Seal Nunataks
Seal Nunataks is located in Antarctica
Seal Nunataks
Seal Nunataks
Highest point
Elevation368 m (1,207 ft)Murdoch Nunatak [1]
Coordinates65°07′30″S 60°00′00″W / 65.12500°S 60.00000°W / -65.12500; -60.00000[2]
Geology
Mountain typevolcanic vent

The Seal Nunataks are a group of 16 islands called nunataks emerging from the Larsen Ice Shelf east of Graham Land, Antarctic Peninsula. The Seal Nunataks have been described as separate volcanic vents of ages ranging from Miocene to Pleistocene. There are unconfirmed reports of Holocene volcanic activity.

Geography and geomorphology

The Seal Nunataks are part of Graham Land and were embedded within the Larsen Ice Shelf[1] until its northern margin collapsed between 1986 and 1996,[3] rising from about 500 metres (1,600 ft) below sea level.[4] They were discovered by the Norwegian Carl Anton Larsen in December 1893,[1] who also identified them as volcanoes and named them Seal Islands.[5] The Argentina Base Aérea Teniente Benjamín Matienzo is located in the Seal Nunataks.[6]

The Seal Nunataks are part of a volcanic province in West Antarctica which extends over the Antarctic Peninsula, Marie Byrd Land and Ross Island. In the Antarctic Peninsula, Alexander Island, James Ross Island and the Seal Nunataks form this volcanic province. Alexander Island was active between 48 and 18 million years ago.[7] James Ross Island lies about 150 kilometres (93 mi) northeast of the Seal Nunataks.[4]

The Seal Nunataks volcanic group contains at least sixteen volcanic cones,[4] the largest of which is 368 metres (1,207 ft) high Murdoch Nunatak.[1] From north to south they are Lindenberg island, Larsen Nunatak, Evensen Nunatak, Dallmann and Murdoch Nunatak, Akerlundh, Bruce and Bull Nunatak, Donald, Pollux and Christensen Nunatak, Arctowski and Gray Nunatak, Oceana Nunatak, Hertha Nunatak and Castor Nunatak.[2] The nunataks consist of ridges with lengths of less than 1 to 6 kilometres (0.62 to 3.73 mi) flanked with scree deposits and occasionally by primary volcanic features.[8] According to Otto Nordenskjöld in 1901-1903, Christensen Nunatak features a crater.[5] Castor, Christensen and Hertha are the only vents which show evidence of subaerial activity in form of lava flows; elsewhere the nunataks are constructed by hyaloclastite and pillow lavas which form beneath ice.[1] The volcanoes appear to align along northwest-striking lines.[4]

Geology

The Antarctic Peninsula was a site of subduction from about 200 million years ago until 4 million years ago, when a number of spreading ridges collided with the subduction zone starting from 50 million years ago at Alexander Island and caused it to cease. The volcanic arc became inactive; however volcanic activity continued in different form over the entire peninsula.[7] In the case of the Seal Nunataks, volcanism commenced immediately after subduction had ceased and was probably facilitated by the presence of fracture zones in the already subducted slab.[9] Alternatively, the development of a slab window may have aided in the onset of volcanism.[10]

There is only little evidence of the basement at Robertson Island, where sediments of Cretaceous age crop out.[2] The tectonic structure in the area appears to be a rift bordered by Robertson Island in the south, the Larsen Rift.[11]

Composition

The Seal Nunataks consist of basalt,[2] basalt which contains clinopyroxene, olivine and plagioclase.[12] Xenoliths consisting of lherzolite and spinel have been found at Seal Nunataks.[1] Their geochemistry implies that the magmas are primitive mantle-derived melts which underwent only a little fractional crystallization.[13]

Eruptive history

Potassium-argon dating has yielded ages between 4 million years ago and "recent" for the rocks in the volcanic field, but the reliability of the dates decreases the younger they are. Pillow lavas are usually about 1.5 million years old while subaerial activity occurred 700,000 years ago.[1] The youngest dates were obtained on Donald and Gray, the dates being less than 200,000 years ago.[4] Glacial erratics on some of the nunataks imply that they were covered with glaciers in the past.[14]

The discoverer Captain Larsen observed volcanic activity on Christensen Nunatak and Lindenberg Island, but the reliability of these reports is considered to be unclear.[1] Fumaroles have been observed on Christensen, Dallman and Murdoch, and eruptions were reported on the last two in 1982.[4] This activity consisted of the possible formation of lava flows and a pyroclastic cone, respectively.[15]

See also

References

  1. 1 2 3 4 5 6 7 8 Hole 1990, p. 151.
  2. 1 2 3 4 Hole 1990, p. 152.
  3. ↑ Rott, Helmut; Rack, Wolfgang; Nagler, Thomas; Skvarca, Pedro (January 1998). "Climatically induced retreat and collapse of northern Larsen Ice Shelf, Antarctic Peninsula". Annals of Glaciology. 27: 89. Bibcode:1998AnGla..27...86R. doi:10.3189/S0260305500017262.
  4. 1 2 3 4 5 6 Oliver, James & Jago 1983, p. 335.
  5. 1 2 Oliver, James & Jago 1983, p. 334.
  6. ↑ Fontana, Pablo Gabriel (1 January 2018). "A hut too far: history of the Argentine Ventimiglia shelter on Peter I Øy". Polar Research. 37 (1): 4. doi:10.1080/17518369.2018.1547043.
  7. 1 2 Hole 1990, p. 150.
  8. ↑ Smellie & Hole 1997, p. 630.
  9. ↑ Hole 1990, p. 164.
  10. ↑ Lawver, Lawrence A.; Keller, Randall A.; Fisk, Martin R.; Strelin, Jorge A. (1995). "Bransfield Strait, Antarctic Peninsula Active Extension behind a Dead Arc". Backarc Basins. Springer, Boston, MA. pp. 315–342. doi:10.1007/978-1-4615-1843-3_8. ISBN 978-1-4613-5747-6.
  11. ↑ Oliver, James & Jago 1983, p. 337.
  12. ↑ Hole 1990, p. 152,153.
  13. ↑ Hole 1990, p. 153.
  14. ↑ Smellie & Hole 1997, p. 629.
  15. ↑ Oliver, James & Jago 1983, p. 336.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.