Fishtrap Cove

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Fishtrap Cove ( 68°11′S67°0′W / 68.183°S 67.000°W / -68.183; -67.000 Coordinates: 68°11′S67°0′W / 68.183°S 67.000°W / -68.183; -67.000 ) is a small cove 0.1 nautical miles (0.2 km) northwest of Boulder Point on the southwest side of Stonington Island, close off the west coast of Graham Land, Antarctica. It was first surveyed by the United States Antarctic Service, 1939–41, and resurveyed in 1946–47 by the Falkland Islands Dependencies Survey (FIDS), who so named it because FIDS parties used this cove for setting fish traps. [1]

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.

Cove A small sheltered bay or coastal inlet

A cove is a small type of bay or coastal inlet. Coves usually have narrow, restricted entrances, are often circular or oval, and are often situated within a larger bay. Small, narrow, sheltered bays, inlets, creeks, or recesses in a coast are often considered coves.

Boulder Point is the southern extremity of Stonington Island, close off the west coast of Graham Land. It was first surveyed in 1940 by the United States Antarctic Service. Upon being resurveyed in 1948 by the Falkland Islands Dependencies Survey it was named for its prominent granite boulder.

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Anemometer Hill is a hill 25 metres (80 ft) high northeast of Fishtrap Cove on Stonington Island, in Marguerite Bay, Antarctica. It was surveyed by the East Base party of the U.S. Antarctic Service, 1939–41, which built its base on this island, and so named by the United Kingdom Antarctic Place-Names Committee because the hill was the site of an anemometer in 1961.

Chinstrap Cove bay

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Flagpole Point is a point 0.2 nautical miles (0.4 km) northwest of Fishtrap Cove, forming the southern part of the western extremity of Stonington Island, close off the west coast of Graham Land, Antarctica. It was first surveyed by the United States Antarctic Service (USAS), 1939–41, whose East Base was located on this island. It was resurveyed in 1946–47 by the Falkland Islands Dependencies Survey, and so named by them because of the flagpole which was erected by the USAS on a rocky knoll close northeast of this point.

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Gaul Cove

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Haulaway Point is a small rocky point midway along the northeast side of Stonington Island, close off the west coast of Graham Land, Antarctica. It was first surveyed by the United States Antarctic Service, 1939–41. It was resurveyed in 1946–47 by the Falkland Islands Dependencies Survey, who so named the point because it is one of the best places for hauling stores ashore.

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Sally Cove cove

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Sorge Island is an island lying just south of The Gullet in Barlas Channel, close east of Adelaide Island. Mapped by Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1948-59. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Ernst F.W. Sorge, German glaciologist who made the first seismic soundings of the Greenland ice sheet, 1929–31, and developed a theory of the densification of firn.

Somigliana Glacier is a glacier flowing north to Langmuir Cove on the north part of Arrowsmith Peninsula in Graham Land. Mapped by Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1956-59. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Carlo Somigliana, Italian mathematician and physicist who originated a viscous theory of glacier flow, in 1921.

Relay Hills is a group of low, ice-covered hills, mainly conical in shape, between Mount Edgell and Kinnear Mountains in western Antarctic Peninsula. First roughly surveyed from the ground by British Graham Land Expedition (BGLE), 1936-37. Photographed from the air by Ronne Antarctic Research Expedition (RARE), November 1947. Resurveyed by Falkland Islands Dependencies Survey (FIDS), November 1958. The name, applied by the United Kingdom Antarctic Place-Names Committee (UK-APC), arose because both the BGLE and the FIDS sledging parties had to relay their loads through this area to the head of Prospect Glacier.

Back Bay is a bay 1 km (0.6 mi) wide along the west coast of Graham Land, Antarctica. Its entrance lies between Stonington Island and Fitzroy Island, with the head of the bay formed by Northeast Glacier. The bay was first surveyed by the US Antarctic Service, 1939–41, and so named by them because of its location at the rear (north-east) side of Stonington Island.

References

PD-icon.svg This article incorporates  public domain material from the United States Geological Survey document "Fishtrap Cove" (content from the Geographic Names Information System ).

United States Geological Survey Scientific agency of the United States government

The United States Geological Survey is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization has four major science disciplines, concerning biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility.

Geographic Names Information System geographical database

The Geographic Names Information System (GNIS) is a database that contains name and locative information about more than two million physical and cultural features located throughout the United States of America and its territories. It is a type of gazetteer. GNIS was developed by the United States Geological Survey in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names.