Baird Peninsula is a peninsula in west central Baffin Island in the Qikiqtaaluk Region of Nunavut, Canada. It juts into the Foxe Basin past Longstaff Bluff. Prince Charles Island lies to the south. [1]
It is named in honor of the Scottish explorer and glaciologist Colonel Patrick Douglas Baird (1913–1984). [2]
Baffin Island, in the Canadian territory of Nunavut, is the largest island in Canada, the second-largest island in the Americas, and the fifth-largest island in the world. Its area is 507,451 km2 (195,928 sq mi) with a population density of 0.03/km2; the population was 13,039 according to the 2021 Canadian census; and it is located at 68°N70°W. It also contains the city of Iqaluit, which is the capital of Nunavut.
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)1 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 between two settlements, the larger of which is Cambridge Bay (Nunavut) and the other Ulukhaktok.
The Arctic Archipelago, also known as the Canadian Arctic Archipelago, is an archipelago lying to the north of the Canadian continental mainland, excluding Greenland and Iceland.
Kitikmeot Region is an administrative region of Nunavut, Canada. It consists of the southern and eastern parts of Victoria Island with the adjacent part of the mainland as far as the Boothia Peninsula, together with King William Island and the southern portion of Prince of Wales Island. The regional centre is Cambridge Bay.
Melville Peninsula is a large peninsula in the Canadian Arctic north of Hudson Bay. To the east is Foxe Basin and to the west the Gulf of Boothia. To the north the Fury and Hecla Strait separates it from Baffin Island. To the south Repulse Bay and Frozen Strait separate it from Southampton Island at the north end of Hudson Bay. On the southwest it is connected to the mainland by the Rae Isthmus, named after the Arctic explorer John Rae.
Cumberland Peninsula is a peninsula in the southeastern part of Baffin Island in Nunavut, Canada. It is located between 64°56' and 67°57' north latitude, and 61°56' to 68° west longitude. The Arctic Circle crosses the peninsula, with the Labrador Sea to the southeast, and the Davis Strait to the east, which lies between the peninsula and Greenland. The Cumberland Sound lies to the southwest, separating the Cumberland Peninsula from the Hall Peninsula, which is also part of Baffin Island.
The Hall Peninsula is a peninsula on the southern end of Baffin Island, in Nunavut, Canada. It lies between Frobisher Bay on the west, and the Cumberland Sound on the east between 62°40'N and 65°10'W. The Hall Peninsula is part of the Arctic Tundra biome—the world's coldest and driest biome. The Blunt Peninsula extends off the southeastern part of the Hall Peninsula.
The Gulf of Boothia is a body of water in Nunavut, Canada. Administratively it is divided between the Kitikmeot Region on the west and the Qikiqtaaluk Region on the east. It merges north into Prince Regent Inlet, the two forming a single bay with different names for its parts. It is surrounded by, clockwise, Baffin Island, Fury and Hecla Strait, the Melville Peninsula, the Canadian mainland, and the Boothia Peninsula. The south end is Committee Bay, northwest of which are the Simpson Peninsula and Pelly Bay. On the west side of the gulf at 70°18′N91°42′W, north of Pelly Bay and Thom Bay, is Eden Bay, which should not be confused with a bay of the same name in the Qikiqtaaluk Region.
Prince Regent Inlet is a body of water in Nunavut, Canada between the west end of Baffin Island and Somerset Island on the west. It opens north into Lancaster Sound and to the south merges into the Gulf of Boothia. The Arctic inlet's northern portion is approximately 40 mi (64 km) wide; the southern portion is approximately 65 mi (105 km) wide. It is deep throughout and there are no islands within the inlet.
The Brodeur Peninsula is an uninhabited headland on Baffin Island in the Qikiqtaaluk Region of Nunavut, Canada. It is located in the northwestern part of the island and is bounded by Prince Regent Inlet to the west, Lancaster Sound to the north, and Admiralty Inlet to the east. The peninsula is connected to the rest of Baffin Island by a narrow isthmus to the south.
Grinnell Peninsula is a peninsula of northwestern Devon Island in Nunavut, Canada.
The Bravo Lake Formation is a mafic volcanic belt and large igneous province located at the northern margin of the Trans-Hudson orogeny on central Baffin Island, Nunavut, Canada. It is exposed along a nearly continuous east–west passage for 120 km (75 mi) and changes in stratigraphic thickness from 1 to 2.5 kilometers. The formation is a rare alkaline-suite that formed as a result of submarine rifting during the Paleoproterozoic period. The Bravo Lake Formation is surprisingly undeformed by the Himalayan-scale forming event during the Trans-Hudsonian orogeny.
The Parry Channel is a natural waterway through the central Canadian Arctic Archipelago. Its eastern two-thirds lie 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.
Wiswell Inlet is a body of water in Nunavut's Qikiqtaaluk Region in Canada. It lies in eastern Frobisher Bay, forming a wedge into Baffin Island's Blunt Peninsula. There are several islands at the mouth of the inlet.
Moffet Inlet is a body of water in Nunavut's Qikiqtaaluk Region. It lies on the eastern side of Admiralty Inlet on Baffin Island's Borden Peninsula. The Inuit hamlet of Arctic Bay is located 105 km south/southeast of the inlet.
The Henry Kater Peninsula is a peninsula on northern Baffin Island, in Nunavut, Canada. It protrudes in an eastern direction into Davis Strait. It's bounded to the north by Arctic Harbour. Further north lies Clyde Inlet. Home Bay borders the peninsula to the south.
The Lindstrom Peninsula is located on the southern coast of Ellesmere Island, a part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. Across Baffin Bay to the south lies Devon Island. Harbour Fiord and Landslip Island are to the west, while the Grise Fiord is to the east. The highest peak on the peninsula is Mount Aqiatushuk 76°25′40″N083°15′00″W.
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.
Bowman Bay is an Arctic waterway in the Qikiqtaaluk Region, Nunavut, Canada. It is located in the Foxe Basin by northeastern Foxe Peninsula off Baffin Island. The nearest community is Kinngait, situated 204 km (127 mi) to the south, while Nuwata, a former settlement, is situated 188 km (117 mi) to the west near Finnie Bay.
Patrick Douglas Baird was a Scottish glaciologist who worked in the Canadian Arctic.
68°55′N076°00′W / 68.917°N 76.000°W
 | This Qikiqtaaluk Region, Nunavut location article is a stub. You can help Wikipedia by expanding it. |
 | This article related to an island or group of islands in Canada is a stub. You can help Wikipedia by expanding it. |