Corner Glacier
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The Priestley Glacier () is a major valley glacier, about long, originating at the edge of the
Polar Plateau The Antarctic Plateau, Polar Plateau or King Haakon VII Plateau is a large area of East Antarctica that extends over a diameter of about , and includes the region of the geographic South Pole and the Amundsen–Scott South Pole Station. This ...
of
Victoria Land Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78th parallel south, 78°00'S, and westward from the Ross Sea to the edge of the Ant ...
, Antarctica. The glacier drains southeast between the Deep Freeze Range and
Eisenhower Range The Eisenhower Range () is a majestic mountain range, about long and rising to , which rises between Reeves Névé on the west, Reeves Glacier on the south, and Priestley Glacier on the north and east, in Victoria Land, Antarctica. The range ...
to enter the northern end of the
Nansen Ice Sheet Nansen Ice Sheet () is a long by wide ice shelf. It is nourished by the Priestley and Reeves Glaciers and abuts the north side of the Drygalski Ice Tongue, along the coast of Victoria Land, Antarctica. This feature was explored by the South M ...
. It was first explored by the Northern Party of the
British Antarctic Expedition, 1910–13 The ''Terra Nova'' Expedition, officially the British Antarctic Expedition, was an expedition to Antarctica which took place between 1910 and 1913. Led by Captain Robert Falcon Scott, the expedition had various scientific and geographical objec ...
, and named for
Raymond Priestley Sir Raymond Edward Priestley (20 July 1886 – 24 June 1974) was an English geologist and early Antarctic explorer. He was Vice-Chancellor of the University of Birmingham, where he helped found The Raymond Priestley Centre on the shores ...
, a geologist with the Northern Party.


Geography

The Priestly Glacier is fed by the Priestly Névé, which lies to the east of the polar plateau, south of the Lister Nunataks, Brawn Rocks and
Rennick Névé Rennick Glacier () is a broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier ...
. It runs southeast between the Szanto Spur and Wasson Rock to the northeast and Clingman Peak, Tantalus Peak and the Ogden Heights to the southwest. Foolsmate Glacier joins it from the southwest. It continues southeast between the
Eisenhower Range The Eisenhower Range () is a majestic mountain range, about long and rising to , which rises between Reeves Névé on the west, Reeves Glacier on the south, and Priestley Glacier on the north and east, in Victoria Land, Antarctica. The range ...
to the southwest and the Deep Freeze Range to the northeast. The Nash Ridge forms part of its southwest flank. South of this it is fed by O'Kane Glacier from the northwest, which in turn receives ice from O'Kane Canyon. South of Black Ridge on its eastern flank, as it merges into the
Nansen Ice Sheet Nansen Ice Sheet () is a long by wide ice shelf. It is nourished by the Priestley and Reeves Glaciers and abuts the north side of the Drygalski Ice Tongue, along the coast of Victoria Land, Antarctica. This feature was explored by the South M ...
, it is fed by the Corner Glacier.


Tributaries


Foolsmate Glacier

. A small, heavily crevassed tributary glacier flowing northeast to enter Priestley Glacier, west of
Shafer Peak The Deep Freeze Range () is a rugged mountain range, over long and about wide, rising between Priestley Glacier, Priestley and Campbell Glacier, Campbell Glaciers in Victoria Land, Antarctica, and extending from the edge of the polar plateau to ...
. The name was applied by the Southern Party of the NZGSAE, 1962-63.


O'Kane Glacier

. A steep glacier, long, draining the east wall of Eisenhower Range between Mount Baxter and Eskimo Point and flowing southeast to its terminus opposite the mouths of the Priestley and Corner Glaciers at the north extremity of Nansen Ice Sheet. Named by US-ACAN in association with O'Kane Canyon, located at the head of the glacier.


O'Kane Canyon

. A steep-walled canyon at the head of O'Kane Glacier, indenting the east side of Eisenhower Range between Mount Baxter and Eskimo Point. Named by the Southern Party of NZGSAE, 1962–63, for H.D. O'Kane, photographer at Scott Base, 1961-62. O'Kane had made several reconnaissance flights to provide aerial photographs of the area.


