Lyttelton Peak
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The Cobham Range () is a mountain range in the
Churchill Mountains The Churchill Mountains are a mountain range group of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica. They border on the western side of the Ross Ice Shelf, between Byrd Glacier and Nimrod Glacier. Seve ...
of the Ross Dependency, Antarctica. It extends to the north of the
Nimrod Glacier The Nimrod Glacier is a major glacier about 135 km (85 mi) long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains between the Geologists and Miller Ranges, then northeasterly between the Chu ...
.


Location

The Cobham Range trends in a northwest–southeast direction for about in the southern part of the
Churchill Mountains The Churchill Mountains are a mountain range group of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica. They border on the western side of the Ross Ice Shelf, between Byrd Glacier and Nimrod Glacier. Seve ...
of the Ross Dependency, Antarctica. The
Prince Philip Glacier The Nimrod Glacier is a major glacier about 135 km (85 mi) long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains between the Geologists and Miller Ranges, then northeasterly between the Chur ...
runs south down the east side of the Cobham Range, and the
Lucy Glacier The Nimrod Glacier is a major glacier about 135 km (85 mi) long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains between the Geologists and Miller Ranges, then northeasterly between the Chur ...
runs southeast down the west side. They both feed the
Nimrod Glacier The Nimrod Glacier is a major glacier about 135 km (85 mi) long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains between the Geologists and Miller Ranges, then northeasterly between the Chu ...
, which flows to the northeast past the south end of the range. The
Holyoake Range Holyoake Range () is a mountain range in the southern section of the Churchill Mountains, extending in a northwest–southeast direction for about between Prince Philip Glacier and Errant Glacier. It and the Churchill Mountains are part of the ...
is east of the Cobham Range on the east side of the Prince Philip Glacier. The Queen Elizabeth Range is south of the Cobham Range on the south side of the Nimrod Glacier.


Early exploration and naming

The Cobham Range was mapped by the northern party of the
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 1957 ...
(NZGSAE), 1961–62, and 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 ...
for a former
Governor-General of New Zealand The governor-general of New Zealand ( mi, te kāwana tianara o Aotearoa) is the viceregal representative of the monarch of New Zealand, currently King Charles III. As the King is concurrently the monarch of 14 other Commonwealth realms and li ...
, Lord Cobham.


Geology

The range gives its name to the "Cobham Formation". This is a sequence of interlayered quartzite, marble and schist of the albite-epidote hornfels facies. It is conformably overlain by greywacke and argillite of the Goldie Formation. The Cobham Formation crops out in the south-west portion of the Cobham Range as a strip about wide extending from west of
Mount Kopere The Cobham Range () is a mountain range in the Churchill Mountains of the Ross Dependency, Antarctica. It extends to the north of the Nimrod Glacier. Location The Cobham Range trends in a northwest–southeast direction for about in the southe ...
south to
Gargoyle Ridge The Cobham Range () is a mountain range in the Churchill Mountains of the Ross Dependency, Antarctica. It extends to the north of the Nimrod Glacier. Location The Cobham Range trends in a northwest–southeast direction for about in the souther ...
.


Features

Geographical features from north to south include:


Frustration Ridge

. Ridge forming the north end of the Cobham Range in the Churchill Mountains. So named by the Holyoake, Cobham, and Queen Elizabeth Ranges party of the NZGSAE (1964–65) because although from below it looked a simple climb, great difficulty was experienced in traversing it.


Schroeder Peak

. Peak, high, standing northwest of Mount Kopere in the Cobham Range. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by the
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 James E. Schroeder,
United States Antarctic Program The United States Antarctic Program (or USAP; formerly known as the United States Antarctic Research Program or USARP and the United States Antarctic Service or USAS) is an organization of the United States government which has presence in the A ...
(USARP) glaciologist at Little America V, 1959-60.


Mount Kopere

. Peak northwest of Lyttelton Peak in the central part of Cobham Range. Named by the Holyoake, Cobham and Queen Elizabeth Ranges party of the NZGSAE (1964-65). Kopere is the Maori word for arrow; the peak's triangular cross section from most directions suggests an arrowhead.


Lyttelton Peak

. The highest peak, 2,335 m, of the Cobham Range. Mapped by the NZGSAE (1961-62) and given the family name of the former Governor-General of New Zealand, Lord Cobham. Not: Lyttleton Peak.


Tarakanov Ridge

. A prominent ridge from the Cobham Range, between the Gray Glacier and Prince Philip Glacier. Mapped by the USGS from tellurometer surveys and Navy air photos, 1960-62. Named by US-ACAN for Gennady Tarakanov, Soviet exchange scientist, meteorologist at
McMurdo Station McMurdo Station is a United States Antarctic research station on the south tip of Ross Island, which is in the New Zealand-claimed Ross Dependency on the shore of McMurdo Sound in Antarctica. It is operated by the United States through the Unit ...
in 1963.


Gray Glacier

. A glacier in the Cobham Range, long, lying south of Tarakanov Ridge and flowing southeast to merge with Prince Philip Glacier where the two join the Nimrod Glacier. Named by the Holyoake, Cobham, and Queen Elizabeth Ranges party of the NZGSAE (1964-65) for M. Gray, postmaster and assistant radio officer at Scott Base, 1965.


Gargoyle Ridge

. High rock ridge forming the south end of Cobham Range in the Churchill Mountains. So named by the Holyoake, Cobham, and Queen Elizabeth Ranges party of the NZGSAE (1964-65) because of the curiously wind-carved rock buttresses on top of the ridge.


Nearby features

Nearby features include:


Olson Névé

. A névé on the northwest side of Cobham Range which nourishes the Lucy and Prince Philip Glaciers, in the Churchill Mountains. Mapped by the Holyoake, Cobham and Queen Elizabeth Ranges party of the NZGSAE (1964-65). Named for Lt. Dennis A. Olson, USN, who flew the New Zealand party to the névé and supported it during the summer season. The feature is incorrectly identified as "Olsen Névé"on some maps of the late 1960's.


Chappell Nunataks

. Group of nunataks west of the central part of the Cobham Range. Named by the NZGSAE (1964-65) for J. Chappell, geologist with the expedition.


Turret Nunatak

. Elongated nunatak, high, standing west of Cobham Range in the lower portion of Lucy Glacier. Mapped by the northern party of the NZGSAE (1961-62) and so named because of the turreted cliffs on its southern side.


Half Dome Nunatak

. Nunatak lying south of Cobham Range, at the mouth of Lucy Glacier. So named by the northern party of the NZGSAE (1961-62) because it is rounded on one side and cut into sheer cliffs on the other side.


Kon-Tiki Nunatak

. Raft-like nunatak, high, surmounting the
Cooper Icefalls The Nimrod Glacier is a major glacier about 135 km (85 mi) long, flowing from the polar plateau in a northerly direction through the Transantarctic Mountains between the Geologists and Miller Ranges, then northeasterly between the ...
in the center of Nimrod Glacier. Seen by the northern party of the NZGSAE (1961-62) and named after the raft Kon-Tiki which drifted across the Pacific Ocean from east to west in 1947.


References


Sources

* * * {{refend Mountain ranges of Oates Land Transantarctic Mountains