McDougall Sound

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McDougall Sound
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McDougall Sound
Coordinates 75°15′N097°30′W / 75.250°N 97.500°W / 75.250; -97.500 (McDougall Sound) Coordinates: 75°15′N097°30′W / 75.250°N 97.500°W / 75.250; -97.500 (McDougall Sound)
Basin  countries Canada
SettlementsUninhabited

McDougall Sound is an Arctic waterway in Qikiqtaaluk, Nunavut, Canada. It is located between southeastern Bathurst Island and western Cornwallis island. The sound's southern mouth opens to the Parry Channel, and beyond that, to the Barrow Strait. The sound's northern mouth opens to Crozier Strait. [1] The sound is populated by several smaller islands, the named ones including Milne Island, Little Cornwallis Island, Wood Island, Neal Islands, Truro Island, and Baker Island. [2]

Contents

McDougall Sound is the namesake of George F. McDougall who explored the sound in 1851 while wintering with Capt. Horatio Austin's search team seeking the lost Franklin Expedition. [3]

Fauna

The sound is home to bearded seal. [4] Atlantic walrus (O. rosmarus rosmarus) have also been charted as far west as McDougall Sound. [5]

Ethnography

In his 1990 study of Paleo-Eskimo people (who preceded the Inuit), Helmer describes three occupation periods in the McDougall Sound region: Transitional Period Dorset (ca. 3000 BP), Early Dorset (2500—2200 BP), and Late Dorset (ca. 1500—1000 BP), demonstrating abrupt ends to three sets of occupations by Palaeo-Eskimo hunters. [6] The University of Calgary's McDougall Sound Arctic Research Project continued this work. [7]

Related Research Articles

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The walrus is a large flippered marine mammal with a discontinuous distribution about the North Pole in the Arctic Ocean and subarctic seas of the Northern Hemisphere. The walrus is the only living species in the family Odobenidae and genus Odobenus. This species is subdivided into two subspecies: the Atlantic walrus, which lives in the Atlantic Ocean, and the Pacific walrus, which lives in the Pacific Ocean.

Ellesmere Island 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 196,235 km2 (75,767 sq mi), slightly smaller than Great Britain, and the total length of the island is 830 km (520 mi).

Melville Island (Northwest Territories and Nunavut) Island of the Arctic Archipelago

Melville Island is an uninhabited island of the Arctic Archipelago with an area of 42,149 km2 (16,274 sq mi). It is the 33rd largest island in the world and Canada's eighth largest island.

Cornwallis Island (Nunavut)

Cornwallis Island is one of the Queen Elizabeth Islands, part of the Arctic Archipelago, in the Qikiqtaaluk Region of Nunavut in the Canadian Arctic. It lies to the west of Devon Island and at its greatest length is about 113 km (70 mi). At 6,995 km2 (2,701 sq mi) in size, it is the 96th largest island in the world, and Canada's 21st largest island. Cornwallis Island is separated by the Wellington Channel from Devon Island, and by the Parry Channel from Somerset Island to the south. Northwest of Cornwallis Island lies Little Cornwallis Island, the biggest of a group of small islands at the north end of McDougall Sound, which separates Cornwallis Island from nearby Bathurst Island.

Southampton Island

Southampton Island is a large island at the entrance to Hudson Bay at Foxe Basin. One of the larger members of the Canadian Arctic Archipelago, Southampton Island is part of the Kivalliq Region in Nunavut, Canada. The area of the island is stated as 41,214 km2 (15,913 sq mi) by Statistics Canada. It is the 34th largest island in the world and Canada's ninth largest island. The only settlement on Southampton Island is Coral Harbour, called Salliq in Inuktitut.

Little Cornwallis Island

Little Cornwallis Island is one of the Canadian Arctic islands in Nunavut, Canada. It is located at 75°30'N 96°30'W, between Cornwallis Island and Bathurst Island in McDougall Sound, and measures 412 km2 (159 sq mi). It is uninhabited.

Foxe Basin Oceanic basin north of Hudson Bay, in Nunavut, Canada

Foxe Basin is a shallow oceanic basin north of Hudson Bay, in Nunavut, Canada, located between Baffin Island and the Melville Peninsula. For most of the year, it is blocked by sea ice and drift ice made up of multiple ice floes.

The Arctic Small Tool tradition (ASTt) was a broad cultural entity that developed along the Alaska Peninsula, around Bristol Bay, and on the eastern shores of the Bering Strait around 2500 BC. ASTt groups were the first human occupants of Arctic Canada and Greenland. This was a terrestrial entity that had a highly distinctive toolkit based on microblade technology. Typically tool types include scrapers, burins and side and end blades used in composite arrows or spears made of other materials, such as bone or antler. Many researchers also assume that it was Arctic Small Tool populations who first introduced the bow and arrow to the Arctic, that eventually became the Eskimo archery material culture. ASTt camps are often found along coasts and streams, to take advantage of seal or salmon populations. While some of the groups were fairly nomadic, more permanent, sod-roofed homes have also been identified from Arctic Small Tool tradition sites.

History of Nunavut

The history of Nunavut covers the period from the arrival of the Paleo-Eskimo thousands of years ago to present day. Prior to the colonization of the continent by Europeans, the lands encompassing present-day Nunavut were inhabited by several historical cultural groups, including the Pre-Dorset, the Dorsets, the Thule and their descendants, the Inuit.

