Herbert Range
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The Herbert Range () is a range in the
Queen Maud Mountains The Queen Maud Mountains () are a major group of mountains, ranges and subordinate features of the Transantarctic Mountains, lying between the Beardmore Glacier, Beardmore and Reedy Glaciers and including the area from the head of the Ross Ice Sh ...
of Antarctica, extending from the edge of the
Antarctic 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. Thi ...
to 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 ...
between the
Axel Heiberg Glacier The Axel Heiberg Glacier () in Antarctica is a valley glacier, long, descending from the high elevations of the Antarctic Plateau into the Ross Ice Shelf (nearly at sea level) between the Herbert Range and Mount Don Pedro Christophersen in the Q ...
and
Strom Glacier Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. Name The g ...
. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for Walter W. Herbert, leader of the Southern Party of the New Zealand GSAE (1961–62) which explored the Axel Heiberg Glacier area.


Course

The Herbert Range runs from west to east between the
Axel Heiberg Glacier The Axel Heiberg Glacier () in Antarctica is a valley glacier, long, descending from the high elevations of the Antarctic Plateau into the Ross Ice Shelf (nearly at sea level) between the Herbert Range and Mount Don Pedro Christophersen in the Q ...
to the south and the
Strom Glacier Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. Name The g ...
to the north. Peaks in the west include Gjelsvik Peak, Mount Fridtjof Nansen,
Webster Knob Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. Name The g ...
and Mount Balchen. Peaks further east include Bell Peak, Mount Cohen, Zigzag Bluff and Mount Betty, to the north of Bigend Saddle.
Cohen Glacier Strom Glacier () is a steep valley glacier flowing northeast from the north side of Mount Fridtjof Nansen to the head of the Ross Ice Shelf, flanked on the northwest by the Duncan Mountains and on the southeast by the Herbert Range. Name The g ...
runs north from Mount Cohen to join Strom Glacier.
Sargent Glacier The Axel Heiberg Glacier () in Antarctica is a valley glacier, long, descending from the high elevations of the Antarctic Plateau into the Ross Ice Shelf (nearly at sea level) between the Herbert Range and Mount Don Pedro Christophersen in the Q ...
runs southwest from Mount Cohen to join Axel Heiberg Glacier.


Features

Geographical features include:


Gjelsvik Peak

. A peak, high, standing northwest of Mount Fridtjof Nansens. Named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961-62) for Tore Gjelsvik, Director of the Norsk Polarinstitutt, Oslo.


Mount Fridtjof Nansen

. A high massive mountain, high, which dominates the area between the heads of Strom and Axel Heiberg Glaciers, in the Queen Maud Mountains. Discovered by Roald Amundsen in 1911, and named by him for Fridtjof Nansen, polar explorer, who helped support Amundsen's expedition.


Barracouta Ridge

. A long jagged ridge which terminates on the north in Webster Knob. The ridge is an extension from the base of Mount Fridtjof Nansen into the head of Strom Glacier. Discovered and visited in 1929 by the geological party under Laurence Gould of the Byrd Antarctic Expedition (ByrdAE), 1928-30. It was climbed by geologists of the Southern Party of the NZGSAE, 1963–64. The descriptive name, applied by the Southern Party derives from the appearance of the toothlike pinnacle along the crest of the ridge.


Cenotaph Hill

. A rock peak, high, on the ridge separating the heads of Strom Glacier and Liv Glacier in the Queen Maud Mountains. The peak is north-northeast of the summit of Mount Fridtjof Nansen. It was visited by the Southern Party of NZGSAE (1963-64) who gave this name because the unusual knob of rock forming the summit resembles a monument.


Mount Balchen

. A prominent peak, 3,085 m, standing east of the summit of Mount Fridtjof Nansen. Named by the Southern Party of the NZGSAE (1961-62) for Bernt Balchen, pilot with Roald Amundsen on Arctic flights, and with R. Admiral Richard E. Byrd on his South Pole flight of 1929.


Bell Peak

. A peak, high, surmounting a southeast trending spur, just southwest of Sargent Glacier. The peak was probably observed by Roald Amundsen's south polar party in 1911, and was later roughly mapped by the ByrdAE, 1928-30. Named by US-ACAN for G. Grant Bell who studied cosmic rays at McMurdo Station, winter party 1962.


Mount Cohen

. A peak, high, standing southwest of Mount Betty in the Herbert Range. Discovered by Rear Admiral Byrd on several ByrdAE plane flights to the Queen Maud Mountains in November 1929, and named by him for Emanuel Cohen of Paramount Pictures, who assisted in assembling the motion picture records of the expedition.


Zigzag Bluff

. A rock bluff at the foot of Herbert Range, overlooking Ross Ice Shelf about west of the terminus of Axel Heiberg Glacier. Probably first seen by Roald Amundsen in 1911, the bluff was roughly mapped by the ByrdAE, 1928-30. So named by the Southern Party of the NZGSAE, 1961-62, because of the peculiar folding of the marble on the bluff.


Mount Betty

. A small ridge overlooking Ross Ice Shelf, located on the north side of Bigend Saddle in the northeast extremity of the Herbert Range. Discovered in November 1911 by Captain Roald Amundsen, and named by him for Betty Andersson, nurse and housekeeper in the Amundsen family for many years. A
cairn A cairn is a human-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the (plural ). Cairns have been and are used for a broad variety of purposes. In prehistory, t ...
was erected on the ridge by Amundsen on 6 January 1912, on his way back to
Framheim Framheim was the name of explorer Roald Amundsen's base at the Bay of Whales on the Ross Ice Shelf in Antarctica during his successful quest for the South Pole. It was used between January 1911 and February 1912. Cabin and tents The hut was co ...
from the
South Pole The South Pole, also known as the Geographic South Pole or Terrestrial South Pole, is the point in the Southern Hemisphere where the Earth's rotation, Earth's axis of rotation meets its surface. It is called the True South Pole to distinguish ...
. It is known as "Amundsen’s cairn" and has been designated a Historic Site or Monument (HSM 24), following a proposal by Norway to the Antarctic Treaty Consultative Meeting.


Bigend Saddle

. A snow-covered saddle at the southwest side of Mount Betty in northern Herbert Range, Queen Maud Mountains. The saddle was traversed in December 1929 by the ByrdAE geological party under Laurence Gould. It was named by the Southern Party of the NZGSAE, 1963-64, because one of the party's motor toboggans was abandoned here with a smashed big end bearing.


References


Sources

* * * * {{Include-USGov , agency=United States Geological Survey East Antarctica Queen Maud Mountains Amundsen Coast