Sawtooth Range (Nunavut)

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Sawtooth Range
Sawtooth Range (04-08-97).jpg
Sawtooth Range; in front: Slidre Fiord and Fosheim Peninsula
Geography
CountryCanada
RegionNunavut
Range coordinates 79°35′00″N83°15′00″W / 79.5833°N 83.25°W / 79.5833; -83.25 Coordinates: 79°35′00″N83°15′00″W / 79.5833°N 83.25°W / 79.5833; -83.25
Parent range Arctic Cordillera
Slidre Fiord with Eureka Weather Station: Fosheim Peninsula and Sawtooth Range Eureka Sawtooth Range (04-08-97).jpg
Slidre Fiord with Eureka Weather Station: Fosheim Peninsula and Sawtooth Range

The Sawtooth Range is a jagged snow-capped mountain range on central Ellesmere Island, Nunavut, Canada. It lies between the Fosheim Peninsula and the Wolf Valley. The Sawtooth Range is a subrange of the Arctic Cordillera. It also runs through a Canadian Forces Station, called Eureka, a base used to study atmospheric changes.

Contents

Geology

Widespread clastic deposits, 80–1,800 m (260–5,910 ft) long, on the eastern side of the Sawtooth Range are the result of debris flows and slushflows. [1]

See also

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Arctic Cordillera Terrestrial ecozone in northern Canada

The Arctic Cordillera is a terrestrial ecozone in northern Canada characterized by a vast, deeply dissected chain of mountain ranges extending along the northeastern flank of the Canadian Arctic Archipelago from Ellesmere Island to the northeasternmost part of the Labrador Peninsula in northern Labrador and northern Quebec, Canada. It spans most of the eastern coast of Nunavut with high glaciated peaks rising through ice fields and some of Canada's largest ice caps, including the Penny Ice Cap on Baffin Island. It is bounded to the east by Baffin Bay, Davis Strait and the Labrador Sea while its northern portion is bounded by the Arctic Ocean.

The Blue Mountains are a small mountain range on Ellesmere Island, Nunavut, Canada. It is a subrange of the Arctic Cordillera. The Blue Mountains contain Mesozoic stratigraphy.

The Prince of Wales Mountains are a mountain range running along the central-east coast of Ellesmere Island, Nunavut, Canada. The range is one of the most northern ranges in the world and of the Arctic Cordillera, which is a vast deeply dissected mountain range from Ellesmere Island to the northernmost tip of Labrador. The Prince of Wales Icefield lies mostly in the range.

Commonwealth Mountain is a mountain on Ellesmere Island, Nunavut, Canada. It lies in western Quttinirpaaq National Park, which is the most northerly extent of Canada, and is the second most northerly park on Earth after Northeast Greenland National Park.

Conger Range

The Conger Range, also called the Conger Mountains, is a mountain range in Quttinirpaaq National Park on Ellesmere Island, Nunavut, Canada, beginning about 16 km (10 mi) west of Mount Osborne. It is part of the Arctic Cordillera which is a vast dissected mountain system extending from Ellesmere Island to the northernmost tip of Labrador and northeastern Quebec. The Conger Range is a structural extension of the Garfield Range and continues into the highlands north of the head of Hare Fiord. The overall extent of the range is about 180 km (112 mi). Most of its peaks are ice-covered, although nearly all of the southern slopes are ice-free. Many of the valleys between the peaks are filled with glacial tongues spilling out to the south from the Grand Land Ice Cap. Its highest point is Mount Biederbick at 1,542 m (5,059 ft).

Norman Lockyer Island is located off the eastern coast of Ellesmere Island, and a part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. Situated in Princess Marie Bay just in front of Franklin Pierce Bay, north of Bache Peninsula, Norman Lockyer Island is within the Arctic Archipelago, a member of the Queen Elizabeth Islands.

The Fosheim Peninsula is located in western Ellesmere Island, a part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. Eureka, a permanent research community, is located on the north side of Slidre Fiord, a few kilometers east of Eureka Sound. While the peninsula was first sighted by the Arctic explorer Adolphus Greely in 1881, it was not explored until 1899 by Otto Sverdrup, who named it after Ivar Fosheim, a member of his expedition.

The Cook Peninsula is located on the eastern coast of Ellesmere Island, a part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. North of Princess Marie Bay, it stretches eastward into Nares Strait. The peninsula is approximately 64 square kilometres (25 sq mi) in size, and has two lowland areas frequented by muskox.

Peary Bay is an Arctic waterway in Qikiqtaaluk Region, Nunavut, Canada. It is located in Nares Strait by eastern Ellesmere Island between the Cook Peninsula and the Bache Peninsula.

Flagler Bay is an Arctic waterway in Qikiqtaaluk Region, Nunavut, Canada. It is located in Nares Strait by eastern Ellesmere Island between Bache Peninsula and Knud Peninsula.

Fosheim may refer to:

The Eurekan orogeny was a Phanerozoic mountain building event that affected the eastern portion of the Arctic Archipelago and, to a lesser extent, northern Greenland. Deformation initiated in the Late Cretaceous, during which time the Sverdrup Basin began to fragment and fold in response to the counterclockwise rotation of Greenland, caused by seafloor spreading in the Canadian Arctic Rift System. Isostatic uplift was most pronounced in the Grantland Mountains and Victoria and Albert Mountains on Ellesmere Island and in the Princess Margaret Range on Axel Heiberg Island, as evidenced by the current physiography. Compression in a broad zone on Ellesmere Island resulted in the formation of the Eurekan Fold Belt.

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