| Goose Fiord Formation | |
|---|---|
  | |
| Location | Nunavut, Canada |
| Coordinates | 76°36′N88°30′W / 76.6°N 88.5°W Coordinates: 76°36′N88°30′W / 76.6°N 88.5°W |
| Depth | 308 metres (1,010 ft) |
| Geology | Formation |
| Age | Silurian/Devonian |
The Goose Fiord Formation is a geologic formation in Nunavut, Canada. It preserves fossils that date back to the Silurian period. It is located on the southern portion of the Ellesmere Island in Canada. It also lies on the northern portion of Devon Island.
The depth of the fiord reaches nearly 308 meters. The fiord is composed largely of dolomite, whose density peaks inside the bottom 60 meters. The other major component of the fiord is siltstone.
The fiord is exposed along the Schei Syncline, which is on the southern portion of the island. The fiord cannot be seen from the northern portion of Ellesmere Island. It remains on top of the Devon Island Formation, and the Blue Fiord Formation overlies the Goose Formation.
Ellesmere Island is part of the Qikiqtaaluk Region in the Canadian territory of Nunavut. Lying within the Arctic Archipelago, it is considered part of the Queen Elizabeth Islands, with Cape Columbia being the most northerly point of land in Canada.. It comprises an area of 196,235 km2 (75,767 sq mi) and the total length of the island is 830 km (520 mi), making it the world's tenth largest island and Canada's third largest island. The Arctic Cordillera mountain system covers much of Ellesmere Island, making it the most mountainous in the Arctic Archipelago. The Arctic willow is the only woody species to grow on Ellesmere Island.
Grise Fiord is an Inuit hamlet on the southern tip of Ellesmere Island, in the Qikiqtaaluk Region in the territory of Nunavut, Canada. It is one of three settlements on the island; despite its low population, it is the largest community on Ellesmere Island. The settlement at Grise Fiord, created by the Canadian Government in 1953 through a forced relocation of Inuit families from Inukjuak, Quebec, is the northernmost public community in Canada. It is also one of the coldest inhabited places in the world, with an average yearly temperature of −16.5 °C (2.3 °F).
Quttinirpaaq National Park is a Canadian national park. Located on the northeastern corner of Ellesmere Island in the Qikiqtaaluk Region of Nunavut, the most northerly extent of Canada, it is the second most northerly park on Earth after Northeast Greenland National Park. In Inuktitut, Quttinirpaaq means "top of the world". It was established as Ellesmere Island National Park Reserve in 1988, and the name was changed to Quttinirpaaq in 1999, when Nunavut was created, and became a national park in 2000. The reserve covers 37,775 km2 (14,585 sq mi), making it the second largest park in Canada, after Wood Buffalo National Park.
The Qikiqtaaluk Region, Qikiqtani Region or Baffin Region is the easternmost 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.
Jones Sound is a waterway in Qikiqtaaluk, Nunavut, Canada. It lies between Devon Island and the southern end of Ellesmere Island. At its northwestern end it is linked by several channels to Norwegian Bay; at its eastern end it opens via Glacier Strait into Baffin Bay. The hamlet of Grise Fiord was established on the south shore Ellesmere Island in 1953, partly to assert Canadian sovereignty in the high Arctic.
The Canadian territory of Nunavut covers about 1.9 million square kilometres of land and water including part of the mainland, most of the Arctic Islands, and all of the islands in Hudson Bay, James Bay, and Ungava Bay which belonged to the Northwest Territories. This makes it the fifth largest country subdivision in the world. If Nunavut were a country, it would rank 13th in area, after the Democratic Republic of the Congo. Nunavut has land borders with Manitoba, the Northwest Territories on several islands as well as the mainland, and a tiny land border with Newfoundland and Labrador on Killiniq Island.
