Ramseier Glacier
   HOME

TheInfoList



OR:

The Byrd Glacier () is a major glacier in Antarctica, about long and wide. It drains an extensive area of the Antarctic plateau, and flows eastward to discharge into the
Ross Ice Shelf The Ross Ice Shelf is the largest ice shelf of Antarctica (, an area of roughly and about across: about the size of France). It is several hundred metres thick. The nearly vertical ice front to the open sea is more than long, and between high ...
.


Location

The Byrd Glacier flows eastward between the Britannia Range to the north and the Churchill Mountains to the south. It discharges into the Ross Ice Shelf at Barne Inlet. Its mouth lies between Cape Kerr to the north and Cape Selborne to the south. The valley below the glacier used to be recognised as one of the lowest points not to be covered by liquid water on Earth, reaching below sea level. The glacier was named by the NZ-APC after Rear Admiral
Richard E. Byrd Richard Evelyn Byrd Jr. (October 25, 1888 – March 11, 1957) was an American naval officer, and pioneering aviator, polar explorer, and organizer of polar logistics. Aircraft flights in which he served as a navigator and expedition leader cr ...
,
United States Navy The United States Navy (USN) is the naval warfare, maritime military branch, service branch of the United States Department of Defense. It is the world's most powerful navy with the largest Displacement (ship), displacement, at 4.5 millio ...
, American Antarctic explorer.


Mouth


Barne Inlet

A reentrant about wide occupied by the lower part of Byrd Glacier, lying between Cape Kerr and Cape Selborne on the west side of the Ross Ice Shelf. Discovered by the BrNAE (1901-04) and named for Lt. Michael Barne, RN, a member of the expedition, who with Sub-Lt. George F.A. Mulock, RN, mapped the coastline this far south in 1903.


Cape Kerr

A high snow-covered cape at the north side of Barne Inlet, the terminus of Byrd Glacier at the W side of the Ross Ice Shelf. Discovered by the BrNAE (1901-04) and named for Admiral of the Fleet, Lord Walter Kerr, one of the Sea Lords who lent his assistance to the expedition.


Cape Selborne

. A high snow-covered cape at the south side of Barne Inlet, the terminus of Byrd Glacier at the west side of the Ross Ice Shelf. Discovered by the BrNAE (1901-04) and named for William Waldegrave Palmer Selborne, Second Earl of Selborne, who entered the Cabinet as First Lord of the Admiralty in 1900. Not: Cape Selbourne, Cape Selhora.


Left tributaries

Tributaries entering the left (north) side of the glacier from the Brittania Range are, from west to east:


Ramseier Glacier

. Steep cirque-type glacier, long, flowing southwest to enter Byrd Glacier immediately east of Mount Rummage. Named by the US-ACAN for Réne O. Ramseier, glaciologist at McMurdo and´South Pole Stations, 1960-61 and 1961-62 seasons.


Peckham Glacier

. A steep tributary glacier, flowing south from Mount McClintock into Byrd Glacier. Named by US-ACAN for Verne E. Peckham, biologist, McMurdo Station winter party 1962, who with use of SCUBA gear made numerous dives under the sea ice of McMurdo Sound at Winter Quarters Bay and off Cape Evans.


DeVries Glacier

A steep tributary glacier just east of Peckham Glacier, flowing from the south slopes of the Britannia Range into Byrd Glacier. Named by US-ACAN for Arthur L. DeVries, USARP biologist at McMurdo Station in the 1961-62 and 1963-64 summer seasons.


Yancey Glacier

. A precipitous glacier, flowing east from the vicinity of Mount McClintock and then southeastward to enter Byrd Glacier just west of Sennet Glacier. Named by US-ACAN in association with nearby Byrd Glacier for the USS Yancey, cargo ship (Central Group of Task Force 68) of USN OpHjp, 1946-47, led by Admiral Byrd.


