|
Random Hills
The Random Hills () are a group of rugged hills in Victoria Land, Antarctica. They are bounded on the west by Campbell Glacier and on the east by Tinker Glacier and Wood Bay. They are centered about ) north-northwest of Mount Melbourne. Exploration and name The Random Hills were named by the Southern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1966–67, because of the random orientation of the ridges which comprise the feature. Geology The Random Hills are part of the Melbourne Volcanic Province of the McMurdo Volcanic Group. K–Ar or Rb–Sr dating has given ages of 12.63 ± 0.17 million years and 12.43 ± 0.16 million years for Random Hills hawaiite. Location The Random Hills lie between the Tinker Glacier Tongue to the east, Baker Rocks on the Mount Melbourne peninsula to the south, and Bier Point and the Campbell Glacier to the west. The Burns Glacier separates the hills from Pinckard Table to the east. The Clausnitzer Glacier flows ea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Tinker Glacier Tongue
The Tinker Glacier () is a long glacier in Antarctica, draining the central part of the Southern Cross Mountains and flowing southeast into Wood Bay, on the coast of Victoria Land. Named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1962–63, for Lieutenant Colonel Ron Tinker, leader at Scott Base during that season. Geography Tinker Glacier forms in the Southern Cross Mountains to the south of the Schulte Hills, and flows south past Mount Jiracek to the west, running parallel to Aviator Glacier to the east. Burns Glacier joins from the west. The Clausnitzer Glacier joins from the west before the Harrow Peaks. Tinker glacier forms the Tinker Glacier Tongue when it flows past Cape Johnson into Wood Bay of the Ross Sea. Features Named features, from north to south, include: Burns Glacier . A tributary glacier, long, flowing north along the east side of Pinckard Table The Random Hills () are a group of rugged hills in Victoria L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borchgrevink Coast
The Borchgrevink Coast is that portion of the coast of Victoria Land between Cape Adare and Cape Washington. The name was recommended by the New Zealand Antarctic Place-Names Committee in 1961 after Carsten Borchgrevink, a member of Henrik Johan Bull's expedition to this area, 1894–95, and leader of the British Antarctic Expedition, 1898–1900, the first to winter on the continent, at Cape Adare. Landmarks *Agate Peak is a summit (topography), peak situated in the southeast area of the Intention Nunataks, at the southwest margin of Evans Neve within the Borchgrevink Coast. So named by the New Zealand Antarctic Place-Names Committee because agate and other semi-precious stones were found here by the Southern Party of New Zealand Geological Survey Antarctic Expedition, 1966–67. See also *Borchgrevink Canyon References * Borchgrevink Coast, Coasts of Victoria Land Coasts of the Ross Dependency {{BorchgrevinkCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hills Of Victoria Land
A hill is a landform that extends above the surrounding terrain. It often has a distinct summit, and is usually applied to peaks which are above elevation compared to the relative landmass, though not as prominent as mountains. Hills fall under the category of slope landforms. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the UK government's Countryside and Rights of Way Act 2000 defined mountainous areas (for the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burns Glacier
The Tinker Glacier () is a long glacier in Antarctica, draining the central part of the Southern Cross Mountains and flowing southeast into Wood Bay, on the coast of Victoria Land. Named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1962–63, for Lieutenant Colonel Ron Tinker, leader at Scott Base during that season. Geography Tinker Glacier forms in the Southern Cross Mountains to the south of the Schulte Hills, and flows south past Mount Jiracek to the west, running parallel to Aviator Glacier to the east. Burns Glacier joins from the west. The Clausnitzer Glacier joins from the west before the Harrow Peaks. Tinker glacier forms the Tinker Glacier Tongue when it flows past Cape Johnson into Wood Bay of the Ross Sea. Features Named features, from north to south, include: Burns Glacier . A tributary glacier, long, flowing north along the east side of Pinckard Table The Random Hills () are a group of rugged hills in Victoria L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Styx Glacier
Campbell Glacier () is a glacier, about long, originating near the south end of Mesa Range and draining southeast between the Deep Freeze Range and Mount Melbourne to discharge into north Terra Nova Bay in Victoria Land, Antarctica. Location Campbell Glacier forms in the Southern Cross Mountains to the south of Gair Mesa and Suture Bench. It flows south past both sides of Mericle Rock, and is joined from the west by Rainey Glacier. Hedge Terrace forms its eastern side in this section. Below Archambau Ridge it is joined from the west by Recoil Glacier, and past Mount Gibbs it is joined from the southwest by Harper Glacier. Further south Rebuff Glacier joins from the west. It continues south past Wood Ridge to the east and the Deep Freeze Range to the west. Capsize Glacier joins it from the west below Mount Cavaney. Styx Glacier joins from the east past the end of Wood Ridge. Further south Bates Glacier joins from the west to the north of Mills Peak. The glacier flows past ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Queensland
