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).
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.
Baker Lake is a hamlet in the Kivalliq Region, in Nunavut on mainland Canada. Located 320 km (200 mi) inland from Hudson Bay, it is near the nation's geographical centre, and is notable for being Nunavut's sole inland community. The hamlet is located at the mouth of the Thelon River on the shore of Baker Lake. The community was given its English name in 1761 from Captain William Christopher who named it after Sir William Baker, the 11th Governor of the Hudson's Bay Company.
Bathurst Inlet,, is a small Inuit community located in Bathurst Inlet in the Kitikmeot Region of Nunavut, Canada. As of the 2016 census the population remained at zero.
Ennadai Lake is a lake in Kivalliq Region, Nunavut, Canada. It is 52 mi (84 km) long, and 3 to 14 mi wide. It is drained to the north by the Kazan River. A 615 km section of the Kazan River from the outlet of Ennadai Lake to Baker Lake, was designated as a part of the Canadian Heritage Rivers System in 1990.
The Kazan River, is a Canadian Heritage River located in Nunavut, Canada. The Dene name for the river was Kasba-tue meaning "white partridge river." The name was apparently changed to Kazan in the late 19th century due to the influence of Order of Mary Immaculate missionaries. The river headwaters are in northern Saskatchewan at Kasba Lake, and it flows north for about 1000 km (621 mi) before emptying into Baker Lake, on the opposite side of the mouth of the Thelon River. Along its course the river flows through several lakes, including Ennadai Lake and Yathkyed Lake, over the Kazan Falls, down a red sandstone gorge and through both boreal forest and tundra. It is the last section of the river, below Ennadai Lake, that is above the timber line and is designated a Canadian Heritage River.
The Churchill Craton is the northwest section of the Canadian Shield and stretches from southern Saskatchewan and Alberta to northern Nunavut. It has a very complex geological history punctuated by at least seven distinct regional tectonometamorphic intervals, including many discrete accretionary magmatic events. The Western Churchill province is the part of the Churchill Craton that is exposed north and west of the Hudson Bay. The Archean Western Churchill province contributes to the complicated and protracted tectonic history of the craton and marks a major change in the behaviour of the Churchill Craton with many remnants of Archean supracrustal and granitoid rocks.
The Burnside River is a river in the Canadian territory of Nunavut. It has its headwaters at Contwoyto Lake, flows across the Precambrian Shield's Contwoyto Plateau, flows through isolated and rugged tundra, into Lake Kathawachaga, and through the Wilberforce Hills region. Before emptying into Bathurst Inlet on the Arctic Ocean, the Mara River empties into the Burnside River. The river has an island, Nadlak, historically notable for Inuit use of caribou antlers as hut roof infrastructures.
Dubawnt Lake is a lake in the Kivalliq Region, Nunavut, Canada. It is 3,630 km2 (1,400 sq mi) in size and has several islands. It is about 320 km (200 mi) north of the Four Corners, about 480 km (300 mi) west of Hudson Bay and about 400 km (250 mi) south of the Arctic Circle. To the northwest is the Thelon Wildlife Sanctuary. Its main inlet and outlet is the north-flowing Dubawnt River which joins the Thelon River at Beverly Lake. The Thelon flows east to Hudson Bay at Chesterfield Inlet. It is on the line of contact between the Sayisi Dene band of Eastern Caribou-Eater Chipewyan people and the Harvaqtuurmiut and Ihalmiut bands of Caribou Inuit. The first recorded European to reach the lake was Samuel Hearne in 1770, but it remained largely unknown to outsiders until it was explored by Joseph Tyrrell in 1893. There are no permanent settlements but there are fly-in fish camps where large lake trout can be caught during the two month ice-free season.
Amadjuak Lake is a lake in the Qikiqtaaluk Region, Nunavut, Canada. Along with Nettilling Lake, it is located in south-central Baffin Island's Great Plain of the Koukdjuak. It is 154 km (96 mi) south of Burwash Bay. The closest community is Iqaluit.
Caribou Inuit, barren-ground caribou hunters, are bands of inland Inuit who lived west of Hudson Bay in Keewatin Region, Northwest Territories, now the Kivalliq Region of present-day Nunavut between 61° and 65° N and 90° and 102° W in Northern Canada. They were originally named "Caribou Eskimo" by the Danish Fifth Thule Expedition of 1921–1924 led by Knud Rasmussen. Caribou Inuit are the southernmost subgroup of the Central Inuit.
Kaminak Lake is a lake in Kivalliq Region, Nunavut, Canada. The sub-Arctic lake is one of eleven lakes of the Ferguson River system which ultimately flow into the northwestern Hudson Bay. The abandoned outpost of Tavani is 60 mi (97 km) to the east.
Tahiryuaq, formerly Ferguson Lake, is located on southern Victoria Island in the Kitikmeot Region of Nunavut, in northern Canada. It drains westward into Iqaluktuuq which is a segment of the Ekalluk River, 5 mi (8.0 km) from the northeastern side of Wellington Bay (Ekaloktok), on Dease Strait, Arctic Ocean Ferguson Lake was the namesake of Constable Ferguson, a Royal Canadian Mounted Police member, but is now known by the original name of Tahiryuaq
Ferguson Lake is a lake in Kivalliq Region, Nunavut, Canada. It is located 150 km (93 mi) north of the tree line, midway between Yathkyed Lake and Qamanirjuaq Lake. The lake's outflow is to the east into the Ferguson River, which flows eastward through several lakes, emptying into northwestern Hudson Bay between Rankin Inlet and Whale Cove. The closest community is Baker Lake, 160 km (99 mi) to the north.
The Ferguson River originates on the eastern bank of Ferguson Lake within the northern Hearne Domain, Western Churchill province of the Churchill craton, the northwest section of the Canadian Shield in Nunavut's Kivalliq Region.
Garry Lake is a lake in sub-Arctic Kivalliq Region, Nunavut, Canada. As a portion of the Back River waterway, Garry Lake originates directly east of Lake Pelly and drains to the east by the Back River. A set of rapids separate Buliard Lake from Garry Lake. Two other sets of rapids separate Garry Lake's three sections which are also differentiated by elevation. Garry Lakes are isolated from nearby communities.
There are several ways of determining the centre of Canada giving different locations.
Mary River is located on Baffin Island in the Qikiqtaaluk Region of Nunavut, about 936 km (582 mi) northwest of the capital, Iqaluit, and about 176 km (109 mi) southwest of Pond Inlet Inuktitut: Mittimatalik, lit. 'the place where the landing place is' The Inuit, name for the Mary River mountain is Nuluyait, meaning buttocks. There is a 4,000 year history in the area. For hundreds of years the semi-nomadic Inuit from the region that includes the hamlets of Pond Inlet and Igloolik, met at Mary River during the summer hunting caribou. By 2011, the population of the region was about 5,400 people, many of whom continued the traditional hunting and fishing lifestyle living off the land.
The Ekalluk River is a river in the Kitikmeot Region, Nunavut, Canada. It is located in central through southeastern Victoria Island. Its source is Tahiryuaq, and it flows west to Wellington Bay and east to Albert Edward Bay. Nearby lakes include Keyhole Lake, Kitigaq, and Surrey Lake. The closest community is Cambridge Bay.
