Rawson Mountains | |
---|---|
Geography | |
Continent | Antarctica |
Region | Ross Dependency |
Range coordinates | 86°43′S 154°40′W / 86.717°S 154.667°W |
Parent range | Queen Maud Mountains |
The Rawson Mountains (86°43′S 154°40′W / 86.717°S 154.667°W) lie within the Queen Maud Mountains to the southeast of the Ross Ice Shelf in Antarctica. They are a crescent-shaped range of tabular, ice-covered mountains including Fuller Dome, Mount Wyatt and Mount Verlautz, standing southeast of Nilsen Plateau and extending southeast for 18 nautical miles (33 km; 21 mi) to the west side of Scott Glacier.[1]
Discovery and naming
The Rawson Mountains were discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn. The were named by Richard E. Byrd for Frederick H. Rawson, American banker and contributor to the Byrd Antarctic Expeditions of 1928-30 and 1933-35.[1]
Location
The Rawson Mountains are to the southeast of Nilsen Plateau and south of the head of the Holdsworth Glacier. The Scott Glacier forms to their east and flows north towards the Ross Ice Shelf. The Amundsen Glacier forms to their west and flows northwest towards the Ross Ice Shelf.[2]
Features of the Rawson Mountains, from west to east, include Fuller Dome, Mount Wyatt and Mount Verlautz. To the south of the mountains is the Poulter Glacier, which in turn is north of the isolated Mount Innes-Taylor, Mount Saltonstall, Mount Weaver and Mount Wilbur. To the north of the mountains are a line of mountains west of Scott Glacier including Mount Przywitowski, McNally Peak, Mount Farley, Mount Denauro, Lee Peak, Mount Ruth and Mount Gardiner. These last two stand where Bartlett Glacier and Scott Glacier converge.[2]
Features
Named features of the Rawson Mountains include, from west to east:
Fuller Dome
86°38′S 156°18′W / 86.633°S 156.300°W. A dome-shaped, ice-covered mountain. 2,850 metres (9,350 ft) high, at the northwest end of the Rawson Mountains. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for C.E. Fuller, storekeeper with United States Navy Squadron VX-6 on Operation Deep Freeze 1966 and 1967.[3]
Mount Wyatt
86°46′S 154°00′W / 86.767°S 154.000°W. A prominent flat-topped mountain, 2,930 metres (9,610 ft) high, standing 3 nautical miles (5.6 km; 3.5 mi) west of Mount Verlautz in the Rawson Mountains. Discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn and named by Rear Admiral Byrd for Jane Wyatt, a friend of Richard S. Russell, Jr., a member of that party. [4]
Mount Verlautz
86°46′S 153°00′W / 86.767°S 153.000°W. A mountain 2,490 metres (8,170 ft) high standing just north of the mouth of Poulter Glacier in the southeast end of the Rawson Mountains. Named by US-ACAN for Major Sidney J. Verlautz, United States Army Transportation Corps, who served as logistics research officer on the staff of the Commander, United States Naval Support Force, Antarctica.[5]
Features to the south
Features south of the Poulter Glacier, which drains east into Scott Glacier, include:
Mount Innes-Taylor
86°51′S 154°27′W / 86.850°S 154.450°W. A mountain, 2,730 metres (8,960 ft) high, standing 1 nautical mile (1.9 km; 1.2 mi) north of Mount Saltonstall at the south side of Poulter Glacier. Discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and named by Byrd for Capt. Alan Innes-Taylor who served with the expedition as chief of trail operations. [6]
Mount Saltonstall
86°53′S 154°18′W / 86.883°S 154.300°W. A tabular mountain, 2,975 metres (9,760 ft) high, standing 1 nautical mile (1.9 km; 1.2 mi) south of Mount Innes-Taylor at the south side of Poulter Glacier. Discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and named by Byrd for John Saltonstall, contributor to the expedition.[7]
Mount Weaver
86°58′S 153°50′W / 86.967°S 153.833°W. A mountain, 2,780 metres (9,120 ft) high, standing 2 nautical miles (3.7 km; 2.3 mi) west of Mount Wilbur at the head of Scott Glacier. Discovered and ascended in December 1934 by members of the Byrd Antarctic Expedition geological party under Quin Blackburn. Named by them for Charles E. Weaver, professor of paleontology at the University of Washington.[8]
Mount Wilbur
86°58′S 152°37′W / 86.967°S 152.617°W. A mountain standing 2 nautical miles (3.7 km; 2.3 mi) east of Mount Weaver at the head of Scott Glacier. Discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and named by Byrd for the Hon. Curtis D. Wilbur, Secretary of the Navy, 1925-29.[9]
Features to the north
The line of mountains north of the Rawson Mountains along the west of Scott Glacier include, from south to north:
Mount Przywitowski
