| Rosse Bay | |
|---|---|
  Rosse Bay  Rosse Bay | |
| Location | Nares Strait |
| Coordinates | 78°40′N74°35′W / 78.667°N 74.583°W |
| Basin countries | Canada |
| Settlements | Uninhabited |
Rosse Bay is an Arctic waterway in Qikiqtaaluk Region, Nunavut, Canada. It is located in Nares Strait between Pim Island and Ellesmere Island's Johan Peninsula. The bay is also connected to Rice Strait.
Physical characteristics include a gravel and sand moraine ridge on its southwestern shore. [1] There are also tidewater glaciers. The main discharge of Lefferts Glacier is into Rosse Bay. [2]
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).
Victoria Island is a large island in the Arctic Archipelago that straddles the boundary between Nunavut and the Northwest Territories of Canada. It is the eighth-largest island in the world, and at 217,291 km2 (83,897 sq mi) in area, it is Canada's second-largest island. It is nearly double the size of Newfoundland (111,390 km2 [43,010 sq mi]), and is slightly larger than the island of Great Britain (209,331 km2 [80,823 sq mi]) but smaller than Honshu (225,800 km2 [87,200 sq mi]). The western third of the island lies in the Inuvik Region of the Northwest Territories; the remainder is part of Nunavut's Kitikmeot Region. The population of 2,168 is divided among two settlements, the larger of which is in Nunavut and the other of which is in the Northwest Territories.
Frobisher Bay is an inlet of the Davis Strait in the Qikiqtaaluk Region of Nunavut, Canada. It is located in the southeastern corner of Baffin Island. Its length is about 230 km (140 mi) and its width varies from about 40 km (25 mi) at its outlet into the Labrador Sea to roughly 20 km (12 mi) towards its inner end.
The Continental Divide of the Americas is the principal, and largely mountainous, hydrological divide of the Americas. The Continental Divide extends from the Bering Strait to the Strait of Magellan, and separates the watersheds that drain into the Pacific Ocean from those river systems that drain into the Atlantic and Arctic Ocean, including those that drain into the Gulf of Mexico, the Caribbean Sea, and Hudson Bay.
Baffin Bay, located between Baffin Island and the west coast of Greenland, is defined by the International Hydrographic Organization as a marginal sea of the Arctic Ocean. It is sometimes considered a sea of the North Atlantic Ocean. It is connected to the Atlantic via Davis Strait and the Labrador Sea. The narrower Nares Strait connects Baffin Bay with the Arctic Ocean. The bay is not navigable most of the year because of the ice cover and high density of floating ice and icebergs in the open areas. However, a polynya of about 80,000 km2 (31,000 sq mi), known as the North Water, opens in summer on the north near Smith Sound. Most of the aquatic life of the bay is concentrated near that region.
Severnaya Zemlya is a 37,000 km2 (14,000 sq mi) archipelago in the Russian high Arctic. It lies off Siberia's Taymyr Peninsula, separated from the mainland by the Vilkitsky Strait. This archipelago separates two marginal seas of the Arctic Ocean, the Kara Sea in the west and the Laptev Sea in the east.
Davis Strait is a northern arm of the Atlantic Ocean that lies north of the Labrador Sea. It lies between mid-western Greenland and Baffin Island in Nunavut, Canada. To the north is Baffin Bay. The strait was named for the English explorer John Davis (1550–1605), who explored the area while seeking a Northwest Passage. By the 1650s it was used for whale hunting.
The Queen Elizabeth Islands are the northernmost cluster of islands in Canada's Arctic Archipelago, split between Nunavut and the Northwest Territories in Northern Canada. The Queen Elizabeth Islands contain approximately 14% of the global glacier and ice cap area.
Boothia Peninsula is a large peninsula in Nunavut's northern Canadian Arctic, south of Somerset Island. The northern part, Murchison Promontory, is the northernmost point of mainland Canada.
Kane Basin is an Arctic waterway lying between Greenland and Canada's northernmost island, Ellesmere Island. It links Smith Sound to Kennedy Channel and forms part of Nares Strait. It is approximately 180 kilometres in length and 130 km at its widest.
Etah is an abandoned settlement in the Avannaata municipality in northern Greenland. It was a starting point of discovery expeditions to the North Pole and the landing site of the last migration of the Inuit from the Canadian Arctic.
Hall Island is an island of the Russian Arctic archipelago of Franz Josef Land.
Pim Island is an uninhabited island located off the eastern coast of Ellesmere Island, part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. Located within the Arctic Archipelago, it is a part of the Queen Elizabeth Islands.
Rice Strait is a narrow waterway between Ellesmere Island's eastern coast and Pim Island in northern Canada's territory of Nunavut. It connects Rosse Bay on the south with Buchanan Bay to the north.
The Johan Peninsula is located on the eastern coast of Ellesmere Island, a part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. It stretches eastward into Nares Strait. Buchanan Bay is to the north, Rosse Bay to the east, and Baird Inlet lies to the south.
Princess Marie Bay is an Arctic waterway in Qikiqtaaluk Region, Nunavut, Canada. It is located in Nares Strait by eastern Ellesmere Island, and marks the southwestern edge of Cook Peninsula. It is also south of the Sven Hedin Glacier.
The Glacier Strait is a natural waterway through the Canadian Arctic Archipelago within Qikiqtaaluk Region, Nunavut, Canada. It separates Ellesmere Island from Coburg Island. To the north-east it opens into Baffin Bay, and to the south-west into the Jones Sound.
The Canadian Arctic Rift System is a major North American geological structure extending from the Labrador Sea in the southeast through Davis Strait, Baffin Bay and the Arctic Archipelago in the northwest. It consists of a series of interconnected rifts that formed during the Paleozoic, Mesozoic and Cenozoic eras. Extensional stresses along the entire length of the rift system have resulted in a variety of tectonic features, including grabens, half-grabens, basins and faults.
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