Scott Island in the context of "Stack (geology)"

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⭐ Core Definition: Scott Island

Scott Island is a small uninhabited island of volcanic origin in the Ross Sea, Southern Ocean, 505 kilometres (310 mi) northeast of Cape Adare, the northeastern extremity of Victoria Land, Antarctica. It is 565 metres (618 yd) long north–south, and between 130 metres (140 yd) and 340 metres (370 yd) wide, reaching a height of 54 metres (177 ft) and covering an area of 4 hectares (9.9 acres). Haggits Pillar, a stack reaching 62 metres (203 ft) in height and measuring 50 metres (55 yd) in diameter, yielding an area of less than 0.2 hectares (0.5 acres), is located 250 metres (270 yd) west of the island. The island has two small coves with beaches, the rest of the island being surrounded by high cliffs. One of the coves is on the northeastern coast and the other opposite Haggitts Pillar on the western coast of the island.

The island was discovered and landed upon on 25 December 1902 by captain William Colbeck, commander of the SY Morning, the relief ship for Robert Scott's expedition. Colbeck originally planned to name the island Markham Island, after Sir Clements Markham, but later decided to name it after Scott. Haggits Pillar is named after Colbeck's mother's family name, Haggit. In 2006, a mapping expedition to the Ross Sea found the islands 2.3 kilometres (1.4 mi) north of their previously determined position.

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Scott Island in the context of Iceberg

An iceberg is a piece of fresh water ice more than 15 meters (16 yards) long that has broken off a glacier or an ice shelf and is floating freely in open water. Smaller chunks of floating glacially derived ice are called "growlers" or "bergy bits". Much of an iceberg is below the water's surface, which led to the expression "tip of the iceberg" to illustrate a small part of a larger unseen issue. Icebergs are considered a serious maritime hazard.

Icebergs vary considerably in size and shape. Icebergs that calve from glaciers in Greenland are often irregularly shaped while Antarctic ice shelves often produce large tabular (table top) icebergs. The largest iceberg in recent history, named B-15, was measured at nearly 300 by 40 kilometres (186 by 25 mi) in 2000. The largest iceberg on record was an Antarctic tabular iceberg measuring 335 by 97 kilometres (208 by 60 mi) sighted 240 kilometres (150 mi) west of Scott Island, in the South Pacific Ocean, by the USS Glacier on November 12, 1956. This iceberg was larger than Belgium.

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Scott Island in the context of Ross Dependency

The Ross Dependency is a region of Antarctica defined by a sector originating at the South Pole, passing along longitudes 160° east to 150° west, and terminating at latitude 60° south. It is claimed by New Zealand, a claim mutually accepted only by Australia, the UK, France and Norway, which are countries that also have territorial claims in Antarctica. Under the 1961 Antarctic Treaty, of which all territorial claimants are signatories, including New Zealand, all claims are held in abeyance. Article IV states: "No acts or activities taking place while the present Treaty is in force shall constitute a basis for asserting, supporting or denying a claim to territorial sovereignty in Antarctica or create any rights of sovereignty in Antarctica".

The Dependency takes its name from Sir James Clark Ross, who discovered the Ross Sea and includes part of Victoria Land, and most of the Ross Ice Shelf. Ross, Balleny, Scott and Roosevelt Islands also form part of the Dependency.

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