Lake Hazen

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Lake Hazen
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Lake Hazen
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Lake Hazen
Location118 km (73 mi) southwest of Alert, Nunavut
Coordinates 81°48′N71°00′W / 81.800°N 71.000°W / 81.800; -71.000 (Lake Hazen)
Primary inflows Glaciers of the Eureka Uplands:
Henrietta Nesmith Glacier
Gilmour Glaciers
Primary outflows Ruggles River
Catchment area 4,900 km2 (1,900 sq mi)
Basin  countriesCanada
Max. length74 km (46 mi) [1]
Max. width12 km (7 mi) [1]
Surface area537.5 km2 (207.5 sq mi) [1]
Max. depth267 m (876 ft) [2]
Water volume51.4×10^9 m3 (41.7×10^6 acre⋅ft) [2]
Shore length1185 km (115 mi)
Surface elevation158 m (518 ft) [1]
Islands St. John's Island
Settlements Hazen Camp
1 Shore length is not a well-defined measure.
Lake Hazen within Quttinirpaaq National Park Quttinirpaaq National Park map-fr.png
Lake Hazen within Quttinirpaaq National Park

Lake Hazen is a freshwater lake in the northern part of Ellesmere Island, Nunavut, Canada, north of the Arctic Circle. It is the largest lake north of the Arctic Circle by volume. By surface area it is third largest, after Lake Taymyr in Russia and Lake Inari in Finland.

Contents

The area around the lake is a thermal oasis within a polar desert, with summer temperatures up to 20 °C (68 °F). [2] The lake itself is covered by ice about ten months a year. It is fed by glaciers (most importantly Henrietta Nesmith and the Gilmour Glaciers) from the surrounding Eureka UplandsPalaeozoic rocks north of the lake, rising up to 2,500 m (8,200 ft) above sea level—and drained by the 15 km-long (9.3 mi) Ruggles River, which flows into Chandler Fjord on the northern east coast of Ellesmere Land. The lake is flanked by the Arctic Cordillera.

The lake is 74 km (46 mi) long and up to 12 km (7 mi) wide, with an area of 537.5 km2 (207.5 sq mi). [1] It stretches in a southwest–northeast direction from 81°40′N72°58′W / 81.667°N 72.967°W / 81.667; -72.967 (Lake Hazen (southwest)) to 81°56′N68°55′W / 81.933°N 68.917°W / 81.933; -68.917 (Lake Hazen (northeast)) . The lake is up to 269 m (883 ft) deep and has an estimated volume of 51.4 km3. [2] The shoreline is 185 km (115 mi) long and 158 m (518 ft) above sea level. The lake has several islands, the largest of them being Johns Island, which is 7 km (4.3 mi) long and less than 1 km (0.62 mi) wide, also extending in a southwest–northeast direction like the lake itself. Other islands include Gatter Island, Clay Island (both close to the northeastern shore), Whisler Island, and Dyas Island (both close to the southern shore).

Lake Hazen is often called the northernmost lake of Canada, but detailed maps show several smaller lakes up to more than 100 km (62 mi) farther north. Turnabout Lake is immediately northeast of the northern end of Lake Hazen. Still further north are the Upper and Lower Dumbell Lakes, with Upper Dumbell Lake 5.2 km (3 mi) southwest of Alert, Canada's northernmost settlement on the coast of the Lincoln Sea, part of the Arctic Ocean. [3]

The northeastern end of Lake Hazen is 118 km (73 mi) southwest of Alert.

The lake is part of Quttinirpaaq National Park.

Artifacts of the Thule civilization were discovered near Lake Hazen in 2004. [4] These included ruins of a stone dwelling near the Ruggles River and discarded fish bones, suggesting an overwintering fishing camp where the strong current resisted freezing over. [5] The Thule were ancestors of the Inuit. In 1882, Adolphus Greely was the first European to discover the lake during his 1881–1883 expedition. He named the lake in honour of General William Babcock Hazen, who had organized the expedition. [1] Camp Hazen was established on the northern shore of the lake in 1957 during the International Geophysical Year (IGY), and has been used by various scientific parties since then.

Lake Hazen is populated by two morphotypes of Arctic char, a larger and a smaller. Studies in the 1990s indicated neither char morphotype is anadromous, but Inuit traditional knowledge states otherwise. [6]

Named inflows

All named rivers and creeks are listed in a clockwise manner, starting in the south:

At the southwestern end (from south to north):

On the northwest coast (from southwest to northeast):

At the northeast end (from north to south):

On the southeast coast (only in the southwest, near the southwest end of the lake):

Tourism

Hikers can start their hiking trips at Lake Hazen itself, or from Tanquary Fiord warden station at Tanquary Fiord Airport 70 km (43 mi) southwest of the lake.