The Deep Freeze Range () is a rugged mountain range, over long and about wide, rising between Priestley and Campbell Glaciers in Victoria Land, Antarctica, and extending from the edge of the polar plateau to Terra Nova Bay. It is southwest of the Southern Cross Mountains, south of the Mesa Range and northeast of the Eisenhower Range of the Prince Albert Mountains. Exploration and name Peaks in the low and mid portions of the range were observed by early British expeditions to the Ross Sea. The range was mapped in detail by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1955-63. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) in recognition of the support to research provided by the U.S. Navy's Operation Deep Freeze expeditions to Antarctica for many years beginning in 1954. Location The Deep Freeze Range extends from southeast to northwest, between Priestley Glacier and Campbell Glacier. The narrow nort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McMurdo Station
McMurdo Station is an American Antarctic research station on the southern tip of Ross Island. It is operated by the United States through the United States Antarctic Program (USAP), a branch of the National Science Foundation. The station is the largest community in Antarctica, capable of supporting up to 1,500 residents, though the population fluctuates seasonally; during the antarctic night, there are fewer than two hundred people. It serves as one of three year-round United States Antarctic science facilities. Personnel and cargo going to or coming from Amundsen–Scott South Pole Station usually first pass through McMurdo, either by flight or by the McMurdo to South Pole Traverse; it is a hub for activities and science projects in Antarctica. McMurdo, Amundsen-Scott, and Palmer are the three non-seasonal United States stations on the continent, though by the Antarctic Treaty System the bases are not a legal claim (though the right is not forfeited); they are dedicated to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Advisory Committee On Antarctic Names
The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established in 1943 as the Special Committee on Antarctic Names (SCAN). It became the Advisory Committee on Antarctic Names in 1947. Fred G. Alberts was Secretary of the Committee from 1949 to 1980. By 1959, a structured nomenclature was reached, allowing for further exploration, structured mapping of the region and a unique naming system. A 1990 ACAN gazeeter of Antarctica listed 16,000 names. Description The United States does not recognise territorial boundaries within Antarctica, so ACAN assigns names to features anywhere within the continent, in consultation with other national nomenclature bodies where appropriate, as defined by the Antarctic Treaty System. The research and staff support for the ACAN is provided by the United States Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Geological Survey
The United States Geological Survey (USGS), founded as the Geological Survey, is an agency of the U.S. Department of the Interior whose work spans the disciplines of biology, geography, geology, and hydrology. The agency was founded on March 3, 1879, to study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The agency also makes maps of planets and moons, based on data from U.S. space probes. The sole scientific agency of the U.S. Department of the Interior, USGS is a fact-finding research organization with no regulatory responsibility. It is headquartered in Reston, Virginia, with major offices near Lakewood, Colorado; at the Denver Federal Center; and in NASA Research Park in California. In 2009, it employed about 8,670 people. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on its hundredth anniversary, was "Earth Science in the Pub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clausnitzer Glacier
The Tinker Glacier () is a long glacier in Antarctica, draining the central part of the Southern Cross Mountains and flowing southeast into Wood Bay, on the coast of Victoria Land. Named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1962–63, for Lieutenant Colonel Ron Tinker, leader at Scott Base during that season. Geography Tinker Glacier forms in the Southern Cross Mountains to the south of the Schulte Hills, and flows south past Mount Jiracek to the west, running parallel to Aviator Glacier to the east. Burns Glacier joins from the west. The Clausnitzer Glacier joins from the west before the Harrow Peaks. Tinker glacier forms the Tinker Glacier Tongue when it flows past Cape Johnson into Wood Bay of the Ross Sea. Features Named features, from north to south, include: Burns Glacier . A tributary glacier, long, flowing north along the east side of Pinckard Table to enter the southwest side of Tinker Glacier. Mapped by USGS fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
