Mollweide Glacier ( 77°56′S163°40′E / 77.933°S 163.667°E Coordinates: 77°56′S163°40′E / 77.933°S 163.667°E ) is a steep glacier 1 nautical mile (2 km) south of Mount Kowalczyk, descending west from Hobbs Ridge into Blue Glacier, in Victoria Land, Antarctica. The name is one of a group in the area associated with surveying applied in 1993 by the New Zealand Geographic Board; this glacier was named from the Mollweide projection, an equal area map projection with the parallels and central meridian being straight lines. [1]
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
A glacier is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. They also abrade rock and debris from their substrate to create landforms such as cirques and moraines. Glaciers form only on land and are distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water.
Mount Kowalczyk is a mountain, 1,690 metres (5,540 ft) high, standing 1 nautical mile (2 km) south of Goat Mountain at the head of Hobbs Glacier in Victoria Land, Antarctica. It was charted by the British Antarctic Expedition, 1910–13, under Robert Falcon Scott, and was named by the Advisory Committee on Antarctic Names in 1964 for Chester Kowalczyk, Chief of the Photogrammetry Branch, U.S. Naval Oceanographic Office, who for many years had responsibility for the photogrammetric compilation of Antarctic charts.
The Queen Elizabeth Range is a rugged mountain range of the Transantarctic Mountains System, located in the Ross Dependency region of Antarctica.
Suess Glacier is a glacier between Canada Glacier and Lacroix Glacier, flowing south into Taylor Valley in Victoria Land, Antarctica. It was charted and named by the British Antarctic Expedition under Scott, 1910–13, for Professor Eduard Suess, noted Austrian geologist and paleontologist.
Crescent Glacier is a small alpine glacier in Antarctica. It is located just east of Howard Glacier in the Kukri Hills, flowing north into Taylor Valley in Victoria Land. The glacier was studied by U.S. geologist Troy L. Pewe in December 1957, and was so named by him because of its crescent shape when viewed from the floor of Taylor Valley.
Garwood Glacier is a glacier occupying the northwest part of Garwood Valley, in Victoria Land, Antarctica. It was first mapped by the British National Antarctic Expedition (1901–04), but was not named until 1911, when Thomas Griffith Taylor of the British Antarctic Expedition, 1910–13, named it for Edmund J. Garwood, professor of geology and mineralogy at the University of London.
Astapenko Glacier is a glacier, 11 miles (18 km) long, draining the north and northeast slopes of Stanwix Peak in the Bowers Mountains and flowing east-northeast to Ob' Bay, situated in Victoria Land, Antarctica. It was mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1960–62, and named by the Advisory Committee on Antarctic Names for Pavel D. Astapenko, Soviet IGY observer, a Weather Central meteorologist at Little America V in 1958. The glacier lies on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Erebus Glacier is a glacier draining the lower southern slopes of Mount Erebus, Ross Island, Antarctica. It flows west to Erebus Bay where it forms the floating Erebus Glacier Tongue. It was named in association with Mount Erebus by the British National Antarctic Expedition, 1901–04, under Robert Falcon Scott.
Blackwelder Glacier is a pocket glacier, 1 nautical mile (2 km) wide and 2 nautical miles (4 km) long, between Salmon Hill and Hobbs Glacier in Victoria Land. The glacier was studied during U.S. Navy Operation Deepfreeze, 1957–58, by Troy L. Pewe and was named by him for Eliot Blackwelder, former head of the Geology Department at Stanford University.
Bonne Glacier is a steep glacier 1 nautical mile (2 km) west-southwest of Hobbs Peak, descending northwest from Hobbs Ridge into Blue Glacier, in Victoria Land. The name is one of a group in the area associated with surveying applied in 1993 by the New Zealand Geographic Board. It was named after the Bonne map projection, a derivative conical projection, in which the parallels are spaced at true distances along meridians which are plotted as curves.
Cassini Glacier is a steep glacier between Goat Mountain and Bonne Glacier, descending northwest from Hobbs Ridge into Blue Glacier, in Victoria Land, Antarctica. One of a group of names in the area associated with surveying applied in 1993 by the New Zealand Geographic Board, it was named from the Cassini map projection, a cylindrical projection in which the cylinder is at right angles to the axis of the globe.
Confluence Cone is a small but conspicuous nunatak 4 nautical miles (7 km) southeast of Sickle Mountain, near the west coast of the Antarctic Peninsula. It was photographed from the air by the Ronne Antarctic Research Expedition in 1947. It was surveyed from the ground by the Falkland Islands Dependencies Survey in 1958, and so named by the UK Antarctic Place-Names Committee because of its position at the confluence of several glaciers which merge with Hariot Glacier to flow into the Wordie Ice Shelf.
The Cranfield Icefalls are a series of about eight spectacular icefalls, in an east-west line, falling steeply from Bucknell Ridge into the narrowest portion of Darwin Glacier near its mouth. The feature was named by the Darwin Glacier Party of the Commonwealth Trans-Antarctic Expedition (1956–58) for W.J. Cranfield, a member of the party.
Mount Jiracek is a mountain, 2,430 metres (7,970 ft) high, rising at the west side of the head of Tinker Glacier, in the Southern Cross Mountains of Victoria Land, Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for George R. Jiracek, a geophysicist at McMurdo Station in 1964–65.
Transit Ridge is a ridge, 4 nautical miles (7 km) long, extending east from Royal Society Range between Spring Glacier and Mitchell Glacier, in Victoria Land. The name is one of a group in the area associated with surveying applied in 1993 by New Zealand Geographic Board (NZGB). Named from transit theodolite, a telescope that can be rotated through the vertical position.
Mount Heiser is a mountain just north of Dorrer Glacier in the Queen Elizabeth Range of Antarctica. It was mapped by the United States Geological Survey from tellurometer surveys and Navy air photos, 1960–62, and was named by the Advisory Committee on Antarctic Names for Paul W. Heiser, Jr., a United States Antarctic Research Program aurora scientist at Scott Base in 1959.
Hobbs Ridge is a prominent arc-shaped ridge which circumscribes Hobbs Glacier to the north and northwest and forms the divide with the lower part of Blue Glacier, on the Scott Coast of Victoria Land, Antarctica. It was named in association with Hobbs Glacier. Projection Peak rises at its most southeastern point.
Husky Pass is a pass between the Lanterman Range and Molar Massif in the Bowers Mountains of Victoria Land, Antarctica, located at the head of Sledgers Glacier and an unnamed tributary, leading to Leap Year Glacier. This mountain pass was so named by the New Zealand Geological Survey Antarctic Expedition, 1963–64, for the great efforts made here by dog teams in hauling out of the Rennick Glacier basin into that of Lillie Glacier. The pass lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Spheroid Hill is a mostly ice-free summit (1,230 m) 1 nautical mile (1.9 km) east of Ellipsoid Hill, on the north side of Blue Glacier in Victoria Land. The name is one of a group in the area associated with