDQ_005579

answers: the Paleozoic era

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Sierra Ballena Shear Zone or SBSZ is a sinistral strike-slip shear zone running across the Uruguayan Shield in eastern Uruguay and the Brazilian state of Rio Grande do Sul. The system was last active in the Precambrian.

text: Sierra Ballena Shear Zone or SBSZ is a

text: sinistral strike-slip

text: shear zone

text: running across the

text: Uruguayan Shield

text: in eastern

text: Uruguay

text: and the Brazilian state of

text: Rio Grande do Sul

text: . The system was last active in the

text: Precambrian

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answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: the Precambrian

answers: NDQ_005574

answers: Precambrian

answers: NDQ_005575

answers: Uruguayan Shield

answers: NDQ_005576

answers: SBSZ

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: Prior to the Svecobaltic orogeny proper there was period of northward-directed subduction at what is now south-central Sweden and southern Finland. The subduction lasted from 1860 to 1840 million years ago and was accompanied by magmatic activity. Two trends in the southern Svecofennian orogen variously overlapped in time and space: extension (1870 to 1840 million years ago) and continent-continent collision (1870 to 1790 million years ago).  Magmatic activity and metamorphism in southern Finland ended gradually after 1870 millions years ago. The orogen at southern Finland with its presumed mountains and thick continental crust collapsed under the influence of gravity and spread out. By 1850 millions years ago this collapse had evolved to a dynamic of extensional tectonics. In this extensional milieu short-lived sedimentary basins formed. The Svecobaltic orogeny developed when subduction bought the Fennoscandian Craton into an oblique collision with the Sarmatian Craton. The mentioned sedimentary basins were destroyed by basin inversion 1830 million years ago. This last event of basin inversion was associated with a period of metamorphism in southern Finland that peaked about 1820 million years ago.

text: Prior to the Svecobaltic orogeny proper there was period of northward-directed subduction at what is now south-central Sweden and southern Finland. The subduction lasted from 1860 to 1840 million years ago and was accompanied by

text: magmatic activity

text: . Two trends in the southern Svecofennian orogen variously overlapped in time and space:

text: extension

text: (1870 to 1840 million years ago) and

text: continent-continent collision

text: (1870 to 1790 million years ago).

text: Magmatic activity

text: and metamorphism in southern Finland ended gradually after 1870 millions years ago. The orogen at southern Finland with its presumed mountains and thick

text: continental crust

text: collapsed under the influence of gravity and spread out. By 1850 millions years ago this collapse had evolved to a dynamic of

text: extensional tectonics

text: . In this extensional milieu short-lived

text: sedimentary basin

text: s formed. The Svecobaltic orogeny developed when subduction bought the Fennoscandian Craton into an oblique collision with the

text: Sarmatian Craton

text: . The mentioned sedimentary basins were destroyed by

text: basin inversion

text: 1830 million years ago. This last event of basin inversion was associated with a period of metamorphism in southern Finland that peaked about 1820 million years ago.

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answers: Fennoscandian

answers: NDQ_005572

answers: Fennoscandian Craton

answers: NDQ_005573

answers: magmatic activity

answers: NDQ_005574

answers: Fennoscandian Craton

answers: NDQ_005575

answers: 1820 million years ago

answers: NDQ_005576

answers: basin inversion

answers: NDQ_005577

answers: short-lived sedimentary basins

answers: NDQ_005579

answers: 1820 million years ago

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: CitCom was originally written in the early 1990s by Louis Moresi (Monash U.). Although the code for three-dimensional problems was incorporated from its inception, early versions of the software only solved for time-dependent convection problems within two-dimensional Cartesian domains. Moresi's original code turned out to be incredibly modular and easily extensible. Consequently, the fundamental finite element infrastructure which Louis wrote is still in place and forms the basis for much of the code contained in the present release.

text: CitCom was originally written in the early 1990s by

text: Louis Moresi

text: (Monash U.). Although the code for three-dimensional problems was incorporated from its inception, early versions of the software only solved for time-dependent convection problems within two-dimensional Cartesian domains. Moresi's original code turned out to be incredibly modular and easily extensible. Consequently, the fundamental finite element infrastructure which Louis wrote is still in place and forms the basis for much of the code contained in the present release.

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text: The fluted stone tool variants of South America represent regional adaptations to the procurement of Pleistocene megafauna that contrasts with the continent-wide use of Clovis points in North America. Such regional technological adaptations seem to reflect the initial dispersal of small paleoindian groups throughout the vast continent. The fishtail points of Cueva Fell thus represent crucial evidence in the distinction between tool technologies in the southern and northern continents of the Americas.

text: The fluted stone tool variants of South America represent regional adaptations to the procurement of Pleistocene

text: megafauna

text: that contrasts with the continent-wide use of Clovis points in North America. Such regional technological adaptations seem to reflect the initial dispersal of small paleoindian groups throughout the vast continent. The fishtail points of Cueva Fell thus represent crucial evidence in the distinction between tool technologies in the southern and northern continents of the Americas.

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answers: stone

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answers: Pleistocene

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answers: Zircons indicate that there was water in the environment

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answers: Pleistocene

answer: Yes

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text: Most stations have island platforms, although Braddell MRT Station and Dover MRT Station have side platforms. This is because island platforms are seen to be less costly than side platforms, or possibly to make it convenient for passengers to transfer to another train on the same line but running in the opposite direction. Also, all stations are made to be as straight as possible because the degree that trains would turn at when approaching and leaving a station would be too great if curved stations were built. A good example of this engineering defect is seen at Mong Kok East Station in Hong Kong, where Platform 1 of this station (to the left if travelling to the Hong Kong-China border) is curved and the gaps are wide. Trains also risk being scratched depending on how it enters the station.

text: Most stations have

text: island platforms

text: , although Braddell MRT Station and Dover MRT Station have

text: side platforms

text: . This is because island platforms are seen to be less costly than side platforms, or possibly to make it convenient for passengers to transfer to another train on the same line but running in the opposite direction. Also, all stations are made to be as straight as possible because the degree that trains would turn at when approaching and leaving a station would be too great if curved stations were built. A good example of this engineering defect is seen at

text: Mong Kok East Station

text: in

text: Hong Kong

text: , where Platform 1 of this station (to the left if travelling to the

text: Hong Kong-China border

text: ) is curved and the gaps are wide. Trains also risk being scratched depending on how it enters the station.

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text: A tropical wave moved off the coast of Africa on July 7. The wave moved west, but it was not until it moved across the Caribbean Sea that the wave's convection organized. The system entered into the northeastern Pacific Ocean with concentrated convection and a surface center of circulation while southeast of Acapulco. Moving west-northwest, Tropical Depression Ten-E formed on July 20  south of Puerto Ángel, Mexico. Early on the following day, the depression strengthened into Tropical Storm Iselle. The storm continued strengthening while in the proximity of Hurricane Hernan, becoming a hurricane on July 22.

text: A tropical wave moved off the coast of Africa on July 7. The wave moved west, but it was not until it moved across the Caribbean Sea that the wave's convection organized. The system entered into the northeastern Pacific Ocean with concentrated convection and a surface center of circulation while southeast of Acapulco. Moving west-northwest, Tropical Depression Ten-E formed on July 20  south of

text: Puerto Ángel

text: , Mexico. Early on the following day, the depression strengthened into Tropical Storm Iselle. The storm continued strengthening while in the proximity of Hurricane Hernan, becoming a hurricane on July 22.

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text: Platform 1 is used by southbound trains from Derry or Portrush on their way to Great Victoria Street. Platform 2 tends to be used for Enterprise services to Dublin. Platform 3 is a bi-directional platform used for northbound trains heading to Derry, Portrush and Bangor, and by trains coming from Bangor en route to Portadown via Great Victoria Street and Platform 4 is used for trains terminating off the Larne Line.

text: Platform 1 is used by southbound trains from

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text: or

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text: on their way to

entity_name: Belfast Great Victoria Street railway station

text: Great Victoria Street

text: . Platform 2 tends to be used for Enterprise services to

text: Dublin

text: . Platform 3 is a bi-directional platform used for northbound trains heading to Derry, Portrush and

entity_name: Bangor railway station (Northern Ireland)

text: Bangor

text: , and by trains coming from Bangor en route to

text: Portadown

text: via Great Victoria Street and Platform 4 is used for trains terminating off the

text: Larne Line

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text: ArtTogether stagesAt the current 2nd stage of the project people from all over the world contribute via Internet platform ArtTogether.com their drawings to allow them to become part of a new cultural code of a generation. They manifest their vision of and aspirations for an ideal world. New parts of installation are created using digital technologies on plastic eggs. No curator is supervising co-creators. To date, 380.000 people from 42 countries have taken part in the project.At the 3rd stage scheduled for 2017-2019 the global community will complete the project, creating 3.640.000 drawings via Internet platform and the entire installation will be demonstrated on all continents.

text: ArtTogether stagesAt the current 2nd stage of the project people from all over the world contribute via Internet platform ArtTogether.com their drawings to allow them to become part of a new cultural code of a generation. They manifest their vision of and aspirations for an ideal world. New parts of installation are created using digital technologies on plastic eggs. No curator is supervising co-creators. To date, 380.000 people from 42 countries have taken part in the project.At the 3rd stage scheduled for 2017-2019 the global community will complete the project, creating 3.640.000 drawings via Internet platform and the entire installation will be demonstrated on all continents.

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answers: The global community will complete the project, creating 3.640.000 drawings

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answers: Zircons indicate that there was water in the environment

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answers: At the current 2nd stage

answer: No

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text: The precambrian biosphere established by the Genesis probe would evolve subsequently on its own, potentially to compex lifeforms. The concepts of the Genesis Project carries a series of fundamental ethical and philosophical aspects, which have been discussed in the media.

text: The

text: precambrian

text: biosphere established by the Genesis probe would evolve subsequently on its own, potentially to

text: compex lifeforms

text: . The concepts of the Genesis Project carries a series of fundamental ethical and philosophical aspects, which have been discussed in the media.

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text: Trapping, tourism, and mining are the main industries of the area. This community is located in the Precambrian Shield.

text: Trapping

text: , tourism, and mining are the main industries of the area. This community is located in the

text: Precambrian Shield

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answers: Precambrian

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answers: Precambrian

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answer: No

answer: No

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text: During the late Silurian period Baltica then collided with Laurentia which is named the Scandian phase of the Caledonian Orogeny. Baltica was subducted below Laurentia forming the Caledonian Belt.  The Caledonian Orogeny caused the closure of the Iapetus Ocean when the continents and terranes of Laurentia, Baltica and Avalonia collided. The combined mass of the three continents formed a "new" continent: Laurussia or Euramerica. The Caledonian orogeny encompasses events that occurred from the Ordovician to Early Devonian, roughly 490–390 Ma. The basement formations of the North Sea were roughly formed during this Caledonian geosynclinal stage of the Cambrian - Devonian periods.  The Caledonian mountains range helped create the ‘Old Red Sandstone’ continent at the joining of the tectonic plates.  The Rheic Ocean began to open to the south.

text: During the late

text: Silurian

text: period

text: Baltica

text: then collided with

text: Laurentia

text: which is named the Scandian phase of the

text: Caledonian Orogeny

text: . Baltica was subducted below Laurentia forming the Caledonian Belt.  The

text: Caledonian Orogeny

text: caused the closure of the

text: Iapetus Ocean

text: when the continents and

text: terrane

text: s of

text: Laurentia

text: Baltica

text: and

text: Avalonia

text: collided. The combined mass of the three continents formed a "new" continent:

text: Laurussia

text: or

text: Euramerica

text: . The Caledonian orogeny encompasses events that occurred from the

text: Ordovician

text: to Early

text: Devonian

text: , roughly 490–390

text: Ma

text: . The basement formations of the North Sea were roughly formed during this Caledonian

text: geosynclinal

text: stage of the

text: Cambrian

text: Devonian

text: periods.  The Caledonian mountains range helped create the ‘

text: Old Red Sandstone

text: ’ continent at the joining of the tectonic plates.  The

text: Rheic Ocean

text: began to open to the south.

