Patterson Peak (Antarctica)
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Patterson Peak (Antarctica)
Patterson Peak () is a summit (topography), peak, 1,610 m, standing at the south end of Medina Peaks, 4 nautical miles (7 km) northwest of Anderson Ridge, in the Queen Maud Mountains of Antarctica. Mapped by United States Geological Survey (USGS) from ground surveys and U.S. Navy air photos, 1960–64. Named by Advisory Committee on Antarctic Names (US-ACAN) for Clair C. Patterson, glaciologist at Byrd Station, summer 1965–66. Mountains of the Ross Dependency Amundsen Coast {{Ross-mountain-stub ...
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Summit (topography)
A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used only for a mountain peak that is located at some distance from the nearest point of higher elevation. For example, a big, massive rock next to the main summit of a mountain is not considered a summit. Summits near a higher peak, with some prominence or isolation, but not reaching a certain cutoff value for the quantities, are often considered ''subsummits'' (or ''subpeaks'') of the higher peak, and are considered part of the same mountain. A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top. Summit may also refer to the highest point along a line, trail, or route. The highest summit in the world is Mount Everest with a height of above sea level. The first official ascent was made by Tenzing Norgay and Sir Edmund Hillary ...
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Medina Peaks
The Medina Peaks () are rugged, mainly ice-free, peaks surmounting a ridge long, extending north along the east side of Goodale Glacier to the edge of the Ross Ice Shelf, Antarctica. Some of the peaks were first seen and roughly mapped by the Byrd Antarctic Expedition, 1928–30. They were named by the Advisory Committee on Antarctic Names for Guillermo Medina, Technical Director of the U.S. Navy Hydrographic Office, 1954–60, and of the Naval Oceanographic Office The Naval Oceanographic Office (NAVOCEANO), located at John C. Stennis Space Center in south Mississippi, comprises approximately 1,000 civilian, military and contract personnel responsible for providing oceanographic products and services to all ..., 1960–64. See also * Hidden Col References Mountains of the Ross Dependency Amundsen Coast {{Ross-mountain-stub ...
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Anderson Ridge
Anderson Ridge () is a ridge long, rising above the middle of the head of Koerwitz Glacier in the Queen Maud Mountains. It was mapped by the United States Geological Survey from ground surveys and from U.S. Navy air photos, 1960–64, and named by the Advisory Committee on Antarctic Names for Arthur J. Anderson, a meteorologist with the South Pole Station South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz ... winter party, 1960. References Ridges of the Ross Dependency Amundsen Coast {{RossDependency-geo-stub ...
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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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United States Geological Survey
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredt ...
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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 ...
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Clair C
Clair or Claire may refer to: *Claire (given name), a list of people with the name Claire *Clair (surname) Places Canada * Clair, New Brunswick, a former village, now part of Haut-Madawaska * Clair Parish, New Brunswick * Pointe-Claire, Quebec, Canada, municipality located on the Island of Montreal * Clair, Saskatchewan United States * Lake Claire (Atlanta), Georgia, neighborhood * Le Claire, Iowa, city in Scott County * Eau Claire, Michigan, village in Berrien County * Eau Claire, Pennsylvania, borough in Butler County * Claire City, South Dakota, town in Roberts County * Eau Claire, Wisconsin, city * Eau Claire County, Wisconsin * Saint Clair, Missouri, city * St. Clair County, Michigan * St. Clair, Michigan, city * St. Clair, Minnesota, city * St. Clair, Pennsylvania, city * St. Clair Shores, Michigan, city Scotland * Clair oilfield in the Atlantic Ocean, 75 km west of Shetland Other uses * Clair (Hampshire cricketer), English professional cricketer * "Cla ...
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Byrd Station
The Byrd Station is a former research station established by the United States during the International Geophysical Year by U.S. Navy Seabees during Operation Deep Freeze II in West Antarctica. History A joint Army, Navy, Air Force, and Marines operation supported an overland tractor train traverse that left out of Little America V in late 1956 to establish the station. The train was led by Army Major Merle Dawson and completed a traverse of over unexplored country in Marie Byrd Land to blaze a trail to a spot selected beforehand. The station consisted of a set of four prefabricated buildings and was erected in less than one month by U.S. Navy Seabees. It was commissioned on January 1, 1957. The original station ("Old Byrd") lasted about four years before it began to collapse under the snow. Construction of a second underground station in a nearby location began in 1960, and it was used until 1972. The Operation Deep Freeze activities were succeeded by "Operation Deep Freez ...
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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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