Antarctic Protected Area

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An Antarctic Protected Area is an area protected under the Antarctic Treaty System. [1] There are three types of Protected Areas under this system:

Guidelines for scientists and other visitors have been developed to protect these areas. [1]

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The Protocol on Environmental Protection to the Antarctic Treaty, also known as the Madrid Protocol, is a complementary legal instrument to the Antarctic Treaty signed in Madrid on 4 October 1991. It entered into force on 14 January 1998.

<span class="mw-page-title-main">Agreed Measures for the Conservation of Antarctic Fauna and Flora</span> Set of environmental protection measures

The Agreed Measures for the Conservation of Antarctic Fauna and Flora is a set of environmental protection measures which were accepted at the third Antarctic Treaty Consultative Meeting in Brussels in 1964. The Agreed Measures were formally in force as part of the Antarctic Treaty System from 1982 to 2011, when they were withdrawn as the principles were now entirely superseded by later agreements such as the 1991 Protocol on Environmental Protection to the Antarctic Treaty. The Agreed Measures were adopted in order to further international collaboration within the administration of the Antarctic Treaty System and promote the protection of natural Antarctic ecological systems while enabling scientific study and exploration.

<span class="mw-page-title-main">Odbert Island</span> Island in Antarctica

Odbert Island is a rocky island, 2.4 km (1.5 mi) long, between Ardery Island and Robinson Ridge in the Windmill Islands of Antarctica.

<span class="mw-page-title-main">Cape Royds</span> Landform on Ross Island, Antarctica

Cape Royds is a dark rock cape forming the western extremity of Ross Island, facing on McMurdo Sound, Antarctica. It was discovered by the British National Antarctic Expedition (BrNAE) (1901–1904) and named for Lieutenant Charles Royds, Royal Navy, who acted as meteorologist on the expedition. Royds subsequently rose to become an Admiral and was later Commissioner of the Metropolitan Police, London. The cape is the site of Shackleton's Hut, the expedition camp of the British Antarctic Expedition, 1907–09.

<span class="mw-page-title-main">Cape Crozier</span> Headland of Antarctica

Cape Crozier is the most easterly point of Ross Island in Antarctica. It was discovered in 1841 during James Clark Ross's polar expedition of 1839 to 1843 with HMS Erebus and HMS Terror, and was named after Commander Francis Crozier, captain of HMS Terror, one of the two ships of Ross' expedition.

<span class="mw-page-title-main">Murray Monolith</span> Monolith of Antarctica

Murray Monolith is a detached part of Torlyn Mountain in Mac.Robertson Land, Antarctica. It is a steep massif of metasedimentary gneiss and granitic origin, with the adjacent coastline consisting of 40 m high ice cliffs. The monolith is dome-shaped with steep sides, rising to a seaward summit of 339 m and an inland summit of 363 m at Torlyn Mountain.

<span class="mw-page-title-main">Svarthamaren Mountain</span> Mountain of Antarctica

Svarthamaren Mountain is a prominent ice-free mountain or large nunatak on the east side of the mouth of Vestreskorve Glacier in the Muhlig-Hofmann Mountains of Queen Maud Land, Antarctica. It was mapped from surveys and aerial photographs by the Norwegian Antarctic Expedition (1956–60) and named Svarthamaren.

<span class="mw-page-title-main">Coppermine Peninsula</span>

Coppermine Peninsula is the rugged, rocky promontory forming the northwest extremity of Alfatar Peninsula and Robert Island in the South Shetland Islands, Antarctica. It lies between the English Strait to the west and Carlota Cove to the east. It is 1.7 km long, 500 m wide and rising to 105 m.

Balham Valley is an ice-free valley] between the Insel Range and the Apocalypse Peaks, in Victoria Land, Antarctica.

Barwick Valley is an ice-free valley north of Apocalypse Peaks, extending from Webb Glacier to Victoria Valley in Victoria Land, Antarctica. A large part of the valley has been designated an Antarctic Specially Protected Area because of its pristine condition.

Davis Valley is an ice-free valley just east of Floridas Ridge in north-east Dufek Massif, in the Pensacola Mountains, Antarctica.

Mule Peninsula is an irregularly shaped rocky peninsula between Ellis Fjord and Krok Fjord in the southern part of the Vestfold Hills of Princess Elizabeth Land, Antarctica. It was mapped from aerial photographs taken by the Lars Christensen Expedition of 1936–37 and named Breidnesmulen by Norwegian cartographers. Mule Peninsula is an adaptation of the original Norwegian name by the Antarctic Names Committee of Australia.

Mount Monique is a mountain, about 600 m high, with a prominent rocky north face and ice-covered south slopes, at the western end of the Marion Nunataks on the north coast of Charcot Island in the east Bellinghausen Sea of Antarctica.

Mount Harding is the largest mountain in the Grove Mountains of Antarctica, in the south-central part of the range and about 4 nautical miles (7 km) west of Gale Escarpment. It was mapped by the Australian National Antarctic Research Expeditions (1956–60) from aerial photographs, and was named by the Antarctic Names Committee of Australia for N.E. Harding, a topographic draftsman with the Division of National Mapping, Australian Department of National Development, who contributed substantially to the production of Antarctic maps.

Linnaeus Terrace is a rock terrace on the north side of Oliver Peak in the Asgard Range of Victoria Land, Antarctica. It is protected under the Antarctic Treaty System as Antarctic Specially Protected Area No.138 because it is one of the richest known sites for the cryptoendolithic communities that colonise the Beacon Sandstone.

Haswell Island is the largest of the Haswell Islands, lying off the coast of Antarctica, about 3 kilometres (1.5 nmi) north of Mabus Point in Queen Mary Land. It was discovered by the Western Base Party of the Australasian Antarctic Expedition, 1911–14, under Mawson, and named by him for Professor William A. Haswell, a zoologist at Sydney University and a member of the expedition's Advisory Committee.

Hawker Island is an irregularly shaped island about 2 km (1.2 mi) long, lying some 7 km south-west of Davis Station between Mule Island and Mule Peninsula, Vestfold Hills, in the eastern part of Prydz Bay, Antarctica. It was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition, 1936–37. It was remapped by the Australian National Antarctic Research Expeditions (1957–58) and named after Alan Charles Hawker, a radio supervisor at Davis Station in 1957.

Mount Martine is a massive mountain, about 800 metres (2,600 ft) high, with a prominent rocky north face and ice-covered south slopes, overlooking the north shore of Charcot Island, south of Cheesman Island, in the east Bellinghausen Sea of Antarctica.

<span class="mw-page-title-main">Marion Nunataks</span>

The Marion Nunataks are a small group of nunataks rising to about 600 m (2,000 ft) on Charcot Island, in the eastern Bellinghausen Sea of Antarctica. They form a 12 km chain of rocky outcrops on the mid-north coast of the island, stretching from Mount Monique at the western end to Mount Martine in the east.

A Historic Site or Monument (HSM) is a protected location of historic interest on the continent of Antarctica, or on its adjacent islands. The list of historic sites was first drawn up in 1972, and has since expanded to cover 95 sites, with the most recent listed in 2021. Five sites have been removed from the list for various reasons.

References

  1. 1 2 Antarctic Protected Areas explained by the Antarctic Treaty System