Henry Ice Rise

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Henry Ice Rise is a triangular-shaped ice rise about 70 miles (110 km) long located between Korff Ice Rise and the southern portion of Berkner Island in the Ronne Ice Shelf, Antarctica. It was first visited by the United States International Geophysical Year geophysical traverse party from Ellsworth Station, 1957–58, and was named by the Advisory Committee on Antarctic Names after Captain Clifford D. Henry of the Military Sealift Command, a veteran American polar sea captain and master of USNS Private John R. Towle (T-AK-240). Henry died aboard his ship, February 16, 1975, while returning from his fourteenth voyage to Antarctica in support of the U.S. Antarctic Research Program. [1]

Ice rise an elevation of the otherwise totally flat ice shelf

An ice rise is a clearly defined elevation of the otherwise totally flat ice shelf, typically dome-shaped and rising 100 to 200 metres above the surrounding ice shelf. An ice rise forms where the ice shelf touches the rocky seabed because of an elevation in the seabed that remains below sea level.. The ice shelf flows over the seabed elevation, completely covering it with ice, thereby forming an ice rise. The resulting tension forms crevasses around the ice rise.

Korff Ice Rise is an ice rise, 80 nautical miles (150 km) long and 20 nautical miles (40 km) wide, lying 50 nautical miles (90 km) east-northeast of Skytrain Ice Rise in the southwestern part of the Ronne Ice Shelf, Antarctica. It was discovered by the US–IGY Ellsworth Traverse Party, 1957–58, and named by the party for Professor Serge A. Korff, vice chairman of the cosmic ray technical panel, U.S. National Committee for the International Geophysical Year, 1957–59.

Berkner Island Ice rise in the British Antarctic Territory, Antarctica

Berkner Island is an Antarctic ice rise, where bedrock below sea level has caused the surrounding ice sheet to create a dome. If the ice cap were removed, the island would be under water. Berkner "Island" is high and completely ice-covered and about 320 kilometres (200 mi) long and 150 kilometres (93 mi) wide, with an area of 44,000 km2 (17,000 sq mi). It is surrounded by the Filchner-Ronne Ice Shelf. The northernmost point of the Berkner is about 20 kilometres (12 mi) from the open sea. It lies in the overlapping portion of the Argentine and the British Antarctic territorial claims.

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Marie Byrd Land geographic region

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Fowler Ice Rise is a very large Antarctic ice rise between Evans Ice Stream and Carlson Inlet, in the southwest part of the Ronne Ice Shelf. The feature appears to be completely ice-covered except for the Haag Nunataks, which protrude above the surface in the northwestern portion. It was mapped by the United States Geological Survey from Landsat imagery taken 1973–74, and named by the Advisory Committee on Antarctic Names for Captain Alfred N. Fowler, U.S. Navy, Commander of the U.S. Naval Support Force, Antarctica, 1972–74.

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Ives Ice Rise is an ice rise about 1 mile (1.6 km) long at the head of Weber Inlet, an ice-filled inlet situated between Bennett Dome and Berlioz Point on the Beethoven Peninsula, situated in the southwest part of Alexander Island, Antarctica. It was mapped by the United States Geological Survey from U.S. Navy aerial photographs taken 1967–68 and Landsat imagery taken 1972–73. In association with the names of composers grouped in this area, it was named by the Advisory Committee on Antarctic Names after Charles Ives, the American composer.

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Moon Bay

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Echelmeyer Ice Stream

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Jutulstraumen Glacier is a large glacier in Queen Maud Land, Antarctica, about 120 nautical miles (220 km) long, draining northward to the Fimbul Ice Shelf between the Kirwan Escarpment, Borg Massif and Ahlmann Ridge on the west and the Sverdrup Mountains on the east. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian–British–Swedish Antarctic Expedition (1949–52) and air photos by the Norwegian expedition (1958–59) and named Jutulstraumen. More specifically jutulen are troll-like figures from Norwegian folk tales. The ice stream reaches speeds of around 4 metres per day near the coast where it is heavily crevassed.

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Bagshawe Glacier glacier in Antarctica

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Dickey Glacier is a glacier 12 nautical miles (22 km) long, flowing north along the east side of the Surveyors Range to enter Beaumont Bay, Ross Ice Shelf. It was named by the Advisory Committee on Antarctic Names for Captain Willie M. Dickey, U.S. Navy, commander of the Naval Support Units, Antarctica, at Little America V in winter 1957.

Doake Ice Rumples is an area of disturbed ice in the Ronne Ice Shelf, extending for about 55 nautical miles (100 km) in a northwest–southeast direction between Korff Ice Rise and Henry Ice Rise. It was first visited and mapped in part by the US–International Geophysical Year geophysical traverse party from Ellsworth Station 1957–58, led by Edward Thiel, and was further delineated from U.S. Landsat imagery taken 1974 and from radio echo sounding by the British Antarctic Survey (BAS) in 1981. It was named by the UK Antarctic Place-Names Committee after Christopher S.M. Doake, a senior BAS glaciologist from 1973, who has contributed to an understanding of the morphology and dynamics of the Ronne Ice Shelf.

Pfrogner Point headland

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Aster Glacier glacier in Antarctica

Aster Glacier is an Antarctic glacier descending the east slope of Craddock Massif and flowing between Elfring Peak and Willis Ridge to Thomas Glacier in the Sentinel Range, Ellsworth Mountains in Antarctica. It was named by the Advisory Committee on Antarctic Names in 2006, after Richard C. Aster, Professor of Geophysics and Department Head of Geosciences at Colorado State University, whose research in Antarctica includes volcanological studies at the Mount Erebus volcano observatory on Ross Island, glaciological, oceanic, and tectonic seismic source studies, seismic tomography, ice shelf studies, and the coupling of solid Earth geophysics and Antarctic ice sheet evolution.

Tulaczyk Glacier

Tulaczyk Glacier is a steep valley glacier draining the west slope of Vinson Massif southwest of Príncipe de Asturias Peak, and descending between Cairns Glacier and Zapol Glacier in the Sentinel Range, Antarctica. The glacier flows southwestward and leaving the range, together with Cairns Glacier joins Nimitz Glacier west of Hodges Knoll and southeast of Klenova Peak. It was named by US-ACAN (2006) after Slawek M. Tulaczyk, Earth Sciences, University of California, Santa Cruz; USAP researcher of West Antarctic ice streams from 1998.

References

PD-icon.svg This article incorporates  public domain material from the United States Geological Survey document "Henry Ice Rise" (content from the Geographic Names Information System ). Coordinates: 80°35′S62°0′W / 80.583°S 62.000°W / -80.583; -62.000

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.