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Ross Island

Orthographic projection centered over Ross Island

Ross Island (77°30′S 168°00′E / 77.500°S 168.000°E / -77.500; 168.000) is an island in Antarctica lying on the east side of McMurdo Sound and extending 43 nautical miles (80 km; 49 mi) from Cape Bird on the north to Cape Armitage on the south, and a like distance from Cape Royds on the west to Cape Crozier on the east. The island is entirely volcanic.Mount Erebus, 3,795 metres (12,451 ft), near the center, is an active volcano.Mount Terror, 3,230 metres (10,600 ft), about 20 nautical miles (37 km; 23 mi) eastward, is an extinct volcano. Mount Bird rises to 1,765 metres (5,791 ft) just south of Cape Bird.[1]Ross Island lies within the boundary of Ross Dependency, an area of Antarctica claimed by New Zealand.

History

Discovery

This area was discovered by Sir James Clark Ross in 1841, but he thought it formed part of the mainland of Victoria Land. It was determined to be an island and named by the British National Antarctic Expedition (1901-04), led by Robert Falcon Scott, for Sir James Clark Ross.[1]Ross Island was the base for many of the early expeditions to Antarctica. It is the southernmost island reachable by sea. Huts built by Scott's and Shackleton's expeditions are still standing on the island, preserved as historical sites.

Today Ross Island is home to New Zealand's Scott Base and to the largest Antarctic settlement, the United States Antarctic Program's McMurdo Station. Greenpeace established World Park Base on the island and ran it for five years, from 1987 to 1992.

Geography

Map of Ross Island

Because of the persistent presence of the ice sheet, the island is sometimes taken to be part of the Antarctic mainland. Only a small portion of the island is free of ice and snow. Its area is 2,460 square kilometres (950 sq mi). Despite its relatively small size, Ross Island is the world's 6th highest island and the highest island in Antarctica. It has the highest average elevation of any island.[citation needed]

Major volcanic peaks include, from west to east, Mount Bird, Mount Erebus, Mount Terra Nova and Mount Terror.[2]Mount Erebus is (3,794 metres (12,448 ft)) is the planet's southernmost active volcano. The dormant volcano Mount Terror (3,230 metres (10,600 ft)), is the second highest on the island. They were named by Captain James Ross after his ships HMS Erebus and HMS Terror. The third highest elevation is Mount Bird, with Shell Glacier and Endeavour Piedmont Glacier on its slopes.[3]

The Erebus hotspot is thought to be responsible for the island's volcanic activity.[4]

Stations and huts

The base of the Hut Point Peninsula is home to McMurdo Station and Scott Base.Scott's Hut is further north on the west coast, at Cape Evans. North of this at Cape Royds is Shackleton's Hut. Finally, the Cape Bird Hut is just south of Cape Bird.[2]

Capes and peninsulas

Aerial view of the tip of Hut Point Peninsula with McMurdo Station on the near side and Scott Base on the far side

Capes and peninsulas include, clockwise from the south, the Hut Point Peninsula, Cape Evans, Cape Royds, Cape Bird, Cape Tennyson, Cape Crozier and Cape MacKay.[2]

Major bays

Large bays include Erebus Bay, Wohlschlag Bay, Lewis Bay and Windless Bight.[2]

Major glaciers

Barne Glacier around 1910

Major glaciers entering the sea or ice cap around the island include, clockwise from the south, Erebus Glacier and the Erebus Glacier Tongue, Barne Glacier, Shell Glacier, Terror Glacier and Aurora Glacier.[2]

See also

References

  1. ^ a b Alberts 1995, p. 631.
  2. ^ a b c d e Ross Island USGS.
  3. ^ LeMasurier & Thomson 1990.
  4. ^ Morgan & Phipps Morgan 2007, pp. 26–27.
  5. ^ McMurdo Station NSF.
  6. ^ Antarctic Station Catalogue, pp. 92–93.
  7. ^ Scott’s Terra Nova Hut AHF.
  8. ^ Ernest Shackleton’s Hut AHT.
  9. ^ Varetto 2021.
  10. ^ Alberts 1995, p. 356.
  11. ^ Alberts 1995, p. 227.
  12. ^ Alberts 1995, p. 634.
  13. ^ Alberts 1995, p. 67.
  14. ^ Alberts 1995, p. 738.
  15. ^ Alberts 1995, p. 164.
  16. ^ Alberts 1995, p. 452.
  17. ^ a b Alberts 1995, p. 224.
  18. ^ Alberts 1995, p. 821.
  19. ^ Alberts 1995, pp. 430–431.
  20. ^ Alberts 1995, p. 818.
  21. ^ Alberts 1995, p. 669.
  22. ^ Alberts 1995, p. 46.
  23. ^ Alberts 1995, p. 740.
  24. ^ Alberts 1995, p. 34.

Sources

Public Domain This article incorporates public domain material from websites or documents of the United States Geological Survey.

External links