Mount Jackson | |
---|---|
Highest point | |
Elevation | 3,184 m (10,446 ft) [1] [2] [3] |
Prominence | 1,384 m (4,541 ft) [4] |
Coordinates | 71°23′S63°22′W / 71.383°S 63.367°W [2] [5] |
Geography | |
Climbing | |
First ascent | 23 November 1964 by J C Cunningham (1927–80) of BAS team. [6] |
Mount Jackson (Mount Andrew Jackson and Mount Ernest Gruening) is a mountain that dominates the upland of the southern part of the Antarctic Peninsula. It is located in Palmer Land, part of the British Antarctic Territory (with unrecognised claims by Chile and Argentina). With an elevation of 3,184 metres (10,446 ft), Mount Jackson was once thought to be the highest mountain in the Antarctic Peninsula and the British Antarctic Territory, before the true height of Mount Hope (Eternity Range) was measured. [3] Discovered by members of the United States Antarctic Service, 1939–41, it was named for Andrew Jackson, the seventh President of the United States. The first ascent of Mount Jackson was made by a team led by John Crabbe Cunningham of the British Antarctic Survey (BAS) in 1964. Mount Jackson's geology was studied in 1972 as part of the Palmer Island investigations by a team of geologists.
Mount Jackson and the Welch Mountains demarcate the central Black Coast, which is dissected by many inlets and is bounded on the west by Dyer Plateau of central Palmer Land. The two mountains rise above the ice shelf with reliefs of about 1,200–1,500 metres (3,900–4,900 ft) towards the east. They are interconnected by icefall zones forming a plateau with steep snow slopes. Mount Jackson rises from its southeast flanks, displaying a steeple summit, whilst the north flank is occupied by a vast cirque. Supraglacial moraines on the mountain's east side measure between 1–5 kilometres (0.62–3.11 mi) in length and display boulders at their distal ends.
The first topographic mapping of Mount Jackson was carried out in November 1940 by a sledge party of the United States Antarctic Service (USAS). The ground survey was facilitated by aerial photographs and aerial observations. The height was estimated at 4,200 metres (13,800 ft), and the mountain was named Mount Ernest Gruening after the Governor of the Alaska Territory at that time, Ernest Gruening. [7] USAS later renamed it Mount Jackson for the seventh President of the United States. [7] President Jackson signed the bill into law authorizing the United States Exploring Expedition of 1838–42. The expedition, led by Lt. Charles Wilkes, included exploration and surveying of the Pacific Ocean and surrounding lands, including Antarctica. [5]
In November 1947, a Falkland Islands Dependencies Survey ground party based at Stonington Island observed Mount Jackson and estimated its height at 3,050 metres (10,010 ft), considerably lower and more accurate than the first estimate in 1940. [7] After the Falkland Islands Dependencies Survey was renamed the British Antarctic Survey in 1962, a series of depots were developed, including one at Mount Jackson. [8] BAS members were successful in making many first ascents of the mountains of the Antarctic Peninsula, and John Cunningham, who served at the BAS base at Adelaide Island, was the first to climb Mount Jackson. Traveling by dog sled for 640 kilometres (400 mi), [9] his team reached the summit on 23 November 1964. [7] [6] [10]
A precise height of the summit was determined by a BAS survey party who ascended the peak during the austral summer of 1996–97. [1]
The mountain is 3,184 metres (10,446 ft) in height, [1] with a prominence of 1,384 metres (4,541 ft) and a saddle DEM of 1,901 metres (6,237 ft). [3] Mount Jackson and the Welch Mountains demarcate the central Black Coast, which is dissected by many inlets and is bounded on the west by Dyer Plateau of central Palmer Land, with elevation ranging between 2,000–3,000 metres (6,600–9,800 ft), [11] and on the west side of the central Black Coast. [12] The two mountains rise above the ice shelf with reliefs of about 1,200–1,500 metres (3,900–4,900 ft) towards the east. They are interconnected by icefall zones forming a plateau with steep snow slopes. [13] The northern part of the mountain system, which extends over 1,590 kilometres (990 mi), covers most of the Antarctic Peninsula, and Mount Jackson is its highest peak. [1] [14] [15]