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answers: Silurian

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answers: Silurian

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answers: 490–390 Ma

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answers: Laurentia

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answers: 490–390 Ma

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answers: late Silurian period

answer: No

answer: No

answer: No

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answer: 1

text: Sedimentary sequences show carbonate platforms as old as the Precambrian, when they were formed by stromatolitic sequences. In the Cambrian carbonate platforms were built by archaeocyatha, metazoa similar to porifera. During Paleozoic brachiopod (richtofenida) and stromatoporoidea reefs were erected. At the middle of the Paleozoic era corals became important platforms builders, first with tabulata (from the Silurian) and then with rugosa (from the Devonian). Scleractinia become important reef builders beginning only in the Carnian (upper Triassic). One of the best examples of a carbonate platform is the Dolomites, deposited during the Triassic. This region of the Southern Alps contains many well preserved atolls, including the Sella, Gardenaccia, Sassolungo and Latemar, the latter being a backstepping type platform. The middle Liassic "bahamian type" carbonate platform of Morocco (Septfontaine, 1985) is characterised by the accumulation of autocyclic regressive cycles and spectacular supratidal (top of sequences) deposits and vadose diagenetic features with dinosaur tracks. The Tunisian coastal "chotts" and their cyclic muddy deposits represent a good recent equivalent (Davaud & Septfontaine, 1995). Such cycles were also observed on the mesozoic Arabic platform, Oman and Abu Dhabi (Septfontaine & De Matos, 1998) with the same microfauna of foraminifera in an almost identical biostratigraphic succession.

text: Sedimentary sequences show carbonate platforms as old as the

text: Precambrian

text: , when they were formed by

text: stromatolitic

text: sequences. In the

text: Cambrian

text: carbonate platforms were built by archaeocyatha,

text: metazoa

text: similar to

text: porifera

text: . During

text: Paleozoic

text: brachiopod

text: (richtofenida) and

text: stromatoporoidea

text: reefs were erected. At the middle of the Paleozoic era corals became important platforms builders, first with tabulata (from the

text: Silurian

text: ) and then with rugosa (from the

text: Devonian

text: ). Scleractinia become important reef builders beginning only in the

text: Carnian

text: (upper

text: Triassic

text: ). One of the best examples of a carbonate platform is the

text: Dolomites

text: , deposited during the Triassic. This region of the Southern

text: Alps

text: contains many well preserved atolls, including the

text: Sella

text: Gardenaccia

text: Sassolungo

text: and

text: Latemar

text: , the latter being a backstepping type platform. The middle

text: Liassic

text: "bahamian type" carbonate platform of Morocco (Septfontaine, 1985) is characterised by the accumulation of autocyclic regressive cycles and spectacular supratidal (top of sequences) deposits and

text: vadose

text: diagenetic

text: features with dinosaur tracks. The Tunisian coastal "chotts" and their cyclic muddy deposits represent a good recent equivalent (Davaud & Septfontaine, 1995). Such cycles were also observed on the mesozoic Arabic platform, Oman and Abu Dhabi (Septfontaine & De Matos, 1998) with the same microfauna of foraminifera in an almost identical biostratigraphic succession.

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answers: Silurian

answers: NDQ_005572

answers: the Devonian

answers: NDQ_005573

answers: dinosaur tracks

answers: NDQ_005574

answers: Carbonate platforms

answers: NDQ_005575

answers: carbonate platforms

answers: NDQ_005576

answers: carbonate platform

answers: NDQ_005577

answers: Sedimentary sequences

answers: NDQ_005579

answers: the Precambrian

answer: No

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: Other early publishers across the continent included Alphonse Giroux & Compagnie in France and Trentsensky in Austria.

text: Other early publishers across the continent included

text: Alphonse Giroux

text: & Compagnie in France and Trentsensky in Austria.

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answers: Austria

answers: NDQ_005572

answers: Austria

answers: NDQ_005573

answers: greenstones in cratons

answers: NDQ_005574

answers: Trentsensky

answers: NDQ_005575

answers: Trentsensky

answers: NDQ_005576

answers: Trentsensky

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: during the last ice age

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Horizontal rolls are counter-rotating vortex rolls that are nearly aligned with the mean wind of the Planetary Boundary Layer (PBL). They can be caused by convection in the presence of a moderate wind and/or dynamic inflection point instabilities in the mean wind profile. Early theory on the features predict that the vortices may be aligned up to 30° to the left for stably stratified environments, 18° to the left for neutral environments, and nearly parallel to the mean wind for unstably stratified (convective) environments. This theory has been supported by aircraft observations from several field experiments.

text: Horizontal rolls are counter-rotating vortex rolls that are nearly aligned with the mean wind of the Planetary Boundary Layer (PBL). They can be caused by convection in the presence of a moderate wind and/or dynamic inflection point instabilities in the mean wind profile. Early theory on the features predict that the vortices may be aligned up to 30° to the left for stably stratified environments, 18° to the left for neutral environments, and nearly parallel to the mean wind for unstably stratified (convective) environments. This theory has been supported by aircraft observations from several field experiments.

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answers: 0

answers: NDQ_005571

answers: PBL

answers: NDQ_005572

answers: PBL

answers: NDQ_005573

answers: horizontal rolls

answers: NDQ_005574

answers: Horizontal rolls

answers: NDQ_005575

answers: Planetary Boundary Layer

answers: NDQ_005576

answers: stratified environments

answers: NDQ_005577

answers: This theory has been supported by aircraft observations from several field experiments

answers: NDQ_005579

answers: stratified environments

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: The NAKP kimberlite fields are aligned along a northeast-southwest trend for a distance of about , roughly subparallel to structural discontinuities called the Great Slave Lake Shear Zone to the north and the Snowbird Tectonic Zone to the south. They lie above or marginal to a 2.0 to 2.4 billion year old Precambrian craton called the Buffalo Head Terrane, which has no surface exposure. Near the fields the Precambrian rocks are overlain by about  to  of Phanerozoic sedimentary rocks, and covered by unconsolidated glacial and post-glacial sediments.

text: The NAKP kimberlite fields are aligned along a northeast-southwest trend for a distance of about , roughly subparallel to structural discontinuities called the Great Slave Lake Shear Zone to the north and the

text: Snowbird Tectonic Zone

text: to the south. They lie above or marginal to a 2.0 to 2.4 billion year old

text: Precambrian

text: craton

text: called the

text: Buffalo Head Terrane

text: , which has no surface exposure. Near the fields the Precambrian rocks are overlain by about  to  of

text: Phanerozoic

text: sedimentary rock

text: s, and covered by unconsolidated

text: glacial

text: and post-glacial sediments.

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text: The design incorporated Britannia at the centre top with a shield and a reclining lion surrounded on either side by a representation of the continents of Asia and North America with people reading their mail in the two lower corners. Rowland Hill expected the lettersheets to be more popular than the postage stamps but the postage stamp prevailed. Many caricatures were produced by stationery manufacturers whose livelihood was threatened by the new lettersheet. Only six days after their introduction, on May 12, Hill wrote in his journal:Within two months a decision had been made to replace the Mulready designed stationery and essentially they were a folly.

text: The design incorporated

text: Britannia

text: at the centre top with a shield and a reclining lion surrounded on either side by a representation of the continents of Asia and North America with people reading their mail in the two lower corners. Rowland Hill expected the lettersheets to be more popular than the postage stamps but the postage stamp prevailed. Many

text: caricature

text: s were produced by stationery manufacturers whose livelihood was threatened by the new lettersheet. Only six days after their introduction, on May 12, Hill wrote in his journal:Within two months a decision had been made to replace the Mulready designed stationery and essentially they were a

text: folly

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text: Scotland is geologically alien to Europe, comprising a lost sliver of the ancient continent of Laurentia (which later formed the bulk of North America). During the Cambrian period the crustal region which became Scotland formed part of the continental shelf of Laurentia, then still south of the equator. Laurentia was separated from the continent of Baltica (which later became Scandinavia and the Baltic region) by the diminishing Iapetus Ocean. The two ancient continents moved toward one another through the Cambrian and Ordovician periods, with tectonic folding during the Silurian pushing the first Scottish land above water. The final collision occurred during the Devonian period, with the Scottish segment of the Laurentian plate smashing into Avalonia (which contained what is now most of England and Wales), a motile subcontinent which had previously joined with Baltica. This impact threw up a massive chain of mountains (at least as tall as the present-day Alps) and saw the formation of the granitic West Highland and Grampian mountain chains and (through the Carboniferous) a period of volcanic activity in central and eastern Scotland. During the Permian and Triassic periods, with the Iapetus Ocean entirely closed, Scotland lay near the centre of the Pangaean supercontinent. At the start of the Tertiary, a constructive plate boundary (at which tectonic plates move apart) became active between Laurentia and Eurasia, pushing the two apart (and parting Scotland from Laurentia). This recession opened the Atlantic Ocean for the first time, and the consequent subduction zone at the western plate margin led to a renewed period of volcanism, this time on Scotland's west coast, producing fresh mountains on Skye, Jura, Mull, Rùm, and Arran.

text: Scotland is geologically alien to Europe, comprising a lost sliver of the ancient continent of

text: Laurentia

text: (which later formed the bulk of

text: North America

text: ). During the

text: Cambrian

text: period the crustal region which became Scotland formed part of the continental shelf of Laurentia, then still south of the equator. Laurentia was separated from the continent of

text: Baltica

text: (which later became

text: Scandinavia

text: and the

text: Baltic region

text: ) by the diminishing

text: Iapetus Ocean

text: . The two ancient continents moved toward one another through the Cambrian and

text: Ordovician

text: periods, with

text: tectonic

text: folding during the

text: Silurian

text: pushing the first Scottish land above water. The final collision occurred during the

text: Devonian

text: period, with the Scottish segment of the Laurentian plate smashing into

text: Avalonia

text: (which contained what is now most of

text: England

text: and

text: Wales

text: ), a motile subcontinent which had previously joined with Baltica. This impact threw up a massive chain of mountains (at least as tall as the present-day

text: Alps

text: ) and saw the formation of the granitic

text: West Highland

text: and

text: Grampian

text: mountain chains and (through the

text: Carboniferous

text: ) a period of volcanic activity in central and eastern Scotland. During the

text: Permian

text: and

text: Triassic

text: periods, with the

text: Iapetus Ocean

text: entirely closed, Scotland lay near the centre of the

text: Pangaea

text: n supercontinent. At the start of the

text: Tertiary

text: , a constructive plate boundary (at which tectonic plates move apart) became active between Laurentia and Eurasia, pushing the two apart (and parting Scotland from Laurentia). This recession opened the

text: Atlantic Ocean

text: for the first time, and the consequent

text: subduction zone

text: at the western plate margin led to a renewed period of

text: volcanism

text: , this time on Scotland's west coast, producing fresh mountains on

text: Skye

text: Jura

text: Mull

text: Rùm

text: , and

text: Arran

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answers: 1: The answer has limited relevance and completeness, with significant gaps or inaccuracy.

