Crisp Glacier
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The Gonville and Caius Range () is a range of peaks, high, between
Mackay Glacier Mackay Glacier () is a large glacier in Victoria Land, descending eastward from the Antarctic Plateau, between the Convoy Range and Clare Range, into the southern part of Granite Harbour. It was discovered by the South magnetic pole party of the B ...
and Debenham Glacier in
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.


Exploration and naming

The Gonville and Caius Range was first mapped by the British Antarctic Expedition, 1910–13, under
Robert Falcon Scott Captain Robert Falcon Scott (6 June 1868 – ) was a British Royal Navy officer and explorer who led two expeditions to the Antarctic regions: the Discovery Expedition, ''Discovery'' expedition of 1901–04 and the Terra Nova Expedition ...
, and was named for Gonville and Caius College, of
Cambridge University The University of Cambridge is a Public university, public collegiate university, collegiate research university in Cambridge, England. Founded in 1209, the University of Cambridge is the List of oldest universities in continuous operation, wo ...
, the alma mater of several members of the expedition.


Location

The
Clare Range The Clare Range () is the range extending west-southwest from Sperm Bluff to the Willett Range on the south side of Mackay Glacier, in Victoria Land, Antarctica. It is south of the Convoy Range and north of the Olympus Range. Exploration and na ...
is to the west of the Gonville and Caius Range, and Saint Johns Range to the south. Wilson Piedmont Glacier is to the east, along the coast of the Ross Sea.
Mackay Glacier Mackay Glacier () is a large glacier in Victoria Land, descending eastward from the Antarctic Plateau, between the Convoy Range and Clare Range, into the southern part of Granite Harbour. It was discovered by the South magnetic pole party of the B ...
defines the north limit of the range. Killer Ridge, Second Facet and First Facet are to the north of Debenham Glacier and its tributary Miller Glacier. Queer Mountain is just west of Killer Ridge. The Crisp Glacier flows between the Killer Ridge and Second Facet. To the north are Mount Jensen, Red Ridge, Robson Glacier, Haystack Mountain and Mount England.


Glaciers


Crisp Glacier

. Glacier between Killer Ridge and Second Facet, flowing southeast into Debenham Glacier. 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 Kelton W. Crisp, United States Navy, who was in charge of the electric shop 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 ...
, 1962.


Griffiths Glacier

. Prominent cirque-type glacier located northeast of Crisp Glacier in Gonville and Caius Range. The feature drains east-southeast to Debenham Glacier to the east of Second Facet. Named after Harold Griffiths (d. 1974) who was associated with Antarctic exploration for over 50 years. He was instrumental in the NZ Antarctic Society's campaign to get the NZ Government to establish a presence in Antarctica.


Robson Glacier

. A glacier about long, which flows north from the Gonville and Caius Range along the east side of Red Ridge. It merges with the general flow of ice toward Granite Harber southward of Redcliff Nunatak. Named by the Western Journey Party, led by Taylor, of the British Antarctic Expedition, 1910-13.


Pyne Glacier

. Glacier east of Robson Glacier in Gonville and Caius Range. Flows north and joins Mackay Glacier system southwest of
The Flatiron Granite Harbour () is a bay in the coast of Victoria Land, Antarctica, about long, entered between Cape Archer and Cape Roberts. It was discovered and named by the British National Antarctic Expedition (BrNAE) of 1901–04 in the ''RRS Discover ...
. Named after Alex Pyne, recipient of the Polar Medal for services in Antarctic geological and in particular glacial research since 1977; currently works at Victoria University's Antarctic Research Centre in Wellington.


Bachtold Glacier

. A glacier flowing north from Mount Chaudoin, into the lower part of
Cotton Glacier Wilson Piedmont Glacier () is a large piedmont glacier extending from Granite Harbour to Marble Point on the coast of Victoria Land. Discovery and name The Wilson Piedmont Glacier was discovered by the ''Discovery'' expedition, 1901–1904. ...
. The glacier drains the broad slopes between Killer Ridge and Red Ridge. Named by US-ACAN (2007) after CE2 Harry W. Bachtold, United States Navy (United States Navy) (Seabees), who at the time was a member of the construction crew which built the original Little America V Station and the original Byrd Station in the 1955-57 pre-IGY period.


Fritter Glacier

. A glacier between Mount Curtiss and Mount Jensen. It flows east to Wilson Piedmont Glacier. Named in association with Mount Curtiss (q.v.) after Captain C.T. Fritter, United States Navy (United States Navy), commander of the seaplane tender USS Curtiss in the Ross Sea, Operation Deep Freeze II, 1956-57.