Lake Hazen is the setting of a major story plot in the novel Good Morning, Midnight , published 2016. [7] A film adaptation of that book was released in 2020 under the title The Midnight Sky , although the actual filming was done in Iceland. [8]

Related Research Articles

<span class="mw-page-title-main">Ellesmere Island</span> Island of the Arctic Archipelago in Nunavut, Canada

Ellesmere Island is Canada's northernmost and third largest island, and the tenth largest in the world. It comprises an area of 196,236 km2 (75,767 sq mi), slightly smaller than Great Britain, and the total length of the island is 830 km (520 mi).

<span class="mw-page-title-main">Quttinirpaaq National Park</span> National park in Nunavut, Canada

Quttinirpaaq National Park is located on the northeastern corner of Ellesmere Island in the Qikiqtaaluk Region of Nunavut, Canada. It is the second most northerly park on Earth after Northeast Greenland National Park. In Inuktitut, Quttinirpaaq means "top of the world". It was established as Ellesmere Island National Park Reserve in 1988, and the name was changed to Quttinirpaaq in 1999, when Nunavut was created, and became a national park in 2000. The reserve covers 37,775 km2 (14,585 sq mi), making it the second largest park in Canada, after Wood Buffalo National Park.

<span class="mw-page-title-main">Qikiqtaaluk Region</span> Region of Nunavut, Canada

The Qikiqtaaluk Region, Qikiqtani Region or the Baffin Region is the easternmost, northernmost, and southernmost administrative region of Nunavut, Canada. Qikiqtaaluk is the traditional Inuktitut name for Baffin Island. Although the Qikiqtaaluk Region is the most commonly used name in official contexts, several notable public organizations, including Statistics Canada prior to the 2021 Canadian census, use the older term Baffin Region.

<span class="mw-page-title-main">Arctic char</span> Species of fish

The Arctic char or Arctic charr is a cold-water fish in the family Salmonidae, native to alpine lakes, as well as Arctic and subarctic coastal waters in the Holarctic.

<span class="mw-page-title-main">Tanquary Fiord Airport</span> Airport in Tanquary Fiord, Nunavut

Tanquary Fiord Airport is located at the southern side of Tanquary Fiord, Nunavut, Canada, close to the end of the fiord. It is located within Quttinirpaaq National Park and is maintained by Parks Canada. It serves as the main access to the park for tourists. Hikers to Lake Hazen, which is located 70 km (43 mi) to the northeast, start from Tanquary Camp.

The Turnabout River is located on Ellesmere Island, Nunavut, Canada. It drains both Turnabout Lake and Turnabout Glacier into Lake Hazen.

Turnabout Lake is a lake in Qikiqtaaluk Region, Nunavut, Canada. It is located northeast of Lake Hazen on Ellesmere Island, It is drained by the Turnabout River which flows into Lake Hazen.

Geoffrey Francis Hattersley-Smith D.Phil, FRSC, FRGS, FAINA was an English-born Canadian geologist and glaciologist, recognized as a pioneering researcher of Northern Canada.

<span class="mw-page-title-main">Garfield Range</span> Mountain range in Nunavut, Canada

The Garfield Range is a mountain range on Ellesmere Island, Nunavut, Canada. The mountains are made of Paleozoic rocks and rise to heights between 1,067 m (3,501 ft) and 1,433 m (4,701 ft) and are separated by valleys through which flow the major rivers fed by the ice fields and glaciers. Like most of the mountain ranges in the Arctic, it is one of the world's northernmost mountain ranges.

<span class="mw-page-title-main">Conger Range</span> Mountain range in Nunavut, Canada

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).

<span class="mw-page-title-main">Osborn Range</span> Mountain range in Nunavut, Canada

The Osborn Range is a small mountain range located on the northwest flank of Tanquary Fiord on north-central Ellesmere Island, Nunavut, Canada. It lies just outside Quttinirpaaq National Park and is one of the northernmost mountain ranges in the world forming part of the Arctic Cordillera.

<span class="mw-page-title-main">Gull Glacier</span> Glacier in Nunavut, Canada

Gull Glacier is a glacier in the Osborn Range of north-central Ellesmere Island, Nunavut, Canada. It lies in the Tanquary Fiord in Quttinirpaaq National Park.

<span class="mw-page-title-main">Ward Hunt Island</span> Island in Nunavut, Canada

Ward Hunt Island is a small, uninhabited island in the Arctic Ocean, located off the north coast of Ellesmere Island near the Ward Hunt Ice Shelf. The island is located just 750 km (470 mi) from the geographical North Pole. The northern cape of Ward Hunt Island is one of the northernmost elements of land in Canada. Only a 17 km (11 mi) stretch of northern coast of Ellesmere Island around Cape Columbia is more northerly. The island is 5.0 km (3.1 mi) long, east to west, and 3.0 km (1.9 mi) wide. The first known sighting was in 1876 by Pelham Aldrich, a lieutenant with the George Nares expedition, and named for George Ward Hunt, who was First Lord of the Admiralty at the time (1874–1877). Today, the Island is part of the Quttinirpaaq National Park.