The Arctic Cordillera is a terrestrial ecozone in northern Canada characterized by a vast, deeply dissected chain of mountain ranges extending along the northeastern flank of the Canadian Arctic Archipelago from Ellesmere Island to the northeasternmost part of the Labrador Peninsula in northern Labrador and northern Quebec, Canada. It spans most of the eastern coast of Nunavut with high glaciated peaks rising through ice fields and some of Canada's largest ice caps, including the Penny Ice Cap on Baffin Island. It is bounded to the east by Baffin Bay, Davis Strait and the Labrador Sea while its northern portion is bounded by the Arctic Ocean.
The Ellesmere Island Volcanics are a Late Cretaceous volcanic group of volcanoes and lava flows in the Qikiqtaaluk Region of northern Ellesmere Island, Nunavut, Canada.
The Strand Fiord Formation is a Late Cretaceous volcanic component, located on northwestern and west-central Axel Heiberg Island, Nunavut, Canada. The formation contains flood basalts which are found on western Axel Heiberg Island at Dragon Cliffs 300 m (984 ft) tall.
The Conger Range, also called the Conger Mountains, is a mountain range in Quttinirpaaq National Park on Ellesmere Island, Nunavut, Canada, beginning about 16 km (10 mi) west of Mount Osborne. It is part of the Arctic Cordillera which is a vast dissected mountain system extending from Ellesmere Island to the northernmost tip of Labrador and northeastern Quebec. The Conger Range is a structural extension of the Garfield Range and continues into the highlands north of the head of Hare Fiord. The overall extent of the range is about 180 km (112 mi). Most of its peaks are ice-covered, although nearly all of the southern slopes are ice-free. Many of the valleys between the peaks are filled with glacial tongues spilling out to the south from the Grand Land Ice Cap. Its highest point is Mount Biederbick at 1,542 m (5,059 ft).
The uninhabited Marvin Islands are located in the Arctic Ocean across the mouth of Disraeli Fiord, in northern Ellesmere Island within the Quttinirpaaq National Park. Ward Hunt Island lies to the northwest. The island group is a part of the Qikiqtaaluk Region Nunavut, Canada.
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 Sverdrup Basin Magmatic Province is a large igneous province located on Axel Heiberg Island and Ellesmere Island, Nunavut, Canada near the rifted margin of the Arctic Ocean at the end of Alpha Ridge.
Brae Bay is an Arctic waterway in the Qikiqtaaluk Region, Nunavut, Canada. It is located in Baffin Bay by northern Devon Island. Directly to the north is the Inuit community of Grise Fiord on Ellesmere Island.
The Bjorne Formation is a formation of sandstones and shales in the Canadian Arctic Archipelago. The southern edge of the formation includes petroleum reserves in Melville Island. The basin also includes Mackenzie King Island, Lougheed Island and portions of Prince Patrick Island, Borden Island, Ellef Ringnes Island, Amund Ringnes Island, and Cornwall Island.
Tanquary Fiord is a fjord on the north coast of the Arctic Archipelago's Ellesmere Island, Nunavut, Canada. It is located in the Quttinirpaaq National Park and extends 30 mi (48 km) in a north-westerly direction from Greely Fiord.
Strathcona Fiord is a fiord on the west central coast of Ellesmere Island, the most northern island within the Arctic Archipelago, Nunavut, Canada.
The Assistance Formation is a geologic formation located on Devon Island and Ellesmere Island in Nunavut. It preserves fossils dating back to the Permian period. The formation rides along the southeastern edges of the Sverdrup Basin, as well as on Melville Island and Grinnell Peninsula
The Devon Island Formation is a geologic formation in the Canadian Arctic. It preserves fossils dating back to the late Silurian and Devonian periods.
The "Cape Rawson Formation" is a geologic formation in Nunavut. It preserves fossils that date back to both the Ordovician and Devonian periods. Because the Blue Fiord Formation lies on top of the formation, it has been determined that it predates the middle Devonian Period. It is located on the southern portion of the Ellesmere Island in Canada.