Mount Jackson rises from its southeast flanks, displaying a steeple summit, [16] whilst the north flank is occupied by a vast cirque. Supraglacial moraines on the mountain's east side measure between 1–5 kilometres (0.62–3.11 mi) in length and display boulders at their distal ends. Mount Jackson and the Rowley Massif are separated by Odom Inlet. [17] Cline Glacier drains eastern Mount Jackson before arriving at Odom Inlet. [18]
Mount Jackson's geology was studied in 1972 as part of the Palmer Island investigations by a team of geologists. They identified various rock types and underlying volcanic activity. [19] The relief of the west facing slopes is gentler when compared to the eastern side, characterized by a steep rocky face. Rock weathering is intense in the area spread with scree and felsenmeer. Fresh rock formations and bedrock disintegration are noted. [13]
Nnearby features include, from north to south, Mount Van Buren, Swarson Nunatak, Davis Ridge and Musson Nunatak. [20]
71°18′S63°30′W / 71.300°S 63.500°W . The prominent mountain 3 nautical miles (5.6 km; 3.5 mi) north-northwest of Mount Jackson, at the east side of the Dyer Plateau. Mapped by the United States Geological Survey (USGS) in 1974. The name was applied by the United States Advisory Committee on Antarctic Names (US-ACAN) in association with Mount Jackson. Martin Van Buren (1782-1862) was the eighth President of the United States, 1837-41. He was Vice President, 1833-37, during the second term of President Andrew Jackson. [21]
71°25′S63°39′W / 71.417°S 63.650°W . A conspicuous nunatak, largely snow covered, located 5 nautical miles (9.3 km; 5.8 mi) southwest of Mount Jackson. Mapped by the USGS in 1974. Named by the US-ACAN for Lieutenant Commander Ronald J. Swarsen, United States Navy Reserve, Medical Officer at Byrd Station, 1971, and at the South Pole Station, 1973. [22]
71°24′S63°00′W / 71.400°S 63.000°W . A ridge of irregular shape, apparently an outlier of the Mount Jackson massif. It rises above the ice surface 6 nautical miles (11 km; 6.9 mi) east-southeast of the summit of Mount Jackson. Mapped by the USGS in 1974. Named by the US-ACAN for Brent L. Davis, USARP biologist at Palmer Station, 1971, and in the Antarctic Peninsula area, 1974-75 season. [23]
71°31′S63°27′W / 71.517°S 63.450°W . A pyramidal nunatak standing 10 nautical miles (19 km; 12 mi) south of Mount Jackson, at the east margin of the Dyer Plateau. Mapped by the USGS in 1974. Named by the US-ACAN for John M. Musson, PH2, United States Navy, photographer and member of the cartographic aerial mapping crew in LC-130 aircraft of Squadron VXE-6, 1968-69. [24]
The Behrendt Mountains is a group of mountains, 20 nautical miles long, aligned in the form of a horseshoe with the opening to the southwest, standing 7 nautical miles southwest of the Merrick Mountains in Ellsworth Land, Antarctica.
The Merrick Mountains are a cluster of mountains, 8 nautical miles long, standing 7 nautical miles northeast of the Behrendt Mountains in Ellsworth Land, Antarctica.
The Eternity Range is a range of mountains 28 nautical miles long, rising to 3,239 metres (10,627 ft), and trending north–south approximately in the middle of the Antarctic Peninsula. The range is divided into three main mountain blocks, the major summits in each from north to south being Mounts Faith, Hope and Charity.
Aitkenhead Glacier is a 10 nautical miles long glacier flowing east-southeast from the Detroit Plateau, Graham Land, into Prince Gustav Channel.