Other features


Queer Mountain

. A conspicuous black mountain, high, with steep slopes showing bands of sandstone above the granite, standing west of Killer Ridge, between the Cotton and Miller Glaciers. Mapped by the British Antarctic Expedition, 1910–13, and so named because, though surrounded by glacier, it has nearly every rock in the district, including coal beds, represented on its cliffs.


Low Nunatak

. A
nunatak A nunatak (from Inuit language, Inuit ) is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They often form natural pyramidal peaks. Isolated nunataks are also cal ...
in the Cotton Glacier north of the western end of Killer Ridge. About long, the nunatak rises above the surrounding ice surface to about above sea level. The descriptive name appears on the map of the British Antarctic Expedition, 1910-13.


Killer Ridge

. Dark ridge rising over high between Crisp and Miller Glaciers. Charted by the British Antarctic Expedition, 1910-13, and named after the
killer whale The orca (''Orcinus orca''), or killer whale, is a toothed whale and the largest member of the oceanic dolphin family. The only extant species in the genus '' Orcinus'', it is recognizable by its black-and-white-patterned body. A cosmopolit ...
, whose outline the ridge is said to resemble.


Second Facet

. A steep ice-free bluff standing just west of First Facet, the two features together forming the north wall of Debenham Glacier. Charted and descriptively named by the British Antarctic Expedition, 1910-13.


First Facet

. Steep ice-free bluff rising just eastward of Second Facet, forming a part of the north wall of Debenham Glacier. Charted and descriptively named by the British Antarctic Expedition, 1910-13.


Mount Jensen

. A peak over high, just north of First Facet. Mapped and named by the British Antarctic Expedition, 1910–13.


Red Ridge

. A ridge just west of Robson Glacier. The descriptive name was given by F. Debenham of the British Antarctic Expedition (1910-13) during his plane table survey in 1912.


Haystack Mountain

. A mountain over high with a rounded summit suggestive of a mound or haystack, standing east of Mount England in the northeast part of the Gonville and Caius Range. Charted and named by the British Antarctic Expedition, 1910-13 under Scott.


Mount England

. Conical-topped mountain, high, rising immediately south of New Glacier. Discovered by the British National Antarctic Expedition, 1901-04, under Scott, who named it for Lieutenant Rupert England, Royal Navy, of the ''Morning'', relief ship to the expedition.


Mount Chaudoin

. An abrupt mountain rising to about in the west part of Gonville and Caius Range. The mountain forms part of the divide between Bachtold Glacier and the head of Griffiths Glacier. Named by US-ACAN (2007) after YNC Robert L. Chaudoin United States Navy (United States Navy) (Seabees), who at the time was the Senior Administrative Yeoman to the commanding officer and member of the construction crew which built the original McMurdo Station and the original South Pole Station in the 1955-57 pre-IGY period. He also was the first United States Navy Postal Clerk at the South Pole Station, 1956.


Prescott Spur

. A rock spur running north-south and rising to between Robson Glacier and Pyne Glacier. Named by US-ACAN (2007) after BU2 Richard J. Prescott, United States Navy (United States Navy) (Seabees), who at the time was a member of the construction crew which built the original McMurdo Station, the original Beardmore Refueling Station and the original South Pole Station in the 1955-57 pre-IGY period. He was also a sled dog handler at McMurdo and South Pole Stations.


Mount Curtiss

. A peak about high at the east end of the main ridge of Gonville and Caius Range. Named after the seaplane tender USS ''Curtiss'' which transported personnel to McMurdo Sound in Operation Deep Freeze II, 1956-57. Departing, she carried out wintering-over personnel of Deep Freeze I and construction party personnel left at Cape Hallett.


Stroup Peak

. A peak rising to at the extremity of the ridge extending east from Mount Curtiss. The peak stands east of Mount Curtiss where it overlooks the north part of Wilson Piedmont Glacier. Named by US-ACAN (2007) after CW04 William E. Stroup, Civil Engineer Corps (CEC), United States Navy (United States Navy) (Seabees), who at the time was the senior enlisted Construction Electrician Chief and member of the construction crew which built the original Little America V Station and the original Byrd Station in the 1955-57 pre-IGY period. He was also a member of the Byrd Traverse to Byrd Station in 1956.


References


Sources

* * * * * * * * * * * * Mountain ranges of Victoria Land Scott Coast {{ScottCoast-geo-stub