Sennet Glacier

. A precipitous glacier between Yancey and Merrick Glaciers, flowing southward from Mount Aldrich to the Byrd Glacier. Named by US-ACAN, ACAN, in association with Byrd Glacier, for the USS Sennet, submarine (Central Group 'of Task Force 68) of USN OpHjp, 1946-47, led by Admiral Byrd.


Merrick Glacier

. A steep tributary glacier just east of Sennet Glacier, descending southwestward to enter Byrd Glacier at the west end of Horney Bluff. Named by US-ACAN, in association with nearby Byrd Glacier, for the USS ''Merrick'', cargo ship (Central Group of Task Force 68) of USN
Operation Highjump Operation HIGHJUMP, officially titled The United States Navy Antarctic Developments Program, 1946–1947, (also called Task Force 68), was a United States Navy (USN) operation to establish the Antarctic research base Little America (exploration b ...
, 1946-47, led by Admiral Byrd.


Hourihan Glacier

Glacier draining the south slopes of Ward Tower, and flowing southeast to Merrick Glacier. Named by the US-ACAN in association with Byrd Glacier and Merrick Glacier, after Captain Joseph J. Hourihan, United States Navy, captain of USS ''Merrick'', a cargo vessel of United States Navy
Operation Highjump Operation HIGHJUMP, officially titled The United States Navy Antarctic Developments Program, 1946–1947, (also called Task Force 68), was a United States Navy (USN) operation to establish the Antarctic research base Little America (exploration b ...
, 1946-47, led by Admiral
Richard E. Byrd Richard Evelyn Byrd Jr. (October 25, 1888 – March 11, 1957) was an American naval officer, and pioneering aviator, polar explorer, and organizer of polar logistics. Aircraft flights in which he served as a navigator and expedition leader cr ...
.


Right tributaries

Tributaries entering the right (south) side of the glacier are:


Zeller Glacier

. A glacier about long, flowing west-north-west to enter the south side of Byrd Glacier just north of Mount Fries. Named by US-ACAN for Edward J. Zeller, geologist at McMurdo Station, 1959-60 and 1960-61 seasons.


Sefton Glacier

. Glacier about long, flowing into the south side of Byrd Glacier just west of Rundle Peaks. Named by the US-ACAN for Ronald Sefton, ionospheric physicist, a member of the Byrd Station winter parties of 1962 and 1964.


Twombley Glacier

A glacier long, flowing from the north side of the Kent Plateau into the south side of Byrd Glacier. Named by US-ACAN for C.E. Twombley of the U.S. Weather Bureau, a member of the Little America V winter party, 1956.


Brecher Glacier

. A broad glacier long in the north Churchill Mountains that flows north between the Rundle Peaks and Mandarich Massif into Byrd Glacier. It was named after Henry H. Brecher of the Byrd Polar Research Center,
Ohio State University The Ohio State University (Ohio State or OSU) is a public university, public Land-grant university, land-grant research university in Columbus, Ohio, United States. A member of the University System of Ohio, it was founded in 1870. It is one ...
; he conducted Antarctic glaciological investigations for over 30 years, 1960–95, including determinations of surface velocities and elevations on Byrd Glacier.


Judith Glacier

. Glacier about long, flowing from the vicinity of Mount Hamilton northeastward to enter Byrd Glacier just east of Mount Tuatara. Named by US-ACAN for Cdr. J.H. Judith, USN, commanding officer of the Edisto during USN OpDFrz 1964.


Névé

The large
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 the Byrd Glacier has several
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 ...
s in or around it. It is fed by a number of glaciers.


Byrd Névé

An immense névé at the head of Byrd Glacier. Named by the NZ-APC in association with Byrd Glacier.


