Innuitian Mountains: Difference between revisions
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The Innuitian Mountains' present form was shaped during the [[Innuitian orogeny]] in the middle of the [[Mesozoic]] [[Era]] when the [[North American Plate]] moved northward. The Innuitian Mountains contain [[igneous rock|igneous]] and [[metamorphic rock]]s, but for the most part are composed of [[sedimentary rock]]. They are younger than the [[Appalachian Mountains|Appalachians]], so [[erosion]] has not yet rounded them significantly. |
The Innuitian Mountains' present form was shaped during the [[Innuitian orogeny]] in the middle of the [[Mesozoic]] [[Era]] when the [[North American Plate]] moved northward. The Innuitian Mountains contain [[igneous rock|igneous]] and [[metamorphic rock]]s, but for the most part are composed of [[sedimentary rock]]. They are younger than the [[Appalachian Mountains|Appalachians]], so [[erosion]] has not yet rounded them significantly. |
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The Innuitian Mountains resemble the Appalachian Mountains in composition and contain similar types of [[mineral]]s. The mineral resources have not been greatly exploited, due to the cost of developing such a remote region while cheaper alternatives are available elsewhere. The estimated amount of resources in the Arctic Region is estimated to have 13% of all the world's oil and 30% of the world's gas reserves. {{citation needed|date=February 2017}}<ref>{{Cite journal|last=Gautier|first=Donald|date=May 29, 2009|title=Assessment of Undiscovered Oil and Gas in the Arctic|url=https://nammco.no/wp-content/uploads/2019/02/o17wwg-gautier-et-al-2009-assessment-undiscovered-oil-arctic.pdf|journal=Science |
The Innuitian Mountains resemble the Appalachian Mountains in composition and contain similar types of [[mineral]]s. The mineral resources have not been greatly exploited, due to the cost of developing such a remote region while cheaper alternatives are available elsewhere. The estimated amount of resources in the Arctic Region is estimated to have 13% of all the world's oil and 30% of the world's gas reserves. {{citation needed|date=February 2017}}<ref>{{Cite journal|last=Gautier|first=Donald|date=May 29, 2009|title=Assessment of Undiscovered Oil and Gas in the Arctic|url=https://nammco.no/wp-content/uploads/2019/02/o17wwg-gautier-et-al-2009-assessment-undiscovered-oil-arctic.pdf|journal=Science |volume=324|issue=5931|pages=1175–9|doi=10.1126/science.1169467|pmid=19478178|bibcode=2009Sci...324.1175G|via=}}</ref> |
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==See also== |
==See also== |
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Revision as of 23:36, 23 April 2020
 | This article needs additional citations for verification. (March 2015) |
| Innuitian Mountains | |
|---|---|
 British Empire Range, in the north of Tanquary Fiord | |
| Highest point | |
| Peak | Barbeau Peak |
| Elevation | 2,616 m (8,583 ft) |
| Coordinates | 81°54′30″N 75°01′30″W / 81.90833°N 75.02500°W |
| Geography | |
| Country | Canada |
| Regions | Nunavut and Northwest Territories |
| Parent range | Arctic Cordillera |
| Geology | |
| Orogeny | Innuitian |
| Age of rock | Mesozoic |
| Type of rock | Igneous, Metamorphic and Sedimentary |
The Innuitian Mountains are a mountain range in Nunavut and the Northwest Territories, Canada. They are part of the Arctic Cordillera and are largely unexplored, due to the hostile climate. They are named after the northern indigenous people, the Inuit. In some locations the Innuitian Mountains measure over 2,500 m (8,202 ft) in height, and 1,290 km (802 mi) in length. The highest point is Barbeau Peak at 2,616 m (8,583 ft). There are no trees or very minimal wildlife in the Innuitian Mountains due to the harsh cold climate as well as being located north of the Arctic tree line. This region is mostly barren with vast areas of permafrost. There are metallic mineral resources including iron and zinc and fossil fuel resources such as coal.
The Innuitian Mountains consist of numerous smaller mountain ranges. Some of these are the British Empire Range, the Princess Margaret Range and the United States Range, which is the world's second most Northern mountain range after the Challenger Mountains.
The Innuitian Mountains were first seen by European explorers in 1882 by the explorer Adolphus Greely from Lake Hazen.
Geology
The Innuitian Mountains' present form was shaped during the Innuitian orogeny in the middle of the Mesozoic Era when the North American Plate moved northward. The Innuitian Mountains contain igneous and metamorphic rocks, but for the most part are composed of sedimentary rock. They are younger than the Appalachians, so erosion has not yet rounded them significantly.
The Innuitian Mountains resemble the Appalachian Mountains in composition and contain similar types of minerals. The mineral resources have not been greatly exploited, due to the cost of developing such a remote region while cheaper alternatives are available elsewhere. The estimated amount of resources in the Arctic Region is estimated to have 13% of all the world's oil and 30% of the world's gas reserves. [citation needed][1]
See also
References
- ^ Gautier, Donald (May 29, 2009). "Assessment of Undiscovered Oil and Gas in the Arctic" (PDF). Science. 324 (5931): 1175–9. Bibcode:2009Sci...324.1175G. doi:10.1126/science.1169467. PMID 19478178.
- Clark, Bruce W. and Wallace, John K. Making Connections: Canada's Geography, Pearson Education Canada; 1st Edition 1999 ISBN 0-7702-6633-9
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