The Barton Mountains () are a group of mountains located south of the

Commonwealth Range The Commonwealth Range is a north-south trending range of rugged mountains, long, located within the Queen Maud Mountains on the Dufek Coast of the continent of Antarctica. The range borders the eastern side of Beardmore Glacier from the Ross ...

and the Hughes Range and bounded by

Keltie Glacier Keltie Glacier is a large Antarctic glacier, long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the Br ...

Brandau Glacier Brandau Glacier () is a wide tributary glacier, long, flowing westward from an ice divide between Haynes Table and Husky Heights to enter Keltie Glacier just west of Ford Spur. It was named by the Advisory Committee on Antarctic Names for Lieute ...

Leigh Hunt Glacier Keltie Glacier is a large Antarctic glacier, long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the Briti ...

, and

Snakeskin Glacier Keltie Glacier is a large Antarctic glacier, long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the Britis ...

, 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 and Reedy Glaciers and including the area from the head of the Ross Ice Shelf to the Antarcti ...

Exploration and naming

The Barton Mountains were mapped by the

United States Geological Survey The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, ...

(USGS) from surveys and from

United States Navy The United States Navy (USN) is the maritime service branch of the United States Armed Forces and one of the eight uniformed services of the United States. It is the largest and most powerful navy in the world, with the estimated tonnage ...

aerial photographs, 1958–63. They were named by the Advisory Committee on Antarctic Names (US-ACAN) after Lieutenant Commander Walter H. Barton, U.S. Navy, officer in charge of the Squadron

VXE-6 Antarctic Development Squadron Six (VXE-6 or ANTARCTIC DEVRON SIX, commonly referred to by its nickname, The Puckered Penguins) was a United States Navy air test and evaluation squadron based at Naval Air Station Point Mugu, California with forwa ...

detachment at Beardmore South Camp in the 1985–86 field season. Lieutenant Commander Barton developed, coordinated, and executed the logistical plan for this large and remote camp, which was in operation for 78 days and required over 800 flight hours in support of research in the Beardmore Glacier area.

Location

The Barton Mountains lie to the south of the point where the

enters the

from the southwest. They are separated from the Supporters Range to the west by the

. Northern features include Mount Usher, and Hare Peak to the east across

. Features of the south of range include Mount Clarke, Graphite Peak and Tricorn Mountain.

Falkenhof Glacier Keltie Glacier is a large Antarctic glacier, long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the Bri ...

forms in the Barton Mountains and runs west into

, which defines the west side of the range. The Lhasa Nunatak is a long ridge running north-south to the west of Snakeskin Glacier.

Features

Mount Usher

. A distinctive mountain overlooking the south side of Keltic Glacier about southwest of the mouth of Brandau Glacier. Discovered and named by the British Antarctic Expedition (1907-09). Identification of this feature varied on subsequent maps. The present description follows the H.E. Saunders map of 1961 which has now been generally accepted.

Hare Peak

. An ice-free peak, high, at the north end of the ridge forming the east side of Leigh Hunt Glacier. Named by 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) for C.H. Hare, a member of the

British National Antarctic Expedition The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–184 ...

(1901-04).

Mount Clarke

. A mountain, high, located due east of Mount Iveagh. The feature rises along the east margin of the Snakeskin Glacier, near the edge of the interior ice plateau. Discovered and named by the Southern Journey Party of the British Antarctic Expedition (1907-09) under Ernest Shackleton.

Graphite Peak

. A peak, high, standing at the northeast end of a ridge running northeast from Mount Clarke, just south of the head of Falkenhof Glacier. So named by the NZGSAE (1961-62) because of the graphite found on the peak.

Tricorn Mountain

. A mountain, high, standing east of Graphite Peak, about midway between the heads of Falkenhof and Leigh Hunt Glaciers. Named by the NZGSAE (1961-62) because of its resemblance to an admiral's tricorn hat.

Lhasa Nunatak

. Narrow rock ridge, long, trending in a northwest–southeast direction between Snakeskin Glacier and Jensen Glacier, to the east of Supporters Range. So named by the NZGSAE (1961-62) because the central peak resembles a Tibetan monastery perched on top of a hill.

References

Sources

* * * *{{Include-USGov , agency=United States Geological Survey Mountain ranges of the Ross Dependency Dufek Coast