Greely Fiord is a natural inlet in the west of Ellesmere Island, Qikiqtaaluk Region, Nunavut in the Arctic Archipelago. To the south lies the Cañon Fiord and the Agassiz Ice Cap. To the northwest is Borup Fiord and Tanquary Fiord is northeast.

The Ruggles River is a waterway in Qikiqtaaluk Region, Nunavut, Canada. It is located within Ellesmere Island's Quttinirpaaq National Park. The Ruggles River flows southeast to Chandler Fiord and out to Lady Franklin Bay.

<span class="mw-page-title-main">Tanquary Fiord</span> Fjord on Ellesmere Island, Nunavut, Canada

Tanquary Fiord is a fjord on the north coast of the Arctic Archipelago's Ellesmere Island, Nunavut, Canada. It is located in the Quttinirpaaq National Park and extends 48 km (30 mi) in a north-westerly direction from Greely Fiord.

Hazen Camp is a shelter maintained and operated by Parks Canada. It contains many all-weather shelters for the park staff. The visiting researchers set up tents in the camp area.

Kangiqtualuk Uqquqti formerly Sam Ford Fiord is an isolated, elongated Arctic fjord on Baffin Island's northeastern coast in the Qikiqtaaluk Region of Nunavut, Canada. The Inuit settlement of Pond Inlet is 320 km (200 mi) to the northwest and Clyde River is 80 km (50 mi) to the east.

Arviqtujuq Kangiqtua formerly Eglinton Fiord is a fjord on Baffin Island's northeastern coast in the Qikiqtaaluk Region of Nunavut, Canada. The Inuit settlement of Pond Inlet is 355 km (221 mi) to the northwest and Clyde River is 55 km (34 mi) to the east.

<span class="mw-page-title-main">Remote Peninsula</span> Peninsula in Nunavut, Canada

The Remote Peninsula is a peninsula located on the eastern coast of Baffin Island. It is part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. The Inuit settlement of Pond Inlet is 295 km (183 mi) to the northwest and Clyde River is 90 km (56 mi) to the southeast.

References

  1. 1 2 3 4 5 6 Mark Nuttal: Encyclopedia of the Artctic. Routledge, 2012, ISBN   9781136786808, S. 835-836 ( excerpt , p. 835, at Google Books)
  2. 1 2 3 4 G. KÖCK, D. MUIR, F. YANG, X. WANG, C. TALBOT, N. GANTNER, D. MOSER: Bathymetry and Sediment Geochemistry of Lake Hazen (Quttinirpaaq National Park, Ellesmere Island, Nunavut). Arctic, Vol. 65, No. 1 (MARCH 2012), pp. 56-66 (JSTOR)
  3. "Description of Lake Hazen". University of Guelph. Archived from the original on 2011-05-18. Retrieved 2008-02-10.
  4. Greg Younger-Lewis (October 29, 2004). "Ambitious plan proposed for Quttinirpaaq National Park". nunatsiaq. Archived from the original on November 14, 2006. Retrieved 2008-02-10.
  5. Dick, Lyle (2001). Muskox Land: Ellesmere Island in the Age of Contact. University of Calgary Press. p. 36. ISBN   978-1-55238-050-5.
  6. Douglas Clark, “Assessing the Health of the Lake Hazen Ecosystem, Ellesmere Island, Northwest Territories,” Parks Canada, 1997. Archived from the original on 2007-09-28. Retrieved 2020-05-14. “Two morphotypes of Arctic char are present in Lake Hazen: a large, cannibalistic form, and a small, presumably benthic-feeding form (Reist et al. 1995). Taken together, the results of both radiotelemetry studies in 1995–6 (Babaluk et al. in prep.) and, more conclusively, strontium uptake by char (Halden et al. 1996) suggest that neither form is anadromous. However, this is in contradiction to Inuit traditional knowledge, which holds that the char in Lake Hazen do go to sea (Ellesmere Island National Park Reserve Advisory Board, March 5, 1997). A comprehensive demographic analysis of the char population of Lake Hazen is in progress (J. Reist, pers. comm.). Fecundity information is still required.”
  7. "Good Morning Midnight Imagines the World Gone Dark" . Retrieved 2024-04-06.
  8. "Where was The Midnight Sky filmed? Explore the filming locations of George Clooney's Netflix film". Archived from the original on 2020-12-25. Retrieved 2020-12-25.