Hall Basin

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Hall Basin, Nunavut, Canada.
Ellesmere Island, Nunavut
Greenland Map indicating Hall Basin, Nunavut, Canada.png
Hall Basin, Nunavut, Canada.
  Ellesmere Island, Nunavut
  Greenland

Hall Basin is an Arctic waterway between Hall Land in Greenland to the west and Canada's northernmost island to the east, Ellesmere Island.

Arctic polar region on the Earths northern hemisphere

The Arctic is a polar region located at the northernmost part of Earth. The Arctic consists of the Arctic Ocean, adjacent seas, and parts of Alaska, Finland, Greenland (Denmark), Iceland, Northern Canada, Norway, Russia and Sweden. Land within the Arctic region has seasonally varying snow and ice cover, with predominantly treeless permafrost -containing tundra. Arctic seas contain seasonal sea ice in many places.

Hall Land

Hall Land is a peninsula in far northwestern Greenland. It is a part of the Northeast Greenland National Park. Hall Land is one of the coldest places in Greenland.

Greenland autonomous country within the Kingdom of Denmark

Greenland is an autonomous constituent country of the Kingdom of Denmark between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. Though physiographically a part of the continent of North America, Greenland has been politically and culturally associated with Europe for more than a millennium. The majority of its residents are Inuit, whose ancestors began migrating from the Canadian mainland in the 13th century, gradually settling across the island.

Contents

Hall Basin is named after American polar explorer Charles Francis Hall.

Charles Francis Hall American explorer of the Arctic

Charles Francis Hall was an American explorer of the Arctic, best known for the suspicious circumstances surrounding his death while leading the American-sponsored Polaris expedition in an attempt to be the first to reach the North Pole. The expedition was marred by insubordination, incompetence, and poor leadership.

Geography

Hall Basin is located in Nares Strait with its entrance between Cape Baird on the eastern coast of Ellesmere Island and Cape Morton on the northwestern coast of Greenland. Robeson Channel is to the north of the basin, and Kennedy Channel to the south. The basin is irregularly shaped, the entrance to Lady Franklin Bay lies on its western shores, being deeply indented by an extensive fjord system. Although the eastern shore is more regular, it includes the Petermann Fjord of the Petermann Glacier at its southern end. [1]

Nares Strait strait

Nares Strait is a waterway between Ellesmere Island and Greenland that connects the northern part of Baffin Bay with the Lincoln Sea. 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.

Cape Morton

Cape Morton is a headland in North Greenland in the Qaasuitsup municipality. The cape is named after Arctic explorer William Morton, who surveyed the Nares Strait area together with Hans Hendrik in June 1854 during the Second Grinnell Expedition.

Robeson Channel strait

Robeson Channel is a body of water lying between Greenland and Canada's northernmost island, Ellesmere Island. It is the most northerly part of Nares Strait, linking Hall Basin to the south with the Arctic Ocean to the north. The Newman Fjord in Greenland has its mouth in the Robeson Channel.

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Baffin Bay A marginal sea between Greenland and Baffin Island, Canada

Baffin Bay, located between Baffin Island and the west coast of Greenland, is a marginal sea of the 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.

Scoresby Sound bay

Scoresby Sund is a large fjord system of the Greenland Sea on the eastern coast of Greenland. It has a tree-like structure, with a main body approximately 110 km (68 mi) long that branches into a system of fjords covering an area of about 38,000 km2 (14,700 sq mi). The longest of the fjords extends 340–350 km inland from the coastline. The depth is 400–600 m in the main basin, but depths increase to up to 1,450 m (4,760 ft) in some fjords. It is one of the largest and longest fjord systems in the world.

Cape Farewell, Greenland cape in Greenland

Cape Farewell is a headland on the southern shore of Egger Island, Nunap Isua Archipelago, Greenland. As the southernmost point of the country, it is one of the important landmarks of Greenland.

Kennedy Channel strait

Kennedy Channel is an Arctic sea passage between Greenland and Canada's most northerly island, Ellesmere Island.

Lincoln Sea A part of the Arctic Ocean from Cape Columbia, Canada, in the west to Cape Morris Jesup, Greenland, in the east

Lincoln Sea is a body of water in the Arctic Ocean, stretching from Cape Columbia, Canada, in the west to Cape Morris Jesup, Greenland, in the east. The northern limit is defined as the great circle line between those two headlands. It is covered with sea ice throughout the year, the thickest sea ice in the Arctic Ocean, which can be up to 15 m (49 ft) thick. Water depths range from 100 m (330 ft) to 300 m (980 ft). Water and ice from Lincoln Sea empty into Robeson Channel, the northernmost part of Nares Strait, most of the time.

Kane Basin bay

Kane Basin is an Arctic waterway lying between Greenland and Canada's northernmost island, Ellesmere Island. It links Smith Sound to Kennedy Channel and forms part of Nares Strait. It is approximately 180 kilometres in length and 130 km at its widest.

Lady Franklin Bay is an Arctic waterway in Qikiqtaaluk Region, Nunavut, Canada. The bay is located in Nares Strait and is an inlet into the northeastern shore of Ellesmere Island.

Petermann Glacier glacier in Greenland

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.

Skjoldungen large uninhabited island in the King Frederick VI Coast, southeastern Greenland

Skjoldungen is a large uninhabited island in the King Frederick VI Coast, southeastern Greenland. Administratively it is part of the Sermersooq municipality. The weather of the island is characterized by tundra climate.

Bernstorff Fjord

Bernstorff Fjord is a fjord in King Frederick VI Coast, eastern Greenland.

Sam Ford Fiord

Sam Ford Fiord is an isolated, elongated Arctic fjord on Baffin Island's northeastern coast in the Qikiqtaaluk Region of Nunavut, Canada. The Inuit settlement of Pond Inlet is 320 km (200 mi) to the northwest and Clyde River is 80 km (50 mi) to the east.

Igutsaat Fjord

Igutsaat Fjord, also known as Igutsait Fjord, is a fjord in the King Frederick VI Coast, Kujalleq municipality, southern Greenland.

Odinland

Odinland, also Odinsland in the Defense Mapping Agency Greenland Navigation charts, is a peninsula in the King Frederick VI Coast, southeastern Greenland. It is a part of the Sermersooq municipality.

Newman Bay

Newman Bay or Newman Fjord is a fjord in northern Greenland. To the northwest, the fjord opens into the Robeson Channel of the Lincoln Sea. It is a part of the Northeast Greenland National Park.

Bessel Fjord, NW Greenland fjord in Greenland

Bessel Fjord, also known as Bessels Bay, is a fjord in northwestern Greenland. Administratively it belongs to the Avannaata municipality.

Joe Island (Greenland) island in Greenland

Joe Island is an island of the Nares Strait, Greenland. Administratively it belongs to the Avannaata municipality.

Petermann Fjord

Petermann Fjord is a fjord in northwestern Greenland. Administratively it marks the boundary between the Avannaata municipality and the Northeast Greenland National Park.

References

  1. Prostar Sailing Directions 2005 Greenland and Iceland Enroute, p. 93

Coordinates: 81°30′N63°30′W / 81.500°N 63.500°W / 81.500; -63.500 (Hall Basin)

Geographic coordinate system Coordinate system

A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.