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answers: the Cambrian period

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: The craton is named after the Laurentian Shield, which in turn is named after the Laurentian Mountains, which were named after the Saint Lawrence River which in turn was named after Lawrence of Rome.

text: The craton is named after the

text: Laurentian Shield

text: , which in turn is named after the

text: Laurentian Mountains

text: , which were named after the

text: Saint Lawrence River

text: which in turn was named after

text: Lawrence of Rome

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answers: Laurentian Mountains

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answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Lawrence of Rome

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Early sauropods and their prosauropod relatives were found around the world as all of the continents were at the time united into the single supercontinent, Pangaea, which made dispersal across the entire terrestrial world possible.

text: Early sauropods and their

text: prosauropod

text: relatives were found around the world as all of the continents were at the time united into the single supercontinent,

text: Pangaea

text: , which made

text: dispersal

text: across the entire terrestrial world possible.

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answers: supercontinent

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answers: Pangaea

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answers: Pangaea

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answers: Zircons indicate that there was water

answers: NDQ_005579

answers: Pangaea

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: A shield is generally a large area of exposed Precambrian crystalline igneous and high-grade metamorphic rocks that form tectonically stable areas. In all cases, the age of these rocks is greater than 570 million years and sometimes dates back 2 to 3.5 billion years. They have been little affected by tectonic events following the end of the Precambrian, and are relatively flat regions where mountain building, faulting, and other tectonic processes are greatly diminished compared with the activity that occurs at the margins of the shields and the boundaries between tectonic plates.

text: A shield is generally a large area of exposed

text: Precambrian

text: crystalline

text: igneous

text: and high-grade

text: metamorphic

text: rocks that form

text: tectonically

text: stable areas. In all cases, the age of these rocks is greater than 570 million years and sometimes dates back 2 to 3.5 billion years. They have been little affected by

text: tectonic

text: events following the end of the Precambrian, and are relatively flat regions where mountain building, faulting, and other tectonic processes are greatly diminished compared with the activity that occurs at the margins of the shields and the boundaries between

text: tectonic plate

text: s.

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answers: 4

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answers: 0

answers: NDQ_005577

answers: 0

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answers: 0

answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: crystalline igneous

answers: NDQ_005574

answers: tectonic plates

answers: NDQ_005575

answers: crystalline igneous and high-grade metamorphic rocks

answers: NDQ_005576

answers: shield

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In 1889 and 1909 Mantovani published a hypothesis of an expanding earth and continental drift. He assumed that a closed continent covered the entire surface of a smaller earth. Through volcanic activity because of thermal expansion this continent broke, so that the new continents were drifting away from each other because of further expansion of the rip-zones, where now the oceans lie.Alfred Wegener saw similarities to his own theory, but did not support Mantovani's earth-expansion hypothesis. He wrote:

text: In 1889 and 1909 Mantovani published a hypothesis of an

text: expanding earth

text: and

text: continental drift

text: . He assumed that a closed continent covered the entire surface of a smaller earth. Through

text: volcanic

text: activity because of

text: thermal expansion

text: this continent broke, so that the new continents were drifting away from each other because of further expansion of the rip-zones, where now the oceans lie.

text: Alfred Wegener

text: saw similarities to his own theory, but did not support Mantovani's earth-expansion hypothesis. He wrote:

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answers: magma

answers: NDQ_005572

answers: a closed continent

answers: NDQ_005573

answers: Earth was expanding

answers: NDQ_005574

answers: Earth's crust is made up of cratons.

answers: NDQ_005575

answers: Earth-expansion

answers: NDQ_005576

answers: Rip-zones

answers: NDQ_005577

answers: The presence of zircons in ancient rocks indicates that there was water in the environment.

answers: NDQ_005579

answers: mantovani's hypothesis

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There is no significant amount of mineral extraction in Equatorial Guinea. Artisanal gold mining occurs in rivers that come from the Precambrian rocks of the Rio Muni. Additional minerals mined are: diamonds, coltan, iron, bauxite, tin, and tungsten

text: There is no significant amount of mineral extraction in Equatorial Guinea. Artisanal gold mining occurs in rivers that come from the Precambrian rocks of the

text: Rio Muni

text: . Additional minerals mined are: diamonds, coltan, iron, bauxite, tin, and tungsten

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answers: Precambrian rocks

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answers: Precambrian rocks

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answers: Precambrian

answers: NDQ_005574

answers: Precambrian

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answers: rocks

answers: NDQ_005576

answers: rocks

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answers: rivers

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: It has been suggested that the Late Mesoproterozoic–Early Neoproterozoic aged Sveconorwegian Orogen in Fennoscandia could have been caused by a  continent–continent collision between the Amazonia and Baltica. The question is open if Telemarkia terrane in Norway was derived from the Amazonian Craton but this possibility does not imply necessarily that there was a continental collision.

text: It has been suggested that the

text: Late Mesoproterozoic

text: Early Neoproterozoic

text: aged

text: Sveconorwegian Orogen

text: in

text: Fennoscandia

text: could have been caused by a

text: continent–continent collision

text: between the Amazonia and

text: Baltica

text: . The question is open if Telemarkia

text: terrane

text: in

text: Norway

text: was derived from the Amazonian Craton but this possibility does not imply necessarily that there was a continental collision.

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answers: Amazonia

answers: NDQ_005572

answers: Amazonia

answers: NDQ_005573

answers: continent–continent collision

answers: NDQ_005574

answers: Amazonian Craton

answers: NDQ_005575

answers: Sveconorwegian Orogen

answers: NDQ_005576

answers: continent–continent collision

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Late Mesoproterozoic–Early Neoproterozoic

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: The Flin Flon domain is in the center of the Trans-Hudson Suture Zone and extends over the border of the Manitoba-Saskatchewan segment east and west.  It is west of the Superior Craton, south of the Kisseynew Domain, and east of the Glennie Domain.

text: The Flin Flon domain is in the center of the Trans-Hudson Suture Zone and extends over the border of the Manitoba-Saskatchewan segment east and west.  It is west of the Superior Craton, south of the Kisseynew Domain, and east of the Glennie Domain.

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answers: NDQ_005571

answers: Superior Craton

answers: NDQ_005572

answers: Trans-Hudson Suture Zone

answers: NDQ_005573

answers: Trans-Hudson Suture Zone

answers: NDQ_005574

answers: Superior Craton

answers: NDQ_005575

answers: Trans-Hudson Suture Zone

answers: NDQ_005576

answers: Trans-Hudson Suture Zone

answers: NDQ_005577

answers: Trans-Hudson Suture Zone

answers: NDQ_005579

answers: Trans-Hudson Suture Zone

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: After Rodinia broke apart, its southern half traveled south and crossed the South Pole while its northern half traveled northward to the North Pole. The two halves of Rodinia eventually collided with the Congo craton to form the supercontinent Pannotia 600 million years ago. In contrast to Rodinia, Pannotia was short-lived. It rifted apart 545 million years ago, or only 65 million years after it formed. This resulted in the creation of at least four continents, namely Baltica, Siberia, Gondwana and Laurentia. By the Early Cambrian 514 million years ago, Laurenta was located on the equator, Baltica was south of Laurenta, Siberia was just south of the equator east of Laurenta, and Gondwana lied mostly in the Southern Hemisphere. Subsequently, Baltica, Laurenta and microcontinent Avalonia collided in the Devonian period (416-359 million years ago) to form minor supercontinent Euramerica. This eventually started to collide with Gondwana and other landmasses to form supercontinent Pangaea 255 million years ago. In the Late Triassic period some 152 million years ago, Pangaea split into two minor supercontinents, namely Gondwana and Laurasia. The Temagami Greenstone Belt represented a minor portion of western Laurasia until it divided into Eurasia and North America about 94 million years ago. Since the Middle Miocene 14 million years ago, the Temagami Greenstone Belt has been part of the Americas, a minor north-south trending supercontinent comprising the continents of North America and South America.

text: After Rodinia broke apart, its southern half traveled south and crossed the

text: South Pole

text: while its northern half traveled northward to the

text: North Pole

text: . The two halves of Rodinia eventually collided with the

text: Congo craton

text: to form the supercontinent

text: Pannotia

text: 600 million years ago. In contrast to Rodinia, Pannotia was short-lived. It rifted apart 545 million years ago, or only 65 million years after it formed. This resulted in the creation of at least four continents, namely Baltica,

text: Siberia

text: Gondwana

text: and Laurentia. By the

text: Early Cambrian

text: 514 million years ago, Laurenta was located on the

text: equator

text: , Baltica was south of Laurenta, Siberia was just south of the equator east of Laurenta, and Gondwana lied mostly in the

text: Southern Hemisphere

text: . Subsequently, Baltica, Laurenta and microcontinent

text: Avalonia

text: collided in the

text: Devonian

text: period (416-359 million years ago) to form minor supercontinent

text: Euramerica

text: . This eventually started to collide with Gondwana and other landmasses to form supercontinent

text: Pangaea

text: 255 million years ago. In the

text: Late Triassic

text: period some 152 million years ago, Pangaea split into two minor supercontinents, namely Gondwana and

text: Laurasia

text: . The Temagami Greenstone Belt represented a minor portion of western Laurasia until it divided into Eurasia and North America about 94 million years ago. Since the

text: Middle Miocene

text: 14 million years ago, the Temagami Greenstone Belt has been part of the

text: Americas

text: , a minor north-south trending supercontinent comprising the continents of North America and

text: South America

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text: Convective inhibition (CIN or CINH)<ref name="colby1984">{{cite journal| author=Colby, Jr., Frank P.| title=Convective Inhibition as a Predictor of Convection during AVE-SESAME II| journal=Mon. Wea. Rev.| year=1984| volume=112| issue=11| pages=2239–2252| doi=10.1175/1520-0493(1984)112

text: Convective inhibition (CIN or CINH)<ref name="colby1984">{{cite journal| author=Colby, Jr., Frank P.| title=Convective Inhibition as a Predictor of Convection during AVE-SESAME II| journal=Mon. Wea. Rev.| year=1984| volume=112| issue=11| pages=2239–2252| doi=10.1175/1520-0493(1984)112

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answers: AVE-SESAME II

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answers: Convective Inhibition as a Predictor of Convection

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answers: Convective Inhibition as a Predictor of Convection

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answers: Convective Inhibition as a Predictor of Convection during AVE-SESAME II was published in Mon. Wea. Rev. in 1984.

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answers: The presence of zircons in ancient rocks indicates that there was water in the environment.

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text: Major changes came to the conference in 1992. First, Akron left for the Mid-American Conference (MAC) and was replaced by another Ohio school, Youngstown State University. More significantly, the Mid-Continent added women's sports by absorbing the North Star Conference (NSC), a women's-only league whose final seven members had all been in the Mid-Continent. All of the final NSC members except for Akron moved their women's sports into the Mid-Continent. At the same time, Eastern Illinois and Western Illinois moved their women's sports into the Mid-Continent when their former women's sports home, the Gateway Conference, merged into the Missouri Valley Conference. A year later, the University of Wisconsin–Milwaukee joined the Mid-Continent.

text: Major changes came to the conference in 1992. First, Akron left for the

text: Mid-American Conference

text: (MAC) and was replaced by another Ohio school,

text: Youngstown State University

text: . More significantly, the Mid-Continent added women's sports by absorbing the

text: North Star Conference

text: (NSC), a women's-only league whose final seven members had all been in the Mid-Continent. All of the final NSC members except for Akron moved their women's sports into the Mid-Continent. At the same time, Eastern Illinois and Western Illinois moved their women's sports into the Mid-Continent when their former women's sports home, the

text: Gateway Conference

text: , merged into the

text: Missouri Valley Conference

text: . A year later, the

text: University of Wisconsin–Milwaukee

text: joined the Mid-Continent.

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text: Emblems that resemble heraldic shields are also called shields. Movie studio Warner Bros. uses a shield emblazoned with WB as its logo. The Looney Tunes cartoons, released through Warner Bros., open with the WB shield zooming through concentric circles. Also, the Superman logo uses a shield emblazoned with the letter S.

text: Emblems that resemble heraldic shields are also called shields. Movie studio

text: Warner Bros.

text: uses a shield emblazoned with WB as its logo. The

text: Looney Tunes

text: cartoons

text: , released through Warner Bros., open with the WB shield zooming through concentric

text: circle

text: s. Also, the

text: Superman logo

text: uses a shield emblazoned with the letter S.