Gamble Glacier

. A
glacier A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires ...
flowing northwest from Chapman Snowfield, and located between Green Nunatak at the southwest and Keating Massif at the northeast. It was named in honor of John A. Gamble, a geological scientist at the
Victoria University of Wellington Victoria University of Wellington (), also known by its shorter names "VUW" or "Vic", is a public university, public research university in Wellington, New Zealand. It was established in 1897 by Act of New Zealand Parliament, Parliament, and w ...
. He spent five field seasons (during 1984–93) in Antarctica working on mantle and crustal
xenolith A xenolith ("foreign rock") is a rock (geology), rock fragment (Country rock (geology), country rock) that becomes enveloped in a larger rock during the latter's development and solidification. In geology, the term ''xenolith'' is almost exclusi ...
studies to understand the nature of the West Antarctic
lithosphere A lithosphere () is the rigid, outermost rocky shell of a terrestrial planet or natural satellite. On Earth, it is composed of the crust and the lithospheric mantle, the topmost portion of the upper mantle that behaves elastically on time ...
. He has worked in
Marie Byrd Land Marie Byrd Land (MBL) is an unclaimed region of Antarctica. With an area of , it is the largest unclaimed territory on Earth. It was named after the wife of American naval officer Richard E. Byrd, who explored the region in the early 20th centu ...
, including the West Antarctica Volcano Expedition (1989–92), and on the volcanoes in
McMurdo Sound The McMurdo Sound is a sound in Antarctica, known as the southernmost passable body of water in the world, located approximately from the South Pole. Captain James Clark Ross discovered the sound in February 1841 and named it after Lieutenant ...
.


Bledisloe Glacier

. A
glacier A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires ...
flowing north west between All-Blacks Nunataks and Wallabies Nunataks. It was named in association with the adjacent All-Blacks and Wallabies Nunataks, and specifically named after the
Bledisloe Cup The Bledisloe Cup is an annual rugby union competition between the national teams of Australia's Wallabies and New Zealand's All Blacks that has been contested since the 1930s. The frequency that the competition is held has varied, as has the n ...
, which is contested between the New Zealand and Australian
rugby union Rugby union football, commonly known simply as rugby union in English-speaking countries and rugby 15/XV in non-English-speaking world, Anglophone Europe, or often just rugby, is a Contact sport#Terminology, close-contact team sport that orig ...
teams, the All-Blacks and the
Wallabies A wallaby () is a small or middle-sized macropod native to Australia and New Guinea, with introduced populations in New Zealand, Hawaii, the United Kingdom and other countries. They belong to the same taxonomic family as kangaroos and som ...
.


Skellerup Glacier

. A glacier flowing west north west between All-Blacks Nunataks and Wilhoite Nunataks, west of the Churchill Mountains. Named in honor of Peter Skellerup (1918–2006), who sponsored the Antarctic wing at Canterbury Museum. He was particularly keen on scientific research and donated money to build a specialist Antarctic Library at the Museum. He also donated a large collection of Antarctic materials to the Museum, including some very old and rare Antarctic manuscripts. He remained interested in the collection and continued his sponsorship and donations over more than 30 years.


Bates Nunataks

. Three isolated nunataks in the névé of Byrd Glacier, west of Vantage Hill, Britannia Range. Discovered by the Darwin Glacier Party of the CTAE (1956-58). Named by the NZ-APC for J. Bates, a member of CTAE who accompanied Sir Edmund Hillary to the South Pole.


Tyke Nunatak

. The smallest and northernmost of the Bates Nunataks at the west end of the Britannia Range. So named because of its small size in relation to the two southern nunataks in the group.


Littleblack Nunataks

A group of about a dozen black nunataks at the southeast side of the Byrd Neve. This scattered group lies southeast of All-Blacks Nunataks and southwest of Mount Nares of the Churchill Mountains. Charted and descriptively named by the NZGSAE, 1960-61.


Wallabies Nunataks

. A large group of nunataks near the polar plateau, lying northeast of All-Blacks Nunataks at the east side of the Byrd Névé. Named by the NZGSAE (1960-61) for the well known Australian rugby team.


References


Sources

* * * * * * * * * {{Authority control Ice streams of Antarctica Glaciers of Oates Land Glaciers of Hillary Coast