Mount Iveagh
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Mount Iveagh
Mount Iveagh () is a broad mountain in the Supporters Range of Antarctica, overlooking the east side of Mill Glacier northwest of Mount White. This peak is located between Keltie Glacier and Mill Glacier, on the east side of Beardmore Glacier. It was discovered by the British Antarctic Expedition, 1907–09, and named for Edward Guinness, 1st Earl of Iveagh, of the firm of Guinness Guinness () is an Irish dry stout that originated in the brewery of Arthur Guinness at St. James's Gate, Dublin, Ireland, in 1759. It is one of the most successful alcohol brands worldwide, brewed in almost 50 countries, and available in ove ..., who helped finance the expedition. References Mountains of the Ross Dependency Queen Maud Mountains Dufek Coast {{DufekCoast-geo-stub ...
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Supporters Range
The Supporters Range () is a rugged range in the Queen Maud Mountains of Antarctica. It is long, bordering the eastern side of Mill Glacier, from Keltie Glacier in the north to Mill Stream Glacier in the south. So named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) because several peaks of the range are named after supporters of Ernest Shackleton's British Antarctic Expedition (1907–09). Location The northern point of the range lies between Keltie Glacier, flowing from the east, and Mill Glacier flowing from the south and converging with Beardmore Glacier. Ranfurly Point is its northernmost point. Laird Glacier flows from the range in Keltie Glacier, and Snakeskin Glacier flows along the northeast side of the range into Keltie Glacier. Other features in the north include Scully Terrace, Mount Kinsey and Mount Westminster. Features further south include Mount Iveagh, Mount Judd, Mount White and Mount Henry Lucy. The Jensen Glacier flows along t ...
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Mill Glacier
Mill Glacier is a tributary glacier, wide, flowing northwest between the Dominion Range and the Supporters Range into Beardmore Glacier, Antarctica. It was discovered by the British Antarctic Expedition, 1907–09, and named for Hugh Robert Mill, a British geographer and Antarctic historian. See also * List of glaciers in the Antarctic There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. Th ... References Glaciers of Dufek Coast {{DufekCoast-glacier-stub ...
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Mount White (Antarctica)
The Supporters Range () is a rugged range in the Queen Maud Mountains of Antarctica. It is long, bordering the eastern side of Mill Glacier, from Keltie Glacier in the north to Mill Stream Glacier in the south. So named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) because several peaks of the range are named after supporters of Ernest Shackleton's British Antarctic Expedition (1907–09). Location The northern point of the range lies between Keltie Glacier, flowing from the east, and Mill Glacier flowing from the south and converging with Beardmore Glacier. Ranfurly Point is its northernmost point. Laird Glacier flows from the range in Keltie Glacier, and Snakeskin Glacier flows along the northeast side of the range into Keltie Glacier. Other features in the north include Scully Terrace, Mount Kinsey and Mount Westminster. Features further south include Mount Iveagh, Mount Judd, Mount White and Mount Henry Lucy. The Jensen Glacier flows along the ...
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Keltie Glacier
Keltie Glacier is a large Antarctic glacier, long, draining from Pain Névé southwest around the southern extremity of the Commonwealth Range, and then northwest to enter Beardmore Glacier at Ranfurly Point. It was discovered by the British Antarctic Expedition, 1907–09, under Ernest Shackleton, who named it for Sir John Scott Keltie Sir John Scott Keltie (29 March 1840 – 12 January 1927) was a Scottish geographer, best known for his work with the Royal Geographical Society. History Keltie was born in Dundee and attended school in Perth. He matriculated at the Unive ..., Secretary of the Royal Geographical Society, 1892–1915. See also * List of glaciers in the Antarctic References Glaciers of Dufek Coast Queen Maud Mountains {{DufekCoast-glacier-stub ...
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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. 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 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 upon the polar plateau. In 1911–1912, Captain Scott and his ''Terra Nova'' Expedition team reached the South Pole by simi ...
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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 successful expeditions to the Antarctic led by Ernest Shackleton and his second expedition to the Antarctic. Its main target, among a range of geographical and scientific objectives, was to be first to 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 preparation ...
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Edward Guinness, 1st Earl Of Iveagh
Edward Cecil Guinness, 1st Earl of Iveagh, (10 November 1847 – 7 October 1927) was an Irish businessman and philanthropist. A member of the prominent Anglo-Irish Guinness family, he was the head of the family's eponymous brewing business, making him the richest man in Ireland. A prominent philanthropist, he is best remembered for his provision of affordable housing in London and Dublin through charitable trusts. Public life Born in Clontarf, Dublin, Guinness was the third son of Sir Benjamin Guinness, 1st Baronet, and younger brother of Arthur Guinness, 1st Baron Ardilaun. Educated at Trinity College Dublin, graduating with BA in 1870, he served as Sheriff of Dublin in 1876, and nine years later became the city's High Sheriff. That same year, he was created a baronet of Castleknock, County Dublin, for helping with the visit of the then Prince of Wales to Ireland. In 1891, Guinness was created Baron Iveagh, of Iveagh in County Down. He was appointed a Knight of St Patrick i ...
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Guinness
Guinness () is an Irish dry stout that originated in the brewery of Arthur Guinness at St. James's Gate, Dublin, Ireland, in 1759. It is one of the most successful alcohol brands worldwide, brewed in almost 50 countries, and available in over 120. Sales in 2011 amounted to . In spite of declining consumption since 2001, it is the best-selling alcoholic drink in Ireland where Guinness & Co. Brewery makes almost €2 billion worth of beer annually. The Guinness Storehouse is a tourist attraction at St. James's Gate Brewery in Dublin, Ireland. Since opening in 2000, it has received over 20 million visitors. Guinness's flavour derives from malted barley and roasted unmalted barley, a relatively modern development, not becoming part of the grist until the mid-20th century. For many years, a portion of aged brew was blended with freshly brewed beer to give a sharp lactic acid flavour. Although Guinness's palate still features a characteristic "tang", the company has refused to ...
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Mountains Of The Ross Dependency
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Queen Maud Mountains
The Queen Maud Mountains are a major group of mountains, ranges and subordinate features of the Transantarctic Mountains, lying between the Beardmore and Reedy Glaciers and including the area from the head of the Ross Ice Shelf to the Antarctic Plateau in Antarctica. Captain Roald Amundsen and his South Pole party ascended Axel Heiberg Glacier near the central part of this group in November 1911, naming these mountains for the Norwegian queen Maud of Wales. Despite the name, they are not located within Queen Maud Land. Elevations bordering the Beardmore Glacier, at the western extremity of these mountains, were observed by the British expeditions led by Ernest Shackleton (1907–09) and Robert Falcon Scott (1910-13), but the mountains as a whole were mapped by several American expeditions led by Richard Evelyn Byrd (1930s and 1940s), and United States Antarctic Program (USARP) and New Zealand Antarctic Research Program (NZARP) expeditions from the 1950s through the 1970s. Featu ...
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