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answers: when Earth's interior was warmer than it is now

answer: No

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text: reported that a weak tropical disturbance had developed, along a slow moving trough of low pressure about  to the southwest of Rotuma. Over the next couple of days the system drifted towards the southeast and Fiji, in an area of strong westerly wind shear to the south of a ridge axis. Early on April 3, RSMC Nadi initiated advisories on the system and designated it as Tropical Depression 14F, while it was located about  to the north of Labasa, on Vanua Levu. During that day the system slightly accelerated, as it moved towards the south-southeast. Later that day RSMC Nadi reported that the systems low level circulation, was exposed to the northwest of the deep convection which was moving over northeastern Vanua Levu, Cikobia and other smaller islands. The westerly wind shear around the system subsequently relaxed sufficiently, which allowed the depression to consolidate and the low level circulation center to move closer to the area of deep convection.

text: reported that a weak tropical disturbance had developed, along a slow moving trough of low pressure about  to the southwest of

text: Rotuma

text: . Over the next couple of days the system drifted towards the southeast and

text: Fiji

text: , in an area of strong westerly wind shear to the south of a ridge axis. Early on April 3, RSMC Nadi initiated advisories on the system and designated it as Tropical Depression 14F, while it was located about  to the north of

text: Labasa

text: , on

text: Vanua Levu

text: . During that day the system slightly accelerated, as it moved towards the south-southeast. Later that day RSMC Nadi reported that the systems low level circulation, was exposed to the northwest of the deep convection which was moving over northeastern

text: Vanua Levu

text: Cikobia

text: and other smaller islands. The westerly wind shear around the system subsequently relaxed sufficiently, which allowed the depression to consolidate and the low level circulation center to move closer to the area of deep convection.

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answers: igneous

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answers: deep convection

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answers: Rotuma

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answers: to the southwest of Rotuma

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answers: Tropical Depression

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answers: Tropical Depression 14F

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answers: tropical

answer: No

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answer: No

answer: 1

text: South China continent, also known as South China Craton, South Chinese Craton, or Yangtze Craton, was an ancient continent (craton) that contained today's South and Southeast China (named after), Indochina, and parts of Southeast Asia (i.e. Borneo and adjacent islands). South China had been part of many past supercontinents, including Rodinia, Pannotia, Gondwana, Pangaea, Laurasia, and Eurasia.

text: South China continent, also known as South China Craton, South Chinese Craton, or Yangtze Craton, was an ancient

text: continent

text: craton

text: ) that contained today's

text: South

text: and

text: Southeast China

text: (named after),

text: Indochina

text: , and parts of

text: Southeast Asia

text: (i.e.

text: Borneo

text: and adjacent islands). South China had been part of many past supercontinents, including

text: Rodinia

text: Pannotia

text: Gondwana

text: Pangaea

text: Laurasia

text: , and

text: Eurasia

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answers: NDQ_005571

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answers: 5

answers: NDQ_005575

answers: 0

answers: NDQ_005576

answers: 0

answers: NDQ_005577

answers: 0

answers: NDQ_005579

answers: 0

answers: NDQ_005571

answers: craton

answers: NDQ_005572

answers: South China

answers: NDQ_005573

answers: supercontinents

answers: NDQ_005574

answers: South China continent

answers: NDQ_005575

answers: South China

answers: NDQ_005576

answers: Craton

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: ancient

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: The Midcontinent Rift System (MRS) or Keweenawan Rift is a  long geological rift in the center of the North American continent and south-central part of the North American plate.  It formed when the continent's core, the North American craton, began to split apart during the Mesoproterozoic era of the Precambrian, about 1.1 billion years ago.  The rift failed, leaving behind thick layers of rock that are exposed in its northern reaches, but buried beneath later sedimentary formations along most of its western and eastern arms. Those arms meet at Lake Superior, which is contained within the rift valley.  The lake's north shore in Ontario and Minnesota defines the northern arc of the rift.  From the lake, the rift's eastern arm trends south to central lower Michigan.  The western arm runs from Lake Superior southwest through portions of Wisconsin, Minnesota, Iowa, and Nebraska to northeastern Kansas.

text: The Midcontinent Rift System (MRS) or Keweenawan Rift is a  long geological

text: rift

text: in the center of the

text: North American continent

text: and south-central part of the

text: North American plate

text: .  It formed when the continent's core, the

text: North American craton

text: , began to split apart during the

text: Mesoproterozoic

text: era of the

text: Precambrian

text: , about 1.1 billion years ago.  The rift failed, leaving behind thick layers of rock that are exposed in its northern reaches, but buried beneath later sedimentary formations along most of its western and eastern arms. Those arms meet at

text: Lake Superior

text: , which is contained within the

text: rift valley

text: .  The lake's

text: north shore

text: in

text: Ontario

text: and

text: Minnesota

text: defines the northern arc of the rift.  From the lake, the rift's eastern arm trends south to central lower

text: Michigan

text: .  The western arm runs from Lake Superior southwest through portions of

text: Wisconsin

text: Minnesota

text: Iowa

text: , and

text: Nebraska

text: to northeastern

text: Kansas

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answers: craton

answers: NDQ_005572

answers: the North American craton

answers: NDQ_005573

answers: 1.1 billion years ago

answers: NDQ_005574

answers: North American

answers: NDQ_005575

answers: 1.1 billion years ago

answers: NDQ_005576

answers: rift valley

answers: NDQ_005577

answers: Lake Superior

answers: NDQ_005579

answers: the Precambrian

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: The Copperhill Formation is part of the greater Ocoee Supergroup, a body of clastic metasedimentary rocks formed 560 million years ago. They unconformably lie upon Precambrian granitic and gneissic rocks. The sediments that originally comprised the Ocoee Supergroup accumulated in a string of narrow, deep-water basins that stretched along the entire southern-central Appalachian margin from Tennessee, North Carolina, to Georgia. These basins were rift basins formed by the rifting of Rodinia.

text: The Copperhill Formation is part of the greater Ocoee Supergroup, a body of

text: clastic

text: metasedimentary

text: rocks formed 560 million years ago. They

text: unconformably

text: lie upon

text: Precambrian

text: granitic

text: and

text: gneiss

text: ic rocks. The sediments that originally comprised the Ocoee Supergroup accumulated in a string of narrow, deep-water basins that stretched along the entire southern-central Appalachian margin from Tennessee, North Carolina, to Georgia. These basins were

text: rift

text: basins formed by the rifting of

text: Rodinia

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answers: Precambrian

answer: Yes

answer: Yes

answer: No

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text: A craton is an ancient part of the Earth's continental crust which has been more or less stable since Precambrian times. Cratons whose ancient rocks are widely exposed at the surface, often with relatively subdued relief, are known as shields. If the ancient rocks are largely overlain by a cover of younger rocks then the 'hidden' craton may be referred to as a platform.

text: A

text: craton

text: is an ancient part of the Earth's continental crust which has been more or less stable since

text: Precambrian

text: times. Cratons whose ancient rocks are widely exposed at the surface, often with relatively subdued relief, are known as

text: shields

text: . If the ancient rocks are largely overlain by a cover of younger rocks then the 'hidden' craton may be referred to as a

text: platform

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answers: cratons

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian times

answers: NDQ_005574

answers: ancient part of the Earth's continental crust

answers: NDQ_005575

answers: Precambrian times

answers: NDQ_005576

answers: platform

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Precambrian times

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: Often presenting an exposed low-level circulation center (LLCC), the tropical depression drifted westward without further development for days owing to a marginal environment within the subsident region of a tropical upper tropospheric trough (TUTT) cell to the northwest, with moderate vertical wind shear. Late on October 7, the Joint Typhoon Warning Center (JTWC) eventually issued a Tropical Cyclone Formation Alert for the system, when the TUTT cell was beginning to move to the west-southwest, allowing convection to develop over the consolidating LLCC.

text: Often presenting an exposed low-level circulation center (LLCC), the tropical depression drifted westward without further development for days owing to a marginal environment within the subsident region of a

text: tropical upper tropospheric trough

text: (TUTT) cell to the northwest, with moderate vertical

text: wind shear

text: . Late on October 7, the

text: Joint Typhoon Warning Center

text: (JTWC) eventually issued a

text: Tropical Cyclone Formation Alert

text: for the system, when the TUTT cell was beginning to move to the west-southwest, allowing

text: convection

text: to develop over the consolidating LLCC.

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answers: Cyclone Formation

answers: NDQ_005572

answers: TUTT

answers: NDQ_005573

answers: greenstones in cratons

answers: NDQ_005574

answers: TUTT cell

answers: NDQ_005575

answers: moderate vertical wind shear

answers: NDQ_005576

answers: TUTT

answers: NDQ_005577

answers: Tropical Cyclone Formation

answers: NDQ_005579

answers: tropical

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The early Precambrian (from 800 to 650 Ma) is a compressional phase where a series of islands-arcs and micro-continent terrane accreted to form the oldest portions of the Arabian Plate (Gondwana). The development of Hormuz saltbasin was a consequence of the last Precambrian orogenic event.

text: The early

text: Precambrian

text: (from 800 to 650 Ma) is a compressional phase where a series of islands-arcs and micro-continent terrane accreted to form the oldest portions of the Arabian Plate (

text: Gondwana

text: ). The development of Hormuz saltbasin was a consequence of the last Precambrian orogenic event.

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answers: NDQ_005571

answers: Arabian Plate

answers: NDQ_005572

answers: the early Precambrian

answers: NDQ_005573

answers: accreted

answers: NDQ_005574

answers: arcs

answers: NDQ_005575

answers: a compressional phase

answers: NDQ_005576

answers: precambrian

answers: NDQ_005577

answers: saltbasin

answers: NDQ_005579

answers: The early Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: is the Sherwood number due only to natural convection and not forced convection.

text: is the Sherwood number due only to natural convection and not forced convection.

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answers: 2: The answer has limited relevance and completeness, with significant gaps or inaccuracy.

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answers: igneous

answers: NDQ_005572

answers: Sherwood number

answers: NDQ_005573

answers: natural convection

answers: NDQ_005574

answers: Sherwood number

answers: NDQ_005575

answers: natural convection

answers: NDQ_005576

answers: natural convection

answers: NDQ_005577

answers: natural convection

answers: NDQ_005579

answers: forced convection

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In the 60s and 70s a simple creationist model proposed that, "The Flood split the land mass into the present continents." Steve Austin and other creationists proposed a preliminary model of catastrophic plate tectonics (CPT) in 1994. Their work built on earlier papers by John Baumgardner and Russell Humphreys in 1986. Baumgardner proposed a model of mantel convection that allows for runaway subduction and Humphrey associated mantle convection with rapid magnetic reversals in earth history. Baumgardner's proposal holds that the rapid plunge of former oceanic plates into the mantle (caused by an unknown trigger-mechanism) increased local mantle pressures to the point that its viscosity dropped several magnitudes according to known properties of mantle silicates.  Once initiated, sinking plates caused the spread of low viscosity throughout the mantle resulting in runaway mantle-convection and catastrophic tectonic motion which dragged continents across the surface of the earth. Once the former ocean plates, which are thought to be denser than the mantle, reached the bottom of the mantle an equilibrium resulted.  Pressures dropped, viscosity increased, runaway mantle-convection stopped, leaving the surface of the earth rearranged.  Proponents point to subducted slabs in the mantle which are still relatively cool, which they regard as evidence that they have not been there for millions of years which would result in temperature equilibration.

text: In the 60s and 70s a simple creationist model proposed that, "The Flood split the land mass into the present continents." Steve Austin and other creationists proposed a preliminary model of catastrophic plate tectonics (CPT) in 1994. Their work built on earlier papers by

text: John Baumgardner

text: and

text: Russell Humphreys

text: in 1986. Baumgardner proposed a model of mantel convection that allows for runaway subduction and Humphrey associated mantle convection with rapid magnetic reversals in earth history. Baumgardner's proposal holds that the rapid plunge of former oceanic plates into the

text: mantle

text: (caused by an unknown trigger-mechanism) increased local mantle pressures to the point that its viscosity dropped several magnitudes according to known properties of mantle silicates.  Once initiated, sinking plates caused the spread of low viscosity throughout the mantle resulting in runaway mantle-convection and catastrophic

text: tectonic

text: motion which dragged continents across the surface of the earth. Once the former ocean plates, which are thought to be denser than the mantle, reached the bottom of the mantle an equilibrium resulted.  Pressures dropped, viscosity increased, runaway mantle-convection stopped, leaving the surface of the earth rearranged.  Proponents point to subducted slabs in the mantle which are still relatively cool, which they regard as evidence that they have not been there for millions of years which would result in temperature equilibration.

