Cape Parr
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Cape Parr
Cape Parr () is a large snow-covered cape along the west side of the Ross Ice Shelf The Ross Ice Shelf is the largest ice shelf of Antarctica (, an area of roughly and about across: about the size of France). It is several hundred metres thick. The nearly vertical ice front to the open sea is more than long, and between hi ..., about 8 nautical miles (15 km) south of Gentile Point. Discovered by the ''Discovery'' expedition (1901–04) under Scott, who named it for Admiral Alfred Arthur Chase Parr, one of Scott's advisors who had served in Arctic exploration. Headlands of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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Ross Ice Shelf
The Ross Ice Shelf is the largest ice shelf of Antarctica (, an area of roughly and about across: about the size of France). It is several hundred metres thick. The nearly vertical ice front to the open sea is more than long, and between high above the water surface. Ninety percent of the floating ice, however, is below the water surface. Most of Ross Ice Shelf is in the Ross Dependency claimed by New Zealand. It floats in, and covers, a large southern portion of the Ross Sea and the entire Roosevelt Island located in the east of the Ross Sea. The ice shelf is named after Sir James Clark Ross, who discovered it on 28 January 1841. It was originally called "The Barrier", with various adjectives including "Great Ice Barrier", as it prevented sailing further south. Ross mapped the ice front eastward to 160° W. In 1947, the U.S. Board on Geographic Names applied the name "Ross Shelf Ice" to this feature and published it in the original U.S. Antarctic Gazetteer. In Ja ...
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Gentile Point
The Darley Hills () are a range of high, ice-covered coastal hills in the Churchill Mountains, Antarctica. Location The Darley Hills overlook the Ross Ice Shelf, and trend north–south for about between Cape Douglas and Cape Parr. To the west, they are bounded by the Skinner Saddle in the north, from which Nursery Glacier flows south and then east into the Ross Ice Shelf. Name The hills were named by the Advisory Committee on Antarctic Names for James M. Darley, chief cartographer of the National Geographic Society, 1940–63, under whose direction many important maps of Antarctica were published. Features Geographical features from north to south include: Skinner Saddle . A high, broad, snow-covered saddle between the northern part of Darley Hills and that portion of Churchill Mountains eastward of Mount Durnford. Mapped by the Northern Party of NZGSAE (1960-61) and named for D.N. Skinner, geologist with the party. Riddiford Nunatak ) A small but conspicuous nunatak ( ...
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Admiral Alfred Arthur Chase Parr
Admiral is one of the highest ranks in some navies. In the Commonwealth nations and the United States, a "full" admiral is equivalent to a "full" general in the army or the air force, and is above vice admiral and below admiral of the fleet, or fleet admiral. Etymology The word in Middle English comes from Anglo-French , "commander", from Medieval Latin , . These evolved from the Arabic () – (), “king, prince, chief, leader, nobleman, lord, a governor, commander, or person who rules over a number of people,” and (), the Arabic article answering to “the.” In Arabic, admiral is also represented as (), where () means the sea. The 1818 edition of Samuel Johnson's ''A Dictionary of the English Language'', edited and revised by the Rev. Henry John Todd, states that the term “has been traced to the Arab. emir or amir, lord or commander, and the Gr. , the sea, q. d. ''prince of the sea''. The word is written both with and without the d, in other languages, as wel ...
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Headlands Of The Ross Dependency
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the ...
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