Cape Kerr
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Cape Kerr
Cape Kerr () is a high snow-covered cape at the north side of Barne Inlet, the terminus of Byrd Glacier at the west side of the Ross Ice Shelf, Antarctica. It was discovered by the British National Antarctic Expedition (1901–1904) and named for Admiral of the Fleet, Lord Walter Kerr Admiral of the Fleet Lord Walter Talbot Kerr, (28 September 1839 – 12 May 1927) was a Royal Navy officer. After taking part in the Crimean War and then the Indian Mutiny, he supervised the handover of Ulcinj to Montenegro to allow Montenegro ..., one of the Sea Lords who lent his assistance to the expedition. References Headlands of the Ross Dependency Hillary Coast {{RossDependency-geo-stub ...
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Cape (geography)
In geography, a cape is a headland or a promontory of large size extending into a body of water, usually the sea.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, p. 80. . A cape usually represents a marked change in trend of the Coast, coastline, often making them important landmarks in sea navigation. This also makes them prone to natural forms of erosion, mainly tidal actions, which results in them having a relatively short geological lifespan. Capes can be formed by glaciers, volcanoes, and changes in sea level. Erosion plays a large role in each of these methods of formation. List of some well-known capes Gallery File:Cape Cornwall.jpg, Cape Cornwall, England File:Nasa photo cape fear.jpg, Satellite image of Cape Fear, North Carolina File:Cape McLear, Malawi (2499273862).jpg, Cape MacLear, Malawi File:Cape horn.png, Map depicting Cape Horn at the southernmost portion of South America File:Spain.Santander.Cabo.Mayor.jpeg, Photograph o ...
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Barne Inlet
Barne Inlet () is a reentrant (an inlet formed by two spurs of land) on the west side of the Ross Ice Shelf, on the coast of Antarctica. It lies between Cape Kerr and Cape Selborne. It is about wide, and is occupied by the lower part of Byrd Glacier. It was discovered by the British National Antarctic Expedition (1901–1904) and named for Lieutenant Michael Barne, Royal Navy, a member of the expedition, who with Sub-Lieutenant George Mulock Captain George Francis Arthur Mulock, DSO, RN, FRGS (7 February 1882 – 26 December 1963) was an Anglo-Irish Royal Navy officer, cartographer and polar explorer who participated in an expedition to the Antarctic regions: the Discovery Expedi ... mapped the coastline this far south in 1903. References Inlets of Antarctica Hillary Coast {{RossDependency-geo-stub ...
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Byrd Glacier
The Byrd Glacier is a major glacier in Antarctica, about long and wide, draining an extensive area of the polar plateau and flowing eastward between the Britannia Range and Churchill Mountains to discharge into the Ross Ice Shelf at Barne Inlet. Its valley below the glacier used to be recognised as one of the lowest points not to be covered by water on Earth (assuming ice doesn't count as water), reaching below sea level. It was named by the NZ-APC after Rear Admiral Byrd, US Navy Antarctic explorer. On the south side of Byrd Glacier is Blake Massif. See also * Glaciology * Ice stream * List of Antarctic ice streams * List of glaciers in the Antarctic * List of places in Antarctica below sea level ** Denman Glacier Denman Glacier is a glacier wide, descending north some , which debouches into the Shackleton Ice Shelf east of David Island, Queen Mary Land. It was discovered in November 1912 by the Western Base party of the Australasian Antarctic Expedition ... Referen ...
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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 Januar ...
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British National Antarctic Expedition
The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–1843). Organized on a large scale under a joint committee of the Royal Society and the Royal Geographical Society (RGS), the new expedition carried out scientific research and geographical exploration in what was then largely an untouched continent. It launched the Antarctic careers of many who would become leading figures in the Heroic Age of Antarctic Exploration, including Robert Falcon Scott who led the expedition, Ernest Shackleton, Edward Wilson, Frank Wild, Tom Crean and William Lashly. Its scientific results covered extensive ground in biology, zoology, geology, meteorology and magnetism. The expedition discovered the existence of the only snow-free Antarctic valleys, which contains the longest river of Antarctica. Further ach ...
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Lord Walter Kerr
Admiral of the Fleet Lord Walter Talbot Kerr, (28 September 1839 – 12 May 1927) was a Royal Navy officer. After taking part in the Crimean War and then the Indian Mutiny, he supervised the handover of Ulcinj to Montenegro to allow Montenegro an outlet to the sea in accordance with the terms of the Treaty of Berlin. He became Flag Captain to the Commander-in-Chief, Channel Squadron and then Commander-in-Chief, Mediterranean Fleet. He went on to be Second-in-Command of the Mediterranean Fleet, then Commander-in-Chief of the Channel Squadron and finally became First Naval Lord. In that capacity he presided over a period of continued re-armament in the face of German naval expansion but was unceasingly harassed by Admiral Sir John Fisher. Early career Born the fourth son of John Kerr, 7th Marquess of Lothian and Lady Cecil Chetwynd Talbot. Kerr was educated at Radley College and joined the first-rate HMS ''Prince Regent'' as a naval cadet in August 1853.Heathcote, p. 143 He ...
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Sea Lord
Sea lord(s) or Sealord(s) may refer to: Military * First Sea Lord, the military head of the Naval Service of the United Kingdom * Second Sea Lord, the deputy of the First Sea Lord * Sea lords, senior members of the British Board of Admiralty from 1628 to 1964 * Operation Sealords, a military operation during the Vietnam War Other * ''Sea Lord'', a 1989 novel by Bernard Cornwell. * Sealord, a brand of canned tuna campaigned against by Greenpeace Aotearoa New Zealand * Sealord deal, a fisheries agreement between Māori and the New Zealand Government as part of the Treaty of Waitangi claims and settlements * Sealord of Braavos, a ruler in the fantasy world of ''A Song of Ice and Fire'' * Sealord Hotel, a hotel in the Indian city of Kochi * Sealords, a student society among the Confraternities in Nigeria * Flensburg Sealords, an American football team in Germany See also * List of water deities A water deity is a deity in mythology associated with water or various bodies of wat ...
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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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