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Eratosthenes, in the 3rd century BC, noted that some geographers divided the continents by rivers (the Nile and the Don), thus considering them "islands". Others divided the continents by isthmuses, calling the continents "peninsulas". These latter geographers set the border between Europe and Asia at the isthmus between the Black Sea and the Caspian Sea, and the border between Asia and Africa at the isthmus between the Red Sea and the mouth of Lake Bardawil on the Mediterranean Sea.

text: Eratosthenes

text: , in the 3rd century BC, noted that some geographers divided the continents by rivers (the Nile and the Don), thus considering them "islands". Others divided the continents by

text: isthmus

text: es, calling the continents "peninsulas". These latter geographers set the border between Europe and Asia at the isthmus between the Black Sea and the

text: Caspian Sea

text: , and the border between Asia and Africa at the isthmus between the

text: Red Sea

text: and the mouth of

text: Lake Bardawil

text: on the

text: Mediterranean Sea

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answers: arethmuses

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answers: isthmus

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answers: Black Sea and the Caspian Sea

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answers: the 3rd century BC

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The mine is within the Saddleback Greenstone Belt, an Archaean structure in the southwestern Yilgarn Craton.

text: The mine is within the Saddleback

text: Greenstone Belt

text: , an

text: Archaean

text: structure in the southwestern

text: Yilgarn Craton

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answers: Archaean

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answers: Archaean

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answers: NDQ_005577

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answers: Archaean

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Curiously, there is another widespread pattern of parallel fault zones, etc., of various ages trending roughly NE-SW, including the Midcontinent Rift System, the Reelfoot Rift (in the New Madrid Seismic Zone), and others. These fault zones and rifts occur on tectonic boundaries that date to the Proterozoic – that is, 1.8 to 1.6 billions of years old. They are also roughly parallel to the Ouachita— Appalachian mountains, raised when Laurentia merged with the other continents to form the Pangaea supercontinent some 350 million years ago.  It is now believed that these two predominant patterns reflect ancient weaknesses in the underlying Precambrian basement rock, which can be reactivated to control the orientation of features formed much later.

text: Curiously, there is another widespread pattern of parallel fault zones, etc., of various ages trending roughly NE-SW, including the

text: Midcontinent Rift System

text: , the

text: Reelfoot Rift

text: (in the

text: New Madrid Seismic Zone

text: ), and others. These fault zones and rifts occur on tectonic boundaries that date to the

text: Proterozoic

text: – that is, 1.8 to 1.6 billions of years old. They are also roughly parallel to the

text: Ouachita

text: Appalachian mountains

text: , raised when

text: Laurentia

text: merged with the other continents to form the

text: Pangaea

text: supercontinent some 350 million years ago.  It is now believed that these two predominant patterns reflect ancient weaknesses in the underlying

text: Precambrian

text: basement

text: rock, which can be reactivated to control the orientation of features formed much later.

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answers: Precambrian

answers: NDQ_005572

answers: Laurentia

answers: NDQ_005573

answers: Precambrian basement rock

answers: NDQ_005574

answers: Laurentia

answers: NDQ_005575

answers: 350 million years ago

answers: NDQ_005576

answers: rift

answers: NDQ_005577

answers: ancient weaknesses in the underlying Precambrian basement rock

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Moist convection releases latent heat and is important to the Earth's energy budget. Convection occurs on too small a scale to be resolved by climate models, and hence it must be handled via parameters. This has been done since the 1950s. Akio Arakawa did much of the early work, and variants of his scheme are still used, although a variety of different schemes are now in use. Clouds are also typically handled with a parameter, for a similar lack of scale. Limited understanding of clouds has limited the success of this strategy, but not due to some inherent shortcoming of the method.

text: Moist convection releases latent heat and is important to the Earth's energy budget. Convection occurs on too small a scale to be resolved by climate models, and hence it must be handled via parameters. This has been done since the 1950s. Akio Arakawa did much of the early work, and variants of his scheme are still used, although a variety of different schemes are now in use. Clouds are also typically handled with a parameter, for a similar lack of scale. Limited understanding of clouds has limited the success of this strategy, but not due to some inherent shortcoming of the method.

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answers: Earth's

answers: NDQ_005572

answers: Earth's energy budget

answers: NDQ_005573

answers: Moist

answers: NDQ_005574

answers: Moist convection releases latent heat

answers: NDQ_005575

answers: Moist convection releases latent heat

answers: NDQ_005576

answers: Moist convection

answers: NDQ_005577

answers: Moist

answers: NDQ_005579

answers: the 1950s

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Shropshire has a huge range of different types of rocks, stretching from the Precambrian until the Holocene. In the northern part of the county there are examples of Jurassic, Carboniferous, Permian and Triassic. Centrally, Precambrian, Cambrian, Ordovician, Carboniferous and Permian predominate. And in the south it is predominantly Silurian and Quaternary. Shropshire has a number of areas with Silurian and Ordivician rocks, where a number of shells, corals and trilobites can be found. Mortimer Forest and Wenlock Edge are examples where a number of fossils can be found.

text: Shropshire has a huge range of different types of rocks, stretching from the

text: Precambrian

text: until the

text: Holocene

text: . In the northern part of the county there are examples of

text: Jurassic

text: Carboniferous

text: Permian

text: and

text: Triassic

text: . Centrally, Precambrian,

text: Cambrian

text: Ordovician

text: , Carboniferous and Permian predominate. And in the south it is predominantly

text: Silurian

text: and

text: Quaternary

text: . Shropshire has a number of areas with Silurian and Ordivician rocks, where a number of

text: shells

text: coral

text: s and

text: trilobite

text: s can be found. Mortimer Forest and Wenlock Edge are examples where a number of

text: fossil

text: s can be found.

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answers: the Precambrian

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Wassa Gold Mine is located in the southwestern region of Ghana, approximately 35km northeast of the town of Tarkwa. It lies in the Birimian Province of the West African Precambrian shield, within the southern portion of the Ashanti Greenstone Belt. Ore is sourced from the single large Wassa Main Pit (open pit mine) and Wassa Underground (underground mine).

text: The Wassa Gold Mine is located in the southwestern region of Ghana, approximately 35km northeast of the town of Tarkwa. It lies in the Birimian Province of the West African Precambrian shield, within the southern portion of the Ashanti Greenstone Belt. Ore is sourced from the single large Wassa Main Pit (open pit mine) and Wassa Underground (underground mine).

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answers: Precambrian

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answers: Ashanti Greenstone Belt

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answers: Ashanti Greenstone Belt

answers: NDQ_005574

answers: Ashanti Greenstone Belt

answers: NDQ_005575

answers: West African

answers: NDQ_005576

answers: Ashanti Greenstone Belt

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Shields vary size and in the number of embossed rings, but the size of the embossed features is consistent. The largest shield (found at Ayrshire) has twenty nine circular ridges and twenty nine rings of bosses; the smallest (originally thought to have been from County Antrim but actually from The River Thames) has eleven ridges and rings.

text: Shields vary size and in the number of embossed rings, but the size of the embossed features is consistent. The largest shield (found at

text: Ayrshire

text: ) has twenty nine circular ridges and twenty nine rings of bosses; the smallest (originally thought to have been from

text: County Antrim

text: but actually from The River Thames) has eleven ridges and rings.

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answers: NDQ_005571

answers: Ayrshire

answers: NDQ_005572

answers: Ayrshire

answers: NDQ_005573

answers: embossed features

answers: NDQ_005574

answers: The River Thames

answers: NDQ_005575

answers: ridges and rings

answers: NDQ_005576

answers: shield

answers: NDQ_005577

answers: The River Thames

answers: NDQ_005579

answers: ancient

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: In 1963 Cornelius Shields, one of the foremost proponents of one-design sailing in the U.S. conceived of a modern followup to the International One Design (IOD). The new boat would have the balance and beauty of the IOD while incorporating modern trends such as fiberglass construction. Shields commissioned Olin Stephens for the design. Over 250 have been built and many are actively raced in fleets around the U.S. Shields are sloop-rigged and usually sailed by a crew of three to five. No hiking straps are allowed, keeping athletic demands on the crew to a minimum. (Shields class web site.)

text: In 1963 Cornelius Shields, one of the foremost proponents of

text: one-design

text: sailing in the U.S. conceived of a modern followup to the

text: International One Design

text: (IOD). The new boat would have the balance and beauty of the IOD while incorporating modern trends such as fiberglass construction. Shields commissioned

text: Olin Stephens

text: for the design. Over 250 have been built and many are actively raced in fleets around the U.S. Shields are

text: sloop-rigged

text: and usually sailed by a crew of three to five. No

text: hiking straps

text: are allowed, keeping athletic demands on the crew to a minimum. (Shields class web site.)

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answers: NDQ_005571

answers: fiberglass

answers: NDQ_005572

answers: U.S

answers: NDQ_005573

answers: greenstones in cratons

answers: NDQ_005574

answers: No hiking straps are allowed

answers: NDQ_005575

answers: one-design sailing

answers: NDQ_005576

answers: sloop

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: during the last ice age

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: The Alpine orogeny is considered one of the three major phases of orogeny in Europe that define the geology of that continent, along with the Caledonian orogeny that formed the Old Red Sandstone Continent when the continents Baltica and Laurentia collided in the early Paleozoic, and the Hercynian or Variscan orogeny that formed Pangaea when Gondwana and the Old Red Sandstone Continent collided in the middle to late Paleozoic.

text: The Alpine orogeny is considered one of the three major phases of orogeny in Europe that define the geology of that continent, along with the

text: Caledonian orogeny

text: that formed the

text: Old Red Sandstone Continent

text: when the continents

text: Baltica

text: and

text: Laurentia

text: collided

text: in the early

text: Paleozoic

text: , and the

text: Hercynian or Variscan orogeny

text: that formed

text: Pangaea

text: when

text: Gondwana

text: and the Old Red Sandstone Continent collided in the middle to late Paleozoic.

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answers: 0

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answers: 0

answers: NDQ_005571

answers: Paleozoic

answers: NDQ_005572

answers: Caledonian orogeny

answers: NDQ_005573

answers: Paleozoic

answers: NDQ_005574

answers: Alpine orogeny

answers: NDQ_005575

answers: Paleozoic

answers: NDQ_005576

answers: orogeny

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: early Paleozoic

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Kirkland Lake is located in the resource-rich Precambrian Shield, an ancient geological core of the North American continent. Nearby is the Arctic Watershed, a drainage divide at an elevation of .  Rivers south of that elevation flow into a drainage basin which includes Lake Ontario and the Saint Lawrence River, while rivers north of the watershed flow into Hudson Bay.

text: Kirkland Lake is located in the resource-rich

text: Precambrian Shield

text: , an ancient geological core of the North American continent. Nearby is the Arctic Watershed, a

text: drainage divide

text: at an elevation of .  Rivers south of that elevation flow into a

text: drainage basin

text: which includes

text: Lake Ontario

text: and the

text: Saint Lawrence River

text: , while rivers north of the watershed flow into

text: Hudson Bay

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answers: Precambrian Shield

answers: NDQ_005572

answers: Precambrian Shield

answers: NDQ_005573

answers: ancient

answers: NDQ_005574

answers: Arctic

answers: NDQ_005575

answers: ancient geological core

answers: NDQ_005576

answers: Shield

answers: NDQ_005577

answers: Kirkland Lake

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: The North American craton is the bedrock forming the heart of the North American continent and the Canadian Shield is the largest exposed part of the craton's bedrock.

text: The

text: North American craton

text: is the bedrock forming the heart of the North American continent and the Canadian Shield is the largest exposed part of the craton's bedrock.

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answers: North American craton

answers: NDQ_005572

answers: North American craton

answers: NDQ_005573

answers: greenstones in cratons indicate that at the time they formed

answers: NDQ_005574

answers: North American craton

answers: NDQ_005575

answers: North American craton

answers: NDQ_005576

answers: Canadian Shield

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: the Canadian Shield

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The seventh root race will arise from the seventh subrace of the sixth root race on the future continent that the sixth root race will be living on that will arise from the Pacific Ocean. The continent they will inhabit is esoterically called Pushkara.

text: The seventh root race will arise from the seventh subrace of the sixth root race on the future continent that the sixth root race will be living on that will arise from the Pacific Ocean. The continent they will inhabit is esoterically called

text: Pushkara

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answers: NDQ_005571

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answers: 0

answers: NDQ_005575

answers: 0

answers: NDQ_005576

answers: 0

answers: NDQ_005577

answers: 0

answers: NDQ_005579

answers: 0

answers: NDQ_005571

answers: Pacific Ocean

answers: NDQ_005572

answers: Pacific Ocean

answers: NDQ_005573

answers: Pacific Ocean

answers: NDQ_005574

answers: Pacific Ocean

answers: NDQ_005575

answers: Pacific Ocean

answers: NDQ_005576

answers: Pacific Ocean

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Pushkara

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Confederation of African Tennis (CAT) () is the continental governing body of tennis in Africa. It is the non-profit private organization based in Tunis and affiliated with International Tennis Federation. The main aim of the CAT is to regulate the rules of tennis in the African continent, to develop the fundamental infrastructures for the sport, and to popularize it throughout the continent. For this, CAT also recognizes the excellence of professionals in the field of tennis, including players and member associations with awards and accolades. It is the largest regional body of the tennis with 50 member countries. English and French are the official languages of the organization. According to CAT, African continent is divided into five different zones on the geographical basis with each zone has its own zonal head.

text: Confederation of African Tennis (CAT) () is the continental

text: governing body

text: of

text: tennis

text: in

text: Africa

text: . It is the non-profit private organization based in

text: Tunis

text: and affiliated with

text: International Tennis Federation

text: . The main aim of the CAT is to regulate the rules of tennis in the African continent, to develop the fundamental infrastructures for the sport, and to popularize it throughout the continent. For this, CAT also recognizes the excellence of professionals in the field of tennis, including players and member associations with awards and accolades. It is the largest regional body of the tennis with 50 member countries.

text: English

text: and

text: French

text: are the official languages of the organization. According to CAT, African continent is divided into five different zones on the geographical basis with each zone has its own zonal head.

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text: passes early on June 3 revealed sustained winds just above the tropical storm threshold, and the depression was subsequently upgraded to Tropical Storm Boris. Despite initial forecasts of several days over water, the center of circulation moved quickly northward in response to an upper-level low west of the system, and the bulk of Boris's deep convection moved ashore near Chiapas, Mexico around 0600 UTC on June 4. However, the cyclone's northward motion slowed, and the low-level circulation remained offshore, failing to ever make landfall. Thereafter, the system degenerated into a trough of low pressure about 80 mi (130 km) east-northeast of Salina Cruz, Mexico.

text: passes early on June 3 revealed sustained winds just above the tropical storm threshold, and the depression was subsequently upgraded to Tropical Storm Boris. Despite initial forecasts of several days over water, the center of circulation moved quickly northward in response to an upper-level low west of the system, and the bulk of Boris's deep convection moved ashore near

text: Chiapas, Mexico

text: around 0600 UTC on June 4. However, the cyclone's northward motion slowed, and the low-level circulation remained offshore, failing to ever make landfall. Thereafter, the system degenerated into a

text: trough

text: of low pressure about 80 mi (130 km) east-northeast of

text: Salina Cruz, Mexico

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text: The geological time period surrounding the breakup of Kenorland is thought by many geologists to be the beginning of the transition point from the deep-mantle-plume method of continent formation in the Hadean to Early Archean (before the final formation of the Earth's inner core) to the subsequent two-layer core-mantle plate tectonics convection theory. However, the findings of an earlier continent, Ur, and a  supercontinent of around 3.1 Ga, Vaalbara, indicate this transition period may have occurred much earlier.

text: The geological time period surrounding the breakup of Kenorland is thought by many geologists to be the beginning of the transition point from the deep-mantle-plume method of continent formation in the

text: Hadean

text: to Early

text: Archean

text: (before the final formation of the Earth's inner

text: core

text: ) to the subsequent two-layer core-

text: mantle

text: plate tectonics

text: convection theory. However, the findings of an earlier continent,

text: Ur

text: , and a

text: supercontinent

text: of around 3.1 Ga,

text: Vaalbara

text: , indicate this transition period may have occurred much earlier.

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answers: 3.1 Ga

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answers: two-layer

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answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Early Archean

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The period is characterised by expansion of existing platform covers, or by new platforms on recently cratonized basements.

text: The period is characterised by expansion of existing

text: platform cover

text: s, or by new

text: platform

text: s on recently

text: craton

text: ized basements.

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answers: basements

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answers: basements

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answers: recently cratonized

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answers: cratonized

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answers: expansion of existing platform covers

answers: NDQ_005576

answers: platform

answers: NDQ_005577

answers: Zircons indicate that there was water

answers: NDQ_005579

answers: cratonized

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There were no large continents in the early Archean, and small protocontinents were probably the norm in the Mesoarchean because they were prevented from coalescing into larger units by the high rate of geologic activity. These felsic protocontinents (cratons) probably formed at hot spots from a variety of sources: mafic magma melting more felsic rocks, partial melting of mafic rock, and from the metamorphic alteration of felsic sedimentary rocks. Although the first continents formed during the Archean, rock of this age makes up only 7% of the world's current cratons; even allowing for erosion and destruction of past formations, evidence suggests that only 5 to 40 percent of the present continental crust formed during the Archean.

text: There were no large continents in the early Archean, and small protocontinents were probably the norm in the

text: Mesoarchean

text: because they were prevented from coalescing into larger units by the high rate of geologic activity. These

text: felsic

text: protocontinents (cratons) probably formed at hot spots from a variety of sources: mafic magma melting more felsic rocks, partial melting of mafic rock, and from the metamorphic alteration of felsic sedimentary rocks. Although the first continents formed during the Archean, rock of this age makes up only 7% of the world's current cratons; even allowing for erosion and destruction of past formations, evidence suggests that only 5 to 40 percent of the present

text: continental crust

text: formed during the Archean.

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answers: NDQ_005571

answers: felsic

answers: NDQ_005572

answers: Archean

answers: NDQ_005573

answers: high rate of geologic activity

answers: NDQ_005574

answers: protocontinents

answers: NDQ_005575

answers: Archean

answers: NDQ_005576

answers: Grand Canyon

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Archean

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Gotland is made up of a sequence of sedimentary rocks of a Silurian age, dipping to the south-east.The main Silurian succession of limestones and shales comprises thirteen units spanning  of stratigraphic thickness, being thickest in the south, and overlies a  thick Ordovician sequence. Precambrian shield rocks that underlie these sediments are found 400 to 500 meters sea level. Sedimentary rocks cropping out in Gotland were deposited in a shallow, hot and salty sea, on the edge of an equatorial continent. The water depth never exceeded , and shallowed over time as bioherm detritus, and terrestrial sediments, filled the basin. Reef growth started in the Llandovery, when the sea was  deep, and reefs continued to dominate the sedimentary record. Some sandstones are present in the youngest rocks towards the south of the island, which represent sand bars deposited very close to the shore line.

text: Gotland

text: is made up of a sequence of

text: sedimentary rock

text: s of a

text: Silurian

text: age, dipping to the south-east.The main Silurian succession of

text: limestone

text: s and

text: shale

text: s comprises thirteen units spanning  of stratigraphic thickness, being thickest in the south, and overlies a  thick

text: Ordovician

text: sequence.

text: Precambrian

text: shield rocks

text: that underlie these sediments are found 400 to 500 meters sea level. Sedimentary rocks cropping out in Gotland were deposited in a shallow, hot and salty sea, on the edge of an equatorial continent. The water depth never exceeded , and shallowed over time as

text: bioherm

text: detritus, and terrestrial sediments, filled the basin. Reef growth started in the

text: Llandovery

text: , when the sea was  deep, and reefs continued to dominate the sedimentary record. Some sandstones are present in the youngest rocks towards the south of the island, which represent sand bars deposited very close to the shore line.

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answers: Silurian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: deposited in a shallow, hot and salty sea

answers: NDQ_005574

answers: Gotland

answers: NDQ_005575

answers: Silurian

answers: NDQ_005576

answers: Silurian succession

answers: NDQ_005577

answers: shallow, hot and salty sea

answers: NDQ_005579

answers: shallow, hot and salty sea

answer: No

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Throughout the history of the Earth, there have been times when continents collided and formed a supercontinent, which later broke up into new continents. About 1000 to 830 Ma, most continental mass was united in the supercontinent Rodinia. Rodinia may have been preceded by Early-Middle Proterozoic continents called Nuna and Columbia.

text: Throughout the history of the Earth, there have been times when continents collided and formed a supercontinent, which later broke up into new continents. About 1000 to 830 Ma, most continental mass was united in the supercontinent Rodinia. Rodinia may have been preceded by Early-Middle Proterozoic continents called Nuna and Columbia.

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answers: NDQ_005571

answers: Proterozoic

answers: NDQ_005572

answers: Rodinia

answers: NDQ_005573

answers: Rodinia

answers: NDQ_005574

answers: supercontinent

answers: NDQ_005575

answers: 1000 to 830 Ma

answers: NDQ_005576

answers: supercontinent

answers: NDQ_005577

answers: Zircons

answers: NDQ_005579

answers: Early-Middle Proterozoic

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Precambrian gneisses that comprise the Torngat Mountains are among the oldest on Earth and have been dated at roughly 3.6 to 3.9 billion years old.  Geologists recognize the gneisses of the Torngats as a part of the Canadian Shield or Laurentian Upland, which, composing the very old North American Craton, split from the continent of Rodinia roughly 750 million years ago to form the geologic core of North America.

text: Precambrian

text: gneisses

text: that comprise the Torngat Mountains are among the oldest on

text: Earth

text: and have been dated at roughly 3.6 to 3.9 billion years old.  Geologists recognize the gneisses of the Torngats as a part of the

text: Canadian Shield

text: or

text: Laurentian Upland

text: , which, composing the very old

text: North American Craton

text: , split from the continent of

text: Rodinia

text: roughly 750 million years ago to form the geologic core of

text: North America

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answers: NDQ_005572

answers: Rodinia

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answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: Precambrian

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Named in honor of George E. Williams, exploration geologist with BrokenHill Proprietary Co., Ltd. at Adelaide, South Australia. Williamsdiscovered the Lake Acraman impact structure of South Australia, the largestsuch feature found so far on the Australian continent. He also discoveredrhythmically layered sedimentary deposits of Precambrian age that exhibitperiods closely matching those of the modern solar cycle.

text: Named in honor of George E. Williams, exploration geologist with BrokenHill Proprietary Co., Ltd. at Adelaide, South Australia. Williamsdiscovered the

text: Lake Acraman impact structure

text: of South Australia, the largestsuch feature found so far on the Australian continent. He also discoveredrhythmically layered sedimentary deposits of Precambrian age that exhibitperiods closely matching those of the modern solar cycle.

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answers: NDQ_005571

answers: Precambrian

answers: NDQ_005572

answers: Precambrian

answers: NDQ_005573

answers: Precambrian

answers: NDQ_005574

answers: Lake Acraman

answers: NDQ_005575

answers: the modern solar cycle

answers: NDQ_005576

answers: impact structure

answers: NDQ_005577

answers: Lake Acraman

answers: NDQ_005579

answers: Precambrian

answer: No

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Shields vary greatly in size, ranging from large panels that protect the user's whole body to small models (such as the buckler) that were intended for hand-to-hand-combat use. Shields also vary a great deal in thickness; whereas some shields were made of relatively deep, absorbent, wooden planking to protect soldiers from the impact of spears and crossbow bolts, others were thinner and lighter and designed mainly for deflecting blade strikes.

text: Shields vary greatly in size, ranging from large panels that protect the user's whole body to small models (such as the

text: buckler

text: ) that were intended for hand-to-hand-combat use. Shields also vary a great deal in thickness; whereas some shields were made of relatively deep, absorbent, wooden planking to protect soldiers from the impact of

text: spear

text: s and

text: crossbow

text: bolts, others were thinner and lighter and designed mainly for deflecting blade strikes.

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answers: NDQ_005571

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answers: NDQ_005574

answers: 0

answers: NDQ_005575

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answers: NDQ_005576

answers: 0

answers: NDQ_005577

answers: 0

answers: NDQ_005579

answers: 0

answers: NDQ_005571

answers: planking

answers: NDQ_005572

answers: Paleogene

answers: NDQ_005573

answers: thick

answers: NDQ_005574

answers: shields also vary a great deal in thickness

answers: NDQ_005575

answers: hand-to-hand-combat

answers: NDQ_005576

answers: shields

answers: NDQ_005577

answers: It's impossible to say

answers: NDQ_005579

answers: Shields

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Irving met his wife Sheila while in Australia. She was a Canadian citizen. In 1964, they moved to Ottawa, Ontario, Canada, and Irving began work as a research officer for Dominion Observatory with the Department of Mines and Technical Surveys. In 1966, Irving returned to England to teach geophysics at the University of Leeds. He returned to Ottawa in 1967 to work as a research scientist in the Earth Physics Branch of the Department of Energy, Mines, and Resources. In 1981, Irving moved to Sidney, British Columbia, to establish a paleomagnetism laboratory at the Pacific Geoscience Centre with the Earth Physics Branch. The branch would later be incorporated into the Geological Survey of Canada. He mapped the movements of Vancouver Island and other parts of the Cordillera that have moved sideways and rotated relative to the Precambrian Canadian Shield.

text: Irving met his wife Sheila while in Australia. She was a Canadian citizen. In 1964, they moved to

text: Ottawa, Ontario

text: , Canada, and Irving began work as a research officer for

text: Dominion Observatory

text: with the Department of Mines and Technical Surveys. In 1966, Irving returned to England to teach geophysics at the

text: University of Leeds

text: . He returned to Ottawa in 1967 to work as a research scientist in the Earth Physics Branch of the Department of Energy, Mines, and Resources. In 1981, Irving moved to

text: Sidney, British Columbia

text: , to establish a paleomagnetism laboratory at the Pacific Geoscience Centre with the Earth Physics Branch. The branch would later be incorporated into the

text: Geological Survey of Canada

text: . He mapped the movements of

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text: and other parts of the

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text: that have moved sideways and rotated relative to the Precambrian Canadian Shield.

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text: The corridor coach was known on the European continent as the American system or American coach in the early 1900s.

text: The corridor coach was known on the European continent as the American system or American coach in the early 1900s.

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text: Cephalonyx is a genus of filamentous acritarchs known from the Precambrian and early Cambrian (and possibly other times).

text: Cephalonyx is a genus of filamentous acritarchs known from the Precambrian and early Cambrian (and possibly other times).

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text: Early on November 17, an extratropical low developed along a stationary front over the central Atlantic. It moved northward and became co-located with an upper-level low. After the fronts dissipated, deep convection began to initiate near the center. As a result, Subtropical Storm Melissa developed at 12:00 UTC on November 18, about  east-southeast of Bermuda. Melissa moved generally northward and strengthened slightly on November 19, but weakened later that day after convection diminished. Early on November 20, convection increased again, and after the storm acquired a warm core, it was reclassified as a tropical storm.

text: Early on November 17, an extratropical low developed along a stationary front over the central Atlantic. It moved northward and became co-located with an upper-level low. After the fronts dissipated, deep convection began to initiate near the center. As a result, Subtropical Storm Melissa developed at 12:00 UTC on November 18, about  east-southeast of Bermuda. Melissa moved generally northward and strengthened slightly on November 19, but weakened later that day after convection diminished. Early on November 20, convection increased again, and after the storm acquired a warm core, it was reclassified as a tropical storm.

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text: Geologically, the Lake Ladoga depression is a graben and syncline structure of Proterozoic age (Precambrian). This "Ladoga–Pasha structure", as it known, hosts Jotnian sediments. During the Pleistocene glaciations the depression was partially stripped of its sedimentary rock fill by glacial overdeepening.

text: Geologically, the Lake Ladoga depression is a

text: graben

text: and

text: syncline

text: structure

text: of

text: Proterozoic

text: age (

text: Precambrian

text: ). This "Ladoga–Pasha structure", as it known, hosts

text: Jotnian sediments

text: . During the

text: Pleistocene glaciation

text: s the depression was partially stripped of its

text: sedimentary rock

text: fill by glacial

text: overdeepening

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answers: Lake Ladoga depression

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answer: Yes

answer: No

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answer: 1

text: Usually platform numbering is a numbering of the boarding areas in the station (hence one island platform, for example, may have several numbered platforms).  In some cases, tracks used only for through traffic without platform access also have a number.  In North America, reference is usually made to a "track" (e.g. "The train is arriving on Track 5").  The term "platform" is also used in the US, but a single island platform may have access to two "tracks".

text: Usually platform numbering is a numbering of the boarding areas in the station (hence one island platform, for example, may have several numbered platforms).  In some cases, tracks used only for through traffic without platform access also have a number.  In North America, reference is usually made to a "track" (e.g. "The train is arriving on Track 5").  The term "platform" is also used in the US, but a single island platform may have access to two "tracks".

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text: The North Rupununi is situated on the Guiana Shield, precambrian rock with a complex geology that includes plutonic, volcanic, metamorphic and sedimentary rocks and various rifting, uplifting, sedimentation and erosion events. The geology of the North Rupununi is critical because it fundamentally defines the topography, soils, hydrology and ultimately the economy of the area.

text: The North Rupununi is situated on the

text: Guiana Shield

text: precambrian

text: rock with a complex geology that includes

text: plutonic

text: volcanic

text: metamorphic

text: and

text: sedimentary

text: rocks and various rifting, uplifting, sedimentation and

text: erosion

text: events. The geology of the North Rupununi is critical because it fundamentally defines the

text: topography

text: , soils,

text: hydrology

text: and ultimately the economy of the area.

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text: The Pyrenees form part of the huge alpine orogenic system. This 430 kilometre long, roughly east-west striking, intracontinental mountain chain divides France, Spain, and Andorra.  It has an extended, polycyclic geological evolution dating back to the Precambrian. The chain's present configuration is due to the collision between the microcontinent Iberia and the southwestern promontory of the European Plate (i.e. Southern France). The two continents were approaching each other since the onset of the Upper Cretaceous (Albian/Cenomanian) about 100 million years ago and were consequently colliding during the Paleogene (Eocene/Oligocene) 55 to 25 million years ago. After its uplift, the chain experienced intense erosion and isostatic readjustments. A cross-section through the chain shows an asymmetric flower-like structure with steeper dips on the French side. The Pyrenees are not solely the result of compressional forces, but also show an important sinistral shearing.

text: The

text: Pyrenees

text: form part of the huge

text: alpine orogenic system

text: . This 430 kilometre long, roughly east-west

text: striking

text: , intracontinental mountain chain divides

text: France

text: Spain

text: , and

text: Andorra

text: .  It has an extended, polycyclic geological evolution dating back to the

text: Precambrian

text: . The chain's present configuration is due to the

text: collision

text: between the microcontinent

text: Iberia

text: and the southwestern promontory of the

text: European Plate

text: (i.e. Southern France). The two continents were approaching each other since the onset of the

text: Upper Cretaceous

text: Albian

text: Cenomanian

text: ) about 100 million years ago and were consequently colliding during the

text: Paleogene

text: Eocene

text: Oligocene

text: ) 55 to 25 million years ago. After its uplift, the chain experienced intense

text: erosion

text: and

text: isostatic readjustments

text: . A cross-section through the chain shows an asymmetric flower-like structure with steeper dips on the French side. The Pyrenees are not solely the result of

text: compressional forces

text: , but also show an important sinistral

text: shearing

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answers: Precambrian

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answers: the Precambrian

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answers: The two continents were approaching each other

answers: NDQ_005574

answers: The Pyrenees form part of the huge alpine orogenic system

answers: NDQ_005575

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answers: NDQ_005576

answers: mountain chain

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

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answers: Precambrian

answer: Yes

answer: Yes

answer: No

answer: No

answer: No

answer: 1

text: Jet stream-powered cirrus can grow long enough to stretch across continents while remaining only a few kilometers deep. When visible light interacts with the ice crystals in cirrus cloud, it produces optical phenomena such as sun dogs and haloes. Cirrus is known to raise the temperature of the air beneath the main cloud layer by an average of 10 °C (18 °F). When the individual filaments become so extensive that they are virtually indistinguishable from one another, they form a sheet of high cloud called cirrostratus. Convection at high altitudes can produce another high-based genus called cirrocumulus, a pattern of small cloud tufts that contain droplets of supercooled water.

text: Jet stream

text: -powered cirrus can grow long enough to stretch across continents while remaining only a few kilometers deep. When visible light interacts with the ice crystals in cirrus cloud, it produces

text: optical phenomena

text: such as

text: sun dog

text: s and

text: haloes

text: . Cirrus is known to raise the temperature of the air beneath the main cloud layer by an average of 10 °C (18 °F). When the individual filaments become so extensive that they are virtually indistinguishable from one another, they form a sheet of high cloud called

text: cirrostratus

text: . Convection at high altitudes can produce another high-based genus called

text: cirrocumulus

text: , a pattern of small cloud tufts that contain droplets of

text: supercooled

text: water.

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answers: ice

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answers: supercooled water

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answers: cirrostratus

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answers: Jet stream-powered cirrus

answers: NDQ_005576

answers: cirrus

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answers: 10 °C

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Shield volcanoes, so named for their broad, shield-like profiles, are formed by the eruption of low-viscosity lava that can flow a great distance from a vent. They generally do not explode catastrophically. Since low-viscosity magma is typically low in silica, shield volcanoes are more common in oceanic than continental settings. The Hawaiian volcanic chain is a series of shield cones, and they are common in Iceland, as well.

text: Shield volcanoes, so named for their broad, shield-like profiles, are formed by the eruption of low-viscosity lava that can flow a great distance from a vent. They generally do not explode catastrophically. Since low-viscosity magma is typically low in silica, shield volcanoes are more common in oceanic than continental settings. The Hawaiian volcanic chain is a series of shield cones, and they are common in

text: Iceland

text: , as well.

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answers: magma

answers: NDQ_005572

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answers: NDQ_005573

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answers: NDQ_005574

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answers: NDQ_005575

answers: low-viscosity magma

answers: NDQ_005576

answers: shield volcano

answers: NDQ_005577

answers: shield volcanoes

answers: NDQ_005579

answers: shield volcanoes

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The first commercially successful oil well drilled in what was to be called the Mid-continent Oil Field was the Norman No. 1 near Neodesha, Kansas, on November 28, 1892. The successes that followed of the Nellie Johnstone No. 1 (Bartlesville, Oklahoma) in 1897, Spindletop (Texas) in 1901, and the Ida Glenn No. 1 (Glenn Pool, Oklahoma) in 1905, demonstrated the existence of a large oil field in the central and southwestern United States. It became known as the Mid-continent Oil Field. Continued drilling found many other oil fields and pools within the Mid-continent, both large and small.

text: The first commercially successful oil well drilled in what was to be called the Mid-continent Oil Field was the

text: Norman No. 1

text: near Neodesha, Kansas, on November 28, 1892. The successes that followed of the Nellie Johnstone No. 1 (Bartlesville, Oklahoma) in 1897,

text: Spindletop

text: (Texas) in 1901, and the Ida Glenn No. 1 (Glenn Pool, Oklahoma) in 1905, demonstrated the existence of a large oil field in the central and southwestern United States. It became known as the Mid-continent Oil Field. Continued drilling found many other oil fields and pools within the Mid-continent, both large and small.

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text: The Institute for Security Studies has engaged with the African Union on various platforms.  ISS was a research partner with the African Union Commission in the Year of Peace and Security in 2010. Additionally, the ISS website hosts as a repository for African Union documents, dating back to 1990. Finally, ISS collaborates with the African Union Peace and Security Council to produce a monthly report on the security challenges and opportunities that face the continent.

text: The Institute for Security Studies has engaged with the African Union on various platforms.  ISS was a research partner with the African Union Commission in the Year of Peace and Security in 2010. Additionally, the ISS website hosts as a repository for African Union documents, dating back to 1990. Finally, ISS collaborates with the African Union Peace and Security Council to produce a monthly report on the security challenges and opportunities that face the continent.

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text: Initially, the cloud pattern associated with the system featured a tight and well-defined circulation, as well as clusters of deep convection south of the center. Due to the proximity of a large upper-level low-pressure area in the southern Gulf of Mexico, the surrounding environment did not favor intensification. Influenced by the low, the depression moved southward. The system completed a cyclonic loop in the central gulf, and by early on September 18 was drifting northward. As a result of wind shear, the center of circulation was separated from the deep convective activity. Early the next day, deep convection persisted in a small area northeast of the center. Forward motion was nearly stationary, with a gradual drift east-southeastward. Despite the wind shear, the depression attained tropical storm status at 1200 UTC on September 19; as such, it was named Hermine by the National Hurricane Center.

text: Initially, the cloud pattern associated with the system featured a tight and well-defined circulation, as well as clusters of deep convection south of the center. Due to the proximity of a large upper-level low-pressure area in the southern Gulf of Mexico, the surrounding environment did not favor intensification. Influenced by the low, the depression moved southward. The system completed a cyclonic loop in the central gulf, and by early on September 18 was drifting northward. As a result of

text: wind shear

text: , the center of circulation was separated from the deep convective activity. Early the next day, deep convection persisted in a small area northeast of the center. Forward motion was nearly stationary, with a gradual drift east-southeastward. Despite the wind shear, the depression attained tropical storm status at 1200 UTC on September 19; as such, it was named Hermine by the

text: National Hurricane Center

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answer: No

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text: Important geological similarities link now remote Archaean cratons in India (Singhbhum and Dharwar), western Australia (Kilbaran and Pilbara), and southern Africa (Kaapvaal and Zimbabwe) which indicate that these protolithic shields were close together in the Mid-Archaean. The name "Ur", from the German prefix ur- meaning "original", was introduced by , since it is the first continent in his tectonic reconstructions. Other Archaean continental assemblages are considerably younger: Arctica (Baltica, Laurentia, and Siberia) consolidated around 2.6 Ga, Atlantica (West Africa and eastern South America) consolidated around 2.2 Ga. In some reconstructions the shields of Ur stayed near each other until the Mesozoic break-up of Gondwana.

text: Important geological similarities link now remote Archaean cratons in India (Singhbhum and Dharwar), western Australia (Kilbaran and Pilbara), and southern Africa (Kaapvaal and Zimbabwe) which indicate that these

text: protolith

text: ic shields were close together in the Mid-Archaean. The name "Ur", from the German prefix

text: ur-

text: meaning "original", was introduced by , since it is the first continent in his tectonic reconstructions. Other Archaean continental assemblages are considerably younger:

text: Arctica

text: Baltica

text: Laurentia

text: , and

text: Siberia

text: ) consolidated around 2.6 Ga,

text: Atlantica

text: West Africa

text: and

text: eastern South America

text: ) consolidated around 2.2 Ga. In some reconstructions the shields of Ur stayed near each other until the Mesozoic break-up of Gondwana.

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answers: protolithic shields

answers: NDQ_005572

answers: Ur

answers: NDQ_005573

answers: protolithic shields were close together

answers: NDQ_005574

answers: Archaean

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answers: 2.2 Ga

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answers: cratons

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answers: Zimbabwe

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answers: Mid-Archaean

answer: No

answer: No

answer: Yes

answer: No

answer: Yes

answer: 1

text: Continents formed, then broke up and reformed as the surface of Earth reshaped over hundreds of millions of years, occasionally combining to make a supercontinent. Roughly 750 million years ago, the earliest known supercontinent Rodinia, began to break apart. The continents later recombined to form Pannotia which broke apart about 540 million years ago, then finally Pangaea, which broke apart about 180 million years ago.

text: Continents formed, then broke up and reformed as the surface of Earth reshaped over hundreds of millions of years, occasionally combining to make a

text: supercontinent

text: . Roughly 750 million years ago, the earliest known supercontinent

text: Rodinia

text: , began to break apart. The continents later recombined to form

text: Pannotia

text: which broke apart about 540 million years ago, then finally

text: Pangaea

text: , which broke apart about 180 million years ago.

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answers: igneous

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answers: Rodinia

answers: NDQ_005573

answers: Continents

answers: NDQ_005574

answers: supercontinent

answers: NDQ_005575

answers: 180 million years ago

answers: NDQ_005576

answers: supercontinent

answers: NDQ_005577

answers: Zircons indicate that there was water in the environment

answers: NDQ_005579

answers: 750 million years ago

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: 1

text: Inter-racial confidence circles were renamed "inter-racial and religious confidence circles" in September 2007 to better reflect their role as constituency-level platforms for thestrengthening of engagement among religious and community leaders, and to signify their active promotion of inter-religious understanding and harmony. Following efforts by the Ministry of Community Development, Youth and Sports to recruit religious organizations into IRCCs, in 2007 about 80% of such organizations were members of IRCCs, up from 20% in 2006. In future, religious leaders will be informed of international and national events so they can help their congregations understand situations better. Religious organizations will also be involved in continency planning so that they know how to react if an incident affecting race or religion occurs.

text: Inter-racial confidence circles were renamed "inter-racial and religious confidence circles" in September 2007 to better reflect their role as constituency-level platforms for thestrengthening of engagement among religious and community leaders, and to signify their active promotion of inter-religious understanding and harmony. Following efforts by the

entity_name: Ministry of Community Development, Youth and Sports

text: Ministry of Community Development, Youth and Sports

text: to recruit religious organizations into IRCCs, in 2007 about 80% of such organizations were members of IRCCs, up from 20% in 2006. In future, religious leaders will be informed of international and national events so they can help their congregations understand situations better. Religious organizations will also be involved in continency planning so that they know how to react if an incident affecting race or religion occurs.

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text: In 1962 he attended an executive conference of African writers in English at the Makerere University College in Kampala, Uganda. He met with important literary figures from around the continent and the world, including Ghanaian poet Kofi Awoonor, Nigerian playwright and poet Wole Soyinka, and US poet-author Langston Hughes. Among the topics of discussion was an attempt to determine whether the term African literature ought to include work from the diaspora, or solely that writing composed by people living within the continent itself. Achebe indicated that it was not "a very significant question", and that scholars would do well to wait until a body of work were large enough to judge. Writing about the conference in several journals, Achebe hailed it as a milestone for the literature of Africa, and highlighted the importance of community among isolated voices on the continent and beyond.

text: In 1962 he attended an executive

text: conference of African writers in English

text: at the

text: Makerere University College

text: in

text: Kampala

text: Uganda

text: . He met with important literary figures from around the continent and the world, including Ghanaian poet

text: Kofi Awoonor

text: , Nigerian playwright and poet

text: Wole Soyinka

text: , and US poet-author

text: Langston Hughes

text: . Among the topics of discussion was an attempt to determine whether the term

text: African literature

text: ought to include work from the

text: diaspora

text: , or solely that writing composed by people living within the continent itself. Achebe indicated that it was not "a very significant question", and that scholars would do well to wait until a body of work were large enough to judge. Writing about the conference in several journals, Achebe hailed it as a milestone for the literature of Africa, and highlighted the importance of community among isolated voices on the continent and beyond.

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text: During the second week of October, an unusually large, monsoon-like lower-level circulation and a broad area of disturbed weather developed over much of the Caribbean Sea. The system was enhanced by diffluence from an upper-level low across the southwestern Atlantic. By October 13, a broad area of low pressure developed and persisted about  southeast of Jamaica, possibly aided by the passage of tropical waves through the area at the time. Convection increased and became slightly better organized, though upper-level wind shear initially prevented development. The system drifted westward, and early on October 14 the convection became more concentrated and a little better organized as upper-level wind shear lessened slightly.

text: During the second week of October, an unusually large,

text: monsoon

text: -like lower-level circulation and a broad area of disturbed weather developed over much of the Caribbean Sea. The system was enhanced by

text: diffluence

text: from an upper-level low across the southwestern Atlantic. By October 13, a broad

text: area of low pressure

text: developed and persisted about  southeast of Jamaica, possibly aided by the passage of

text: tropical wave

text: s through the area at the time.

text: Convection

text: increased and became slightly better organized, though upper-level wind shear initially prevented development. The system drifted westward, and early on October 14 the convection became more concentrated and a little better organized as upper-level wind shear lessened slightly.

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answer: 1

text: Manchuria consists mainly of the northern side of the funnel-shaped North China Craton, a large area of tilled and overlaid Precambrian rocks spanning 100 million hectares. The North China Craton was an independent continent before the Triassic period and is known to have been the northernmost piece of land in the world during the Carboniferous. The Khingan Mountains in the west are a Jurassic mountain range formed by the collision of the North China Craton with the Siberian Craton, which marked the final stage of the formation of the supercontinent Pangaea.

text: Manchuria consists mainly of the northern side of the funnel-shaped

text: North China Craton

text: , a large area of tilled and overlaid

text: Precambrian

text: rocks spanning 100 million hectares. The North China Craton was an independent continent before the

text: Triassic

text: period and is known to have been the northernmost piece of land in the world during the

text: Carboniferous

text: . The

text: Khingan Mountains

text: in the west are a Jurassic mountain range formed by the collision of the North China Craton with the

text: Siberian Craton

text: , which marked the final stage of the formation of the

text: supercontinent

text: Pangaea