The Helliwell Hills are a group of rocky hills and low mountains about 18 miles (29 km) long and 9 miles (14 km) wide in the Usarp Mountains of North Victoria Land, Antarctica.
The Latady Mountains are a group of mountains rising west of Gardner Inlet and between Wetmore Glacier and Ketchum Glacier, in southeastern Palmer Land, Antarctica.
The Anderson Hills are an irregular group of hills, ridges and peaks between Mackin Table and the Thomas Hills in the Patuxent Range, Pensacola Mountains, Antarctica.
The Carey Range is a mountain range, about 35 nautical miles long and 5 nautical miles wide with peaks rising to 1,700 metres (5,600 ft), between Mosby Glacier and Fenton Glacier in southeast Palmer Land, Antarctica.
Condor Peninsula is a mountainous, ice-covered peninsula, 30 nautical miles long and 10 to 15 nautical miles wide, between Odom Inlet and Hilton Inlet on the east coast of Palmer Land, Antarctica.
Welch Mountains is a group of mountains that dominate the area, the highest peak rising to 3,015 metres (9,892 ft), located 25 nautical miles north of Mount Jackson on the east margin of the Dyer Plateau of Palmer Land, Antarctica
The Werner Mountains are a group of mountains located just west-southwest of New Bedford Inlet and between the Meinardus Glacier and Bryan Glacier, in Palmer Land, Antarctica.
The Dana Mountains are a group of mountains just northwest of New Bedford Inlet, bounded by Mosby Glacier on the north and Haines Glacier and Meinardus Glacier on the south, in Palmer Land, Antarctica.
Kvinge Peninsula is a snow-covered peninsula at the north side of Palmer Inlet terminating in Cape Bryant, on the east coast of Palmer Land, Antarctica.
The Gutenko Mountains are a large, scattered group of hills, nunataks and small mountains at the south end of Dyer Plateau in central Palmer Land, Antarctica. The feature includes the Elliott Hills, the Rathbone Hills, the Guthridge Nunataks and the Blanchard Nunataks.
The Playfair Mountains are a group of mountains between Swann Glacier and Squires Glacier in southeast Palmer Land, Antarctica.
The Eland Mountains are a range of mountains which rise above 2,440 metres (8,010 ft) and extend about 20 nautical miles in a northeast–southwest direction along the south side of Clifford Glacier, on the east coast of Palmer Land, Antarctica.
The Goodenough Glacier is a broad sweeping glacier to the south of the Batterbee Mountains, flowing from the west shore of Palmer Land, Antarctica, into George VI Sound and the George VI Ice Shelf.
Hilton Inlet is an ice-filled inlet, 12 nautical miles wide, which recedes about 22 nautical miles west from its entrance between Cape Darlington and Cape Knowles, along the east coast of Palmer Land, Antarctica.
The Lyon Nunataks are a group of nunataks lying west of the Grossman Nunataks and 30 nautical miles northwest of the Behrendt Mountains, in Ellsworth Land, Antarctica. They include Grossenbacher Nunatak, Holtet Nunatak, Christoph Nunatak and Isakson Nunatak.
The Columbia Mountains are a group of largely bare rock peaks, ridges and nunataks located near the east margin of the Dyer Plateau, 20 nautical miles south-east of the Eternity Range, in Palmer Land, Antarctica.
Footnote (14) from site: Elevation from American Alpine Journal (1999). GNIS offers elevation of 3050m.
Ascent of the highest mountain in the entire Peninsula, Mount Jackson at 3,184 metres (10,446 ft) well to the south in remote Palmer Land, fell to the Scot, John Cunningham, in 1964
Of the many young mountaineers that have served at the BAS stations over the years, space allows mention of only two. J. C. Cunningham (1927–80) … on 23 November 1964 he led the first ascent of Mount Jackson, Palmer Land 3,180 metres (10,430 ft); the highest peak in the BAT.
This article incorporates public domain material from websites or documents of the United States Geological Survey .
Media related to Mount Jackson at Wikimedia Commons