| Foulk Fjord | |
|---|---|
  Foulk Fjord Location in Greenland | |
| Location | Arctic |
| Coordinates | 78°18′N72°35′W / 78.300°N 72.583°W Coordinates: 78°18′N72°35′W / 78.300°N 72.583°W |
| Ocean/sea sources | Baffin Bay |
| Basin countries | Greenland |
| Max. length | 50 km (31 mi) |
| Max. width | 1.5 miles (2.4 km) |
Foulk Fjord is a fjord in the Qaasuitsup municipality in northwestern Greenland.
Located near Reindeer Point, the fjord is about 1.5 miles (2.4 km) wide and several miles long with 2,000 ft (610 m) cliffs on each side. Brother John's Glacier terminates at the eastern end of the fjord. At the foot of the glacier is Lake Alida, a small body of frozen fresh water. The northern end of Baffin Bay west of the former village of Etah, narrows into Nares Strait between Greenland and Ellesmere Island, and is usually frozen from October to July. Given the harsh climate, the growing season in the fjord is limited to about six to eight weeks. [1]
The area lies on the ancient migration route from the north of the Canadian Arctic, with several waves of ancient migrants passing through the area, from the northbound Independence I and Independence II cultures 4,400 and 2,700 years ago, respectively, to the southbound Thule culture migrants a thousand years ago. It is also the point where the last migration of the Inuit from Baffin Island reached the coast of Greenland in 1865. [2] An Inuit shaman named Qidlaq led the migrants from Baffin Island alongside the coast of Ellesmere Island for seven years, crossing the strait and fjord to Etah. The group split there, with some returning to Pond Inlet in Canada at a cost of many lives. Inhabitants of Pituffik, later relocated to Qaanaaq, are partially descended from this last group of Arctic migrants to Greenland. [2]
Greenland is located between the Arctic Ocean and the North Atlantic Ocean, northeast of Canada and northwest of Iceland. The territory comprises the island of Greenland—the largest island in the world—and more than a hundred other smaller islands. As an island, Greenland has no land boundaries and 44,087 km of coastline. A sparse population is confined to small settlements along certain sectors of the coast. Greenland possesses the world's second largest ice sheet.
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.
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) and its population was 13,148 as of the 2016 Canadian Census. It is located in the region of 70° N and 75° W.
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 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.
The first USS Advance was a brigantine in the United States Navy which participated in an arctic rescue expedition. Advance was built in 1847 as Augusta in New Kent County, Virginia and loaned to the Navy on 7 May 1850 by Mr. Henry Grinnell to participate in the search for Sir John Franklin's arctic expedition which had been stranded in the frozen north since 1846. After last-minute preparations, the ship, under the command of Lieutenant Edwin J. De Haven and in company with Rescue, put to sea from New York on 23 May 1850.
Nares Strait is a waterway between Ellesmere Island and Greenland that connects the northern part of Baffin Bay in the Atlantic Ocean with the Lincoln Sea in the Arctic Ocean. From south to north, the strait includes Smith Sound, Kane Basin, Kennedy Channel, Hall Basin and Robeson Channel. During 1962–64, a 20 km (12 mi) by 10 km (6.2 mi) ice island drifted southward from the Lincoln Sea through the Nares and Davis Straits to the Atlantic Ocean. Nares strait has a nearly permanent current from the north, powered by the Beaufort Gyre, making it harder to traverse for ships coming from the south.
Uummannaq Fjord is a large fjord system in the northern part of western Greenland, the largest after Kangertittivaq fjord in eastern Greenland. It has a roughly south-east to west-north-west orientation, emptying into the Baffin Bay in the northwest.
Cape York is a cape on the northwestern coast of Greenland, in northern Baffin Bay.
Smith Sound is an uninhabited Arctic sea passage between Greenland and Canada's northernmost island, Ellesmere Island. It links Baffin Bay with Kane Basin and forms part of the Nares Strait.
The history of Nunavut covers the period from the arrival of the Paleo-Eskimo thousands of years ago to present day. Prior to the colonization of the continent by Europeans, the lands encompassing present-day Nunavut were inhabited by several historical cultural groups, including the Pre-Dorset, the Dorsets, the Thue and their descendants, the Inuit.
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.
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.
The MacGregor Arctic Expedition was a privately funded expedition which set out to reoccupy Fort Conger, Ellesmere Island, Canada, a site within flying distance of the North Pole. The expedition, which took place from July 1, 1937, to October 3, 1938, had four main objectives: To collect weather data; to make a magnetic survey; to photograph the aurora borealis and study its effects upon radio transmission; and to explore the area northwest of Ellesmere Island, in order to clear up the questions about Crocker Land, which Robert Peary placed on the map more than 30 years earlier.
The Baffin Mountains are a mountain range running along the northeastern coast of Baffin Island and Bylot Island, Nunavut are part of the Arctic Cordillera. The ice-capped mountains are some of the highest peaks of eastern North America, reaching a height of 1,525–2,146 metres (5,003–7,041 ft) above sea level. While they could be considered a single mountain range as they are separated by bodies of water to make Baffin Island, this is not true, as they are closely related to the other mountain ranges that make the much larger Arctic Cordillera mountain range.
The Pre-Dorset is a loosely defined term for a Paleo-Eskimo culture or group of cultures that existed in the Eastern Canadian Arctic from c. 3200 to 850 cal BC, and preceded the Dorset culture.
Petermann Glacier is a large glacier located in North-West Greenland to the east of Nares Strait. It connects the Greenland ice sheet to the Arctic Ocean at 81°10' north latitude, near Hans Island.
David Haig-Thomas was a British ornithologist, explorer and rower who competed for Great Britain in the 1932 Summer Olympics. He was an army commando during the Second World War, and was killed in action during the Normandy Landings. Haig-Thomas Island in the Canadian Arctic is named after him.
Upernavik Archipelago is a vast coastal archipelago in the Avannaata municipality in northwestern Greenland, off the shores of northeastern Baffin Bay. The archipelago extends from the northwestern coast of Sigguup Nunaa peninsula in the south at approximately 71°50′N56°00′W to the southern end of Melville Bay in the north at approximately 74°50′N57°30′W.
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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