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Lamping Peak
Mount Falla () is a prominent conical mountain, high, standing northeast of Mount Stonehouse, between Berwick Glacier and Prebble Glacier, in the Queen Alexandra Range, Antarctica. It was sighted in January 1958 by the New Zealand party of the Commonwealth Trans-Antarctic Expedition (1956–58), and named for R.A. Falla Sir Robert Alexander Falla (21 July 1901 – 23 February 1979) was a New Zealand museum administrator and ornithologist. Early life Falla was born in Palmerston North in 1901 to George Falla and his wife, Elizabeth Kirk. As his father was work ..., a member of the Ross Sea Committee. References Mountains of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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Mount Stonehouse
Mount Stonehouse () is a peak, 2,900 m, standing 3.5 nautical miles (6 km) southwest of Mount Falla in Queen Alexandra Range. Named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1961–62) for Bernard Stonehouse Bernard Stonehouse (1 May 1926 – 12 November 2014) was a British scientist who specialised in animal behaviour, polar research and popular science. In 1953 he received the Polar Medal. Early life and military service Stonehouse was born in Hu ... who has made studies of Antarctic penguins and seals. Mountains of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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Berwick Glacier
Berwick Glacier () is a tributary glacier, long, flowing southeast between the Marshall Mountains and the Adams Mountains to enter Beardmore Glacier at Willey Point in Antarctica Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest contine .... It was named by the British Antarctic Expedition, 1907–09, (BrAE) after HMS ''Berwick'', a vessel on which Lieutenant Jameson B. Adams of the BrAE had served. The map of the British Antarctic Expedition, 1910–13, and some subsequent maps transpose the positions of Berwick Glacier and Swinford Glacier. The latter lies southwestward, and the original 1907–09 application of Berwick Glacier is the one recommended. References Glaciers of the Ross Dependency {{RossDependency-glacier-stub ...
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Prebble Glacier
Lennox-King Glacier is a large valley glacier, about long, draining Bowden Névé and flowing northeast between the Holland Range and the Queen Alexandra Range of Antarctica to enter Richards Inlet, Ross Ice Shelf. It was named by the New Zealand Geological Survey Antarctic Expedition (1959–60) for Lieutenant Commander James Lennox-King, Royal New Zealand Navy, leader at Scott Base, 1960. See also *Vertigo Bluff Vertigo Bluff () is a prominent rock bluff (1,950 m) located 4 nautical miles (7 km) south of Asquith Bluff on the west side of Lennox-King Glacier Lennox-King Glacier is a large valley glacier, about long, draining Bowden Névé and flowin ... References Glaciers of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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Queen Alexandra Range
The Queen Alexandra Range is a major mountain range of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica. It is about long, bordering the entire western side of Beardmore Glacier from the Polar Plateau to the Ross Ice Shelf. Alternate names for this range include Alexandra Mountains, Alexandra Range and Königin Alexandra Gebirge. The highest peak of the range is Mount Kirkpatrick at . Other peaks in the range include Mount Dickerson (4,120 m). Discovery This mountain range was discovered on the journey toward the South Pole by the British Antarctic Expedition, and was named by Ernest Shackleton for Queen consort Alexandra of the United Kingdom. Shackleton and his men, and a later expedition headed by Robert Falcon Scott, both collected rock samples from the range that contained fossils. The discovery that multicellular life forms had lived so close to the South Pole was an additional piece of evidence that accompanied the publicatio ...
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New Zealand
New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island country by area, covering . New Zealand is about east of Australia across the Tasman Sea and south of the islands of New Caledonia, Fiji, and Tonga. The country's varied topography and sharp mountain peaks, including the Southern Alps, owe much to tectonic uplift and volcanic eruptions. New Zealand's capital city is Wellington, and its most populous city is Auckland. The islands of New Zealand were the last large habitable land to be settled by humans. Between about 1280 and 1350, Polynesians began to settle in the islands and then developed a distinctive Māori culture. In 1642, the Dutch explorer Abel Tasman became the first European to sight and record New Zealand. In 1840, representatives of the United Kingdom and Māori chiefs ...
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Commonwealth Trans-Antarctic Expedition
The Commonwealth Trans-Antarctic Expedition (CTAE) of 1955–1958 was a Commonwealth-sponsored expedition that successfully completed the first overland crossing of Antarctica, via the South Pole. It was the first expedition to reach the South Pole overland for 46 years, preceded only by Amundsen's expedition and Scott's expedition in 1911 and 1912. In keeping with the tradition of polar expeditions of the Heroic Age of Antarctic Exploration, the CTAE was a private venture, though it was supported by the governments of the United Kingdom, New Zealand, United States, Australia and South Africa, as well as many corporate and individual donations, under the patronage of Queen Elizabeth II. It was headed by British explorer Vivian Fuchs, with New Zealander Sir Edmund Hillary leading the New Zealand Ross Sea Support team. The New Zealand party included scientists participating in International Geophysical Year research while the British team were separately based at Halley Ba ...
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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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