86°36′S 154°08′W / 86.600°S 154.133°W. A mountain, 2,770 metres (9,090 ft) high, standing at the southeast side of Holdsworth Glacier, 2.5 nautical miles (4.6 km; 2.9 mi) west of McNally Peak. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for Richard F. Przywitowski, USARP scientific leader at South Pole Station, winter 1966.[10]
McNally Peak
86°35′S 153°24′W / 86.583°S 153.400°W. A peak 2,570 metres (8,430 ft) high, standing 3.5 nautical miles (6.5 km; 4.0 mi) west of Mount Parley, near the southeast side of Holdsworth Glacier, in the Queen Maud Mountains. Named by US-ACAN for Cdr. Joseph J. McNally, United States Navy, supply officer at McMurdo Station, winter 1959; on the staff of the Commander, United States Naval Support Force, Antarctica, during United States Navy OpDFrz 1967.[11]
Mount Farley
86°35′S 152°30′W / 86.583°S 152.500°W. A conspicuous rock peak, 2,670 metres (8,760 ft) high, standing at the west side of Scott Glacier, 3 nautical miles (5.6 km; 3.5 mi) east of McNally Peak. Discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and named at that time by Byrd for the Hon. James Farley, Postmaster General of the United States.[12]
Mount Amherst
86°32′S 153°06′W / 86.533°S 153.100°W. A peak rising to 2,400 metres (7,900 ft) between Holdsworth Glacier and Scott Glacier, 3 nautical miles (5.6 km; 3.5 mi) north-northeast of McNally Peak. Mapped by USGS from surveys and United States Navy aerial photographs, 1960-64. The geology of the peak was studied in the 1978-79 season by a USARP-Arizona State University field party. Named by US-ACAN after Amherst College, Amherst, MA, alma mater of Michael F. Sheridan, a member of the field party.[13]
Mount Denauro
86°27′S 151°30′W / 86.450°S 151.500°W. Mountain, 2,340 metres (7,680 ft) high, standing on the west side of Scott Glacier, 3 nautical miles (5.6 km; 3.5 mi) south of Lee Peak. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for Ralph Denauro, aviation mechanic with United States Navy Squadron VX-6 on Operation Deep Freeze 1966.[14]
Cowie Dome
86°25′S 152°00′W / 86.417°S 152.000°W. A dome-shaped summit at the east side of Bartlett Glacier, located 2 nautical miles (3.7 km; 2.3 mi) directly west of Lee Peak. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by NZ-APC for George Donald (Don) Cowie, leader of the NZGSAE which visited the region in 1969-70.[15]
Lee Peak
86°25′S 151°35′W / 86.417°S 151.583°W. A peak along the west side of Scott Glacier, 3 nautical miles (5.6 km; 3.5 mi) north of Mount Denauro. Mapped by USGS from surveys and United States Navy air photos, 1960-64. Named by US-ACAN for Frank P. Lee, photographer on aerial flights in Antarctica during United States Navy Operation Deep Freeze 1965, 1966 and 1967.[16]
Mount Ruth
86°18′S 151°45′W / 86.300°S 151.750°W. A ridge-shaped mountain, 2,170 metres (7,120 ft) high, standing 3 nautical miles (5.6 km; 3.5 mi) west of Mount Gardiner, at the southeast side of the lower reaches of Bartlett Glacier. Discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and named at that time by R. Admiral Byrd for Ruth Black, deceased wife of Richard B. Black, expedition member who assisted with seismic, survey, and radio operations in the vicinity of Little America II.[17]
Mount Gardiner
86°19′S 150°57′W / 86.317°S 150.950°W. A ridge-like granitic mountain, 2,480 metres (8,140 ft) high, standing 3 nautical miles (5.6 km; 3.5 mi) east of Mount Ruth and just south of the junction of Bartlett and Scott Glaciers. Discovered in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn. Named by Byrd for Joseph T. Gardiner of Wellington, New Zealand, agent for the Byrd Antarctic Expedition of 1928-30 and 1933-35.[18]
References
- 1 2 Alberts 1995, p. 606.
- 1 2 Nilsen Plateau USGS.
- ↑ Alberts 1995, p. 263.
- ↑ Alberts 1995, p. 825.
- ↑ Alberts 1995, p. 780.
- ↑ Alberts 1995, p. 361.
- ↑ Alberts 1995, p. 645.
- ↑ Alberts 1995, p. 799.
- ↑ Alberts 1995, p. 812.
- ↑ Alberts 1995, p. 594.
- ↑ Alberts 1995, p. 480.
- ↑ Alberts 1995, p. 233.
- ↑ Alberts 1995, p. 16.
- ↑ Alberts 1995, p. 183.
- ↑ Alberts 1995, p. 158.
- ↑ Alberts 1995, p. 426.
- ↑ Alberts 1995, p. 639.
- ↑ Alberts 1995, p. 268.
Sources
- Alberts, Fred G., ed. (1995), Geographic Names of the Antarctic (PDF) (2 ed.), United States Board on Geographic Names, retrieved 2023-12-03 This article incorporates public domain material from websites or documents of the United States Board on Geographic Names.
- Nilsen Plateau, USGS: United States Geological Survey, retrieved 2023-12-27
- This article incorporates public domain material from websites or documents of the United States Geological Survey.