Baffin Island, in the Canadian territory of Nunavut, is the largest island in Canada and the fifth-largest island in the world. Its area is 507,451 km2 (195,928 sq mi)—slightly larger than Spain, its population was 13,039 as of the 2021 Canadian census, and is located at 68°N70°W. It also contains the city of Iqaluit, 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) 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 Arctic Archipelago, also known as the Canadian Arctic Archipelago, is an archipelago lying to the north of the Canadian continental mainland, excluding Greenland.
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 District of Franklin was a regional administrative district of Canada's Northwest Territories. The district consisted of the Canadian high Arctic Islands, notably Ellesmere Island, Baffin Island, and Victoria Island. The district also contained the mainland Melville Peninsula and Boothia Peninsula.
Igloolik is an Inuit hamlet in Foxe Basin, Qikiqtaaluk Region in Nunavut, northern Canada. Because its location on Igloolik Island is close to Melville Peninsula, it is often mistakenly thought to be on the peninsula. The name "Igloolik" means "there is a house here". It derives from iglu, meaning house or building, and refers to the sod houses that were originally in the area, not to snow igloos. In Inuktitut the residents are called Iglulingmiut.
The Qikiqtaaluk Region, Qikiqtani Region or 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 prefer the older term Baffin Region.
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.
Somerset Island is a large, uninhabited island of the Arctic Archipelago, that is part of the Canadian territory of Nunavut. The island is separated from Cornwallis Island and Devon Island to the north by the Parry Channel, from Baffin Island to the east by Prince Regent Inlet, from the Boothia Peninsula to the south by Bellot Strait, and from Prince of Wales Island to the west by Peel Sound. It has an area of 24,786 km2 (9,570 sq mi), making it the 46th largest island in the world and Canada's twelfth largest island.
Southampton Island is a large island at the entrance to Hudson Bay at Foxe Basin. One of the larger members of the 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.
One of the larger members of the Arctic Archipelago, Prince of Wales Island is an Arctic island in Nunavut, Canada, lying between Victoria Island and Somerset Island and south of the Queen Elizabeth Islands.
Amund Ringnes Island is one of the Sverdrup Islands in the Qikiqtaaluk Region, Nunavut, Canada. It is located in the Arctic Ocean, between 78 and 79 degrees of latitude. It lies east of Ellef Ringnes Island, west of Axel Heiberg Island. Hassel Sound separates Amund Ringnes Island from Ellef Ringnes Island. Hendriksen Strait is to the south, as is Cornwall Island. Norwegian Bay is to the east, as is Haig-Thomas Island. To the north lies Peary Channel.
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.
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.
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.
Fury and Hecla Strait is a narrow Arctic seawater channel located in the Qikiqtaaluk Region of Nunavut, Canada.
Prince Alfred Bay is a waterway in Qikiqtaaluk Region, Nunavut, Canada. It lies off the western coast of Devon Island, forming a border of the Grinnell Peninsula, in the eastern high Arctic. Like Pioneer Bay to the south, it is an arm of Wellington Channel.
The geology of Nunavut began to form nearly three billion years ago in the Archean and the territory preserves some of the world's oldest rock units.
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.