Based on archeological finds, Brooman Point Village is an abandoned village in Qikiqtaaluk Region, Nunavut, Canada. It is located in the central High Arctic on a point of the Gregory Peninsula, part of the eastern coast of Bathurst Island. Brooman was both a Late Dorset culture Paleo-Eskimo village as well as an Early Thule culture village. Both the artifacts and the architecture, specifically longhouses, are considered important historical remains of the two cultures. The site shows traces of Palaeo-Eskimo occupations between about 2000 BC and 1 AD, but the major prehistoric settlement occurred from about 900 to 1200 AD.

Pitsiulartok

Pitsiulartok or Pituilaktok, is a small, uninhabited island located at 63°15'N, 90°33'W in Hudson Bay, about 13 km from the community of Chesterfield Inlet, Nunavut, Canada. The narrow island is about 3.5 km in length and barely 1 km wide at its widest point. Traditionally it was a walrus-hunting ground for the local Inuit, and a landmark for southern whalers. It is part of a loose chain of small islands running along the coast, including Sakpik Island and Promise Island.

Barrow Strait Waterway in Northern Canadas territory of Nunavut

Barrow Strait is a shipping waterway in Northern Canada's territory of Nunavut. Forming part of the Parry Channel, the strait separates several large islands including Cornwallis Island and Devon Island to the north, from Prince of Wales Island, Somerset Island, and Prince Leopold Island to the south.

Lowther Island

Lowther Island lies within the Canadian Arctic Archipelago in the Qikiqtaaluk Region of northern Canada's territory of Nunavut. It is one of the mid-channel islands in the western sector of Barrow Strait. Bathurst Island and Cornwallis Island are to the north, while Prince of Wales Island is to the south. The island is clustered within a group of uninhabited islands. It is 15.5 mi (24.9 km) northeast of Young Island, separated by the Kettle Passage, a shipping route, and 13 mi (21 km) southeast of Garrett Island, separated by Hayes Channel.

Griffith Island (Nunavut)

Griffith Island lies within the Arctic Archipelago in the Qikiqtaaluk Region of northern Canada's territory of Nunavut. It is one of the mid-channel islands in the western sector of Barrow Strait.

Truro Island

Truro Island lies within the Canadian Arctic Archipelago in the Qikiqtaaluk Region of northern Canada's territory of Nunavut. It is one of the mid-waterway islands in the McDougall Sound between Bathurst Island and Cornwallis Island. Long and narrow, the island is 21 km2 (8.1 sq mi).

Crozier Strait is a natural waterway in Qikiqtaaluk, Nunavut, Canada. It separates Bathurst Island's Gregory Peninsula to the west from Milne Island and Little Cornwallis Island to the east. The strait, an arm of the Arctic Ocean, connects Queens Channel to the north with the McDougall Sound to the south. Kalvik Island is located within the strait, as is Karluk Island, an archaeological site.

Parry Channel Natural waterway through the central Canadian Arctic Archipelago

The Parry Channel is a natural waterway through the central Canadian Arctic Archipelago. Its eastern two-thirds lies in the territory of Nunavut, while its western third lies in the Northwest Territories. It runs east to west, connecting Baffin Bay in the east with the Beaufort Sea in the west. Its eastern end is the only practical entrance to the Northwest Passage. Its western end would be a natural exit from the archipelago were it not filled with ice. The channel separates the Queen Elizabeth Islands to the north from the rest of Nunavut.

Dundas Island (Nunavut)

Dundas Island is a member of the Queen Elizabeth Islands and the Canadian Arctic Archipelago in the territory of Nunavut. It is an irregularly shaped island located between Devon Island and Baillie-Hamilton Island. The smaller Margaret Island is 1 km (0.62 mi) to the east of Dundas.

Nimigen Island

Nimigen Island is an uninhabited Baffin Island offshore island located in the Canadian Arctic Archipelago in Nunavut's Qikiqtaaluk Region. It lies in Cumberland Sound, approximately 10.5 km (6.5 mi) east of Robert Peel Inlet To its east is Utsusivik Island; south is Chidliak Bay.

The Pre-Dorset is a loosely defined term for a Paleo-Eskimo culture or group of cultures that existed in the Eastern Canadian Arctic from c. 3200 to 850 cal BC, and preceded the Dorset culture.

References

  1. "Cornwallis Island". The Columbia Gazetteer of North America. 2000. Retrieved 2008-04-30.
  2. "Map of McDougall Sound (sound), Nunavut, Canada". encarta.msn.com. 2007. Retrieved 2008-04-30.[ dead link ]
  3. Bray, E. F. d., & Barr, W. (1992). A Frenchman in search of Franklin: de Bray's Arctic journal, 1852-1854. Toronto: University of Toronto Press. pp. 48–50. ISBN   0-8020-2813-6.CS1 maint: multiple names: authors list (link)
  4. Stirling, I., Cleator, H., & Calvert, W. (1980). "Underwater vocalizations as a tool for studying the distribution and relative abundance of wintering pinnipeds in the High Arctic" (PDF). Calgary, Alta: Pallister Resource Management Ltd. OCLC   16581532.CS1 maint: multiple names: authors list (link)
  5. Harington, C. R. (August 1966). "Extralimital Occurrences of Walruses in the Canadian Arctic". 47 (3). Journal of Mammalogy: 506–513. OCLC   65831135 . Retrieved 2008-04-30.Cite journal requires |journal= (help)
  6. Helmer, James W. (1990-06-05). "The Palaeo-Eskimo Prehistory of the North Devon Lowlands" (PDF). 44 (4). Arctic: 301–317.Cite journal requires |journal= (help)
  7. Helmer, James; LeMoine, Genevieve (1995). "McDougall Sound Arctic Research Project". ucalgary.ca. Archived from the original on 2008-03-07. Retrieved 2008-04-30.