Corner Glacier

. A steep glacier descending Deep Freeze Range between Black Ridge and
Mount Dickason The Deep Freeze Range () is a rugged mountain range, over long and about wide, rising between Priestley and Campbell Glaciers in Victoria Land, Antarctica, and extending from the edge of the polar plateau to Terra Nova Bay. It is southwest of ...
to merge with the confluent ice of Nansen Ice Sheet. First explored by the Northern Party of the British Antarctic Expedition (BrAE), 1910-13, and so named by them because of its location with respect to the Nansen Ice Sheet.


Other features


Priestley Névé

. The
névé Névé is a young, granular type of snow which has been partially melted, refrozen and compacted, yet precedes the form of ice. This type of snow can contribute to glacier formation through the process of ''nivation''. Névé that survives a ...
at the head of Priestley Glacier. Named by the
New Zealand Antarctic Place-Names Committee New Zealand Antarctic Place-Names Committee (NZ-APC) is an adjudicating committee established to authorize the naming of features in the Ross Dependency on the Antarctic continent. It is composed of the members of the New Zealand Geographic Board pl ...
(NZ-APC) in about 1966 in association with Priestley Glacier.


Lister Nunataks

. Isolated nunataks located in the north reaches of Priestley Névé, about south-southwest of Brawn Rocks. Mapped by the
United States Geological Survey The United States Geological Survey (USGS), founded as the Geological Survey, is an agency of the U.S. Department of the Interior whose work spans the disciplines of biology, geography, geology, and hydrology. The agency was founded on Mar ...
(USGS) from surveys and United States Navy air photos, 1960-64. Named by the United States
Advisory Committee on Antarctic Names The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established ...
(US-ACAN) for Larry W. Lister, helicopter flight crewman with United States Navy Squadron VX-6 during Operation Deep Freeze 1966, 1967 and 1968.


Brawn Rocks

. Prominent isolated rocks extending over long, lying southwest of
Sequence Hills Sequence Hills () is an escarpment-like hills on the west margin of the upper Rennick Glacier, about 7 nautical miles (13 km) northwest of Caudal Hills, Victoria Land. They provided the only good geological sequence in the area. Mapped and na ...
. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for James E. Brawn, aviation machinist's mate with United States Navy Squadron VX-6 at
McMurdo Station McMurdo Station is an American Antarctic research station on the southern tip of Ross Island. It is operated by the United States through the United States Antarctic Program (USAP), a branch of the National Science Foundation. The station is ...
, 1966.


Szanto Spur

. A noteworthy rock spur jutting from the north wall into Priestley Glacier, at the head of the glacier. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for Otto R. Szanto, United States Navy, radio man who served in Antarctic support activities for four seasons at McMurdo Station in the 1960s.


Wasson Rock

. A prominent, mainly ice-free rock situated along the north wall near the head of Priestley Glacier. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for William G. Wasson, aviation electrician's mate with United States Navy Squadron VX-6 at McMurdo Station, 1966.


Clingman Peak

. The final peak, high, along the south wall at the head of Priestley Glacier. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for Otis Clingman, Jr., biologist at McMurdo Station, 1965-66.


Tantalus Peak

. The highest peak, high, along the south wall at the head of Priestley Glacier. So named by the southern party of
New Zealand Geological Survey Antarctic Expedition The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 19 ...
(NZGSAE), 1962–63, because an attempt to establish a station there proved abortive due to steep ice. (Tantalus, son of Zeus, was punished for transgressions by "standing in water that ebbed when he would drink.")


Ogden Heights

. Flattish, mainly ice-covered heights, about long, forming a part of the south wall of upper Priestley Glacier to the southeast of Tantalus Peak. The heights are near where the southern party of the NZGSAE, 1962–63, was landed. Named by them for Lieutenant John H. Ogden, United States Navy, pilot who airlifted the party to this point, flew in their resupply, and later flew the party back to base at the end of the season.


Simpson Crags

. A series of rugged crags descending southeast from Mount Baxter of the Eisenhower Range and forming the south wall of O'Kane Glacier. Mapped by USGS from surveys and United States Navy air photos, 1955-63. Named by US-ACAN for Lieutenant Commander William A. Simpson, Jr., United States Navy, aircraft commander with Squadron VX-6 during USN Operation Deep Freeze 1967.


References


Sources

* * * * {{Antarctica Glaciers of Victoria Land Scott Coast