Cape Ross
Evans Piedmont Glacier () is a broad ice sheet occupying the low-lying coastal platform between Tripp Island and Cape Archer in Victoria Land, Antarctica. Exploration and naming Evans Piedmont Glacier was circumnavigated in 1957 by the New Zealand Northern Survey Party of the Commonwealth Trans-Antarctic Expedition (CTAE), 1956–58, and was named after Petty Officer Edgar Evans, Royal Navy, of the British Antarctic Expedition, 1910–13, who was one of the South Pole Party under Captain Robert Falcon Scott, and who lost his life on the Beardmore Glacier on the return journey. Location The Evans Piedmont Glacier is on the west coast of the Ross Sea between Fry Glacier to the north and Granite Harbour to the south. Named coastal features include Tripp Bay, Tripp Island, Albrecht Penck Glacier, Depot Island, Cape Ross, Gregory Island and Cape Archer. Tripp Bay . A bay along the coast of Victoria Land formed by a recession in the ice between the Gates Piedmont Glacier and Evans ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Victoria Land
Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78th parallel south, 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It was discovered by Captain James Clark Ross in January 1841 and named after Victoria of the United Kingdom, Queen Victoria. The rocky promontory of Minna Bluff is often regarded as the southernmost point of Victoria Land, and separates the Scott Coast to the north from the Hillary Coast of the Ross Dependency to the south. History Early explorers of Victoria Land include James Clark Ross and Douglas Mawson. In 1979, scientists discovered a group of 309 Meteorite, meteorites in Antarctica, some of which were found near the Allan Hills in Victoria Land. The meteorites appeared to have undergone little change since they were formed at what scientists believe was the birth of the Solar System. In 1981, Lichen, lichens fo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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James Clark Ross
Sir James Clark Ross (15 April 1800 – 3 April 1862) was a British Royal Navy officer and explorer of both the northern and southern polar regions. In the Arctic, he participated in two expeditions led by his uncle, Sir John Ross, John Ross, and in four led by Sir William Parry, William Edward Parry: in the Antarctic, he led Ross expedition, his own expedition from 1839 to 1843. Biography Early life Ross was born in London, the son of George Ross and nephew of Sir John Ross, John Ross, under whom he entered the Royal Navy on 5 April 1812. Ross was an active participant in the Napoleonic Wars, being present at an action where HMS Briseis (1808), HMS ''Briseis'', commanded by his uncle, captured ''Le Petit Poucet'' (a French privateer) on 9 October 1812. Ross then served successively with his uncle on HMS Acteon (1805), HMS ''Actaeon'' and HMS Driver (1840), HMS ''Driver''. Arctic exploration Ross participated in John's unsuccessful first Arctic voyage in search o ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tito Peak
The Kirkwood Range () is a massive coastal mountain range in Antarctica, extending north–south between Fry Glacier and Mawson Glacier. A broad low-level platform on the seaward side of the range is occupied by the Oates Piedmont Glacier. It is south of the Prince Albert Mountains and northeast of the Convoy Range. Exploration and naming The Kirkwood Range was named by the New Zealand Northern Survey Party of the Commonwealth Trans-Antarctic Expedition (1956–58) for Captain Harry Kirkwood, Royal Navy, captain of the supply ship '' Endeavour'' during this period. Location The Kirkwood Range is just inland from the Oates Piedmont Glacier, which extends along the west coast of the Ross Sea from Mawson Glacier to the north to Fry Glacier to the south. Inland, the Convoy Range lies to the southwest, terminating in Mount Douglas at the head of the Fry Glacier. The Mawson Glacier extends to the northwest, forming near Trinity Nunatak and Jarina Nunatak. On a 1962 map, featur ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Oates Piedmont Glacier
The Mawson Glacier () is a large glacier on the east coast of Victoria Land, Antarctica, descending eastward from the Antarctic Plateau to the north of Trinity Nunatak and the Kirkwood Range, to enter the Ross Sea, where it forms the Nordenskjöld Ice Tongue. The glacier was first mapped by the British Antarctic Expedition (1907–09) and named for Douglas Mawson, the expedition physicist, who later led two other Antarctic expeditions, 1911–14, and 1929–31. Glaciology After the Last Glacial Maximum (LGM) there was dynamic retreat of the ice sheet covering the Ross Sea in the Mawson Glacier region. The glacier thinned abruptly between 7,500 and 4,500 years ago, then thinned more gradually until recently. This thinning was very similar to what happened at the Mackay Glacier to the south. Probably the ice sheet retreat and glacial ice drawdown were caused by ocean warming. Course The Mawson Glacier rises on the Antarctic Plateau. Features of the region of its head include B ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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British Antarctic Expedition, 1907–09
The ''Nimrod'' Expedition of 1907–1909, otherwise known as the British Antarctic Expedition, was the first of three expeditions to the Antarctic led by Ernest Shackleton and his second time to the Continent. Its main target, among a range of geographical and scientific objectives, was to be first to reach the South Pole. This was not attained, but the expedition's southern march reached a Farthest South latitude of 88° 23' S, just from the pole. This was by far the longest southern polar journey to that date and a record convergence on either Pole. A separate group led by Welsh Australian geology professor Edgeworth David reached the estimated location of the South magnetic pole, and the expedition also achieved the first ascent of Mount Erebus, Antarctica's second highest volcano. The expedition lacked governmental or institutional support, and relied on private loans and individual contributions. It was beset by financial problems and its preparations were hur ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Granite Harbour
Granite Harbour () is a bay in the coast of Victoria Land, Antarctica, about long, entered between Cape Archer and Cape Roberts. It was discovered and named by the British National Antarctic Expedition (BrNAE) of 1901–04 in the ''Discovery'' in January 1902, while searching for safe winter quarters for the ship. The name derives from the great granite boulders found on its shores. Features Granite Harbor extends from Cape Archer at the south tip of Evans Piedmont Glacier to Cape Roberts on the north of Wilson Piedmont Glacier. Its main inflow is Mackay Glacier, which terminates in Mackay Glacier Tongue, extending into the bay. Features to the north of this glacier include Tiger Island, Benson Glacier, Lion Island, Hunt Glacier, Dreikanter Head, Marston Glacier, Kar Plateau and Point Retreat. Features to the south include Cuff Cape, The Flatiron, Devils Punchbowl, Finger Point, New Glacier, Discovery Bluff, Avalanche Bay, Couloir Cliffs, First View Point and Cape Roberts. ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Fry Glacier
Fry Glacier () is a glacier draining the slopes at the northeast corner of the Convoy Range and flowing along the south end of the Kirkwood Range into Tripp Bay, Victoria Land, Antarctica. It was first charted by the British Antarctic Expedition, 1907–09, and named for A.M. Fry, a contributor to the expedition. Location Fry Glacier rises to the west of the north end of the Convoy Range, south of the Kirkwood Range. At its head Fry Saddle drops down from the mouth of the Chattahoochee Glacier, between Mount Naab and Mount Douglas. The Towle Glacier joins the Fry Glacier from the west, to the north of Elkhorn Ridge. The Northwind Glacier and Atka Glacier join the head of Fry Glacier from the south. Fry Glacier flows past Shoulder Mountain to the north to enter Tripp Bay on the Ross Sea. Albrecht Penck Glacier converges with Fry Glacier in Tripp Bay. Features Tributaries and features of the terrain the glacier flows through include: Fry Saddle . Narrow ice saddle at ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ross Sea
The Ross Sea is a deep bay of the Southern Ocean in Antarctica, between Victoria Land and Marie Byrd Land and within the Ross Embayment, and is the southernmost sea on Earth. It derives its name from the British explorer James Clark Ross who visited this area in 1841. To the west of the sea lies Ross Island and Victoria Land, to the east Roosevelt Island and Edward VII Peninsula in Marie Byrd Land, while the southernmost part is covered by the Ross Ice Shelf, and is about from the South Pole. Its boundaries and area have been defined by the New Zealand National Institute of Water and Atmospheric Research as having an area of . The circulation of the Ross Sea is dominated by a wind-driven ocean gyre and the flow is strongly influenced by three submarine ridges that run from southwest to northeast. The circumpolar deep water current is a relatively warm, salty and nutrient-rich water mass that flows onto the continental shelf at certain locations. The Ross Sea is covered ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Beardmore Glacier
The Beardmore Glacier in Antarctica is one of the largest valley glaciers in the world, being long and having a width of . It descends about from the Antarctic Plateau to the Ross Ice Shelf and is bordered by the Commonwealth Range of the Queen Maud Mountains on the eastern side and the Queen Alexandra Range of the Central Transantarctic Mountains on the western. Its mouth is east of the Lennox-King Glacier. It is northwest of the Ramsey Glacier. Early exploration The glacier is one of the main passages through the Transantarctic Mountains to the great polar plateau beyond, and was one of the early routes to the South Pole despite its steep upward incline. The glacier was discovered and climbed by Ernest Shackleton during his Nimrod Expedition, ''Nimrod'' Expedition of 1908. Although Shackleton turned back at latitude 88° 23' S, just from the South Pole, he established the first proven route towards the pole and, in doing so, became the first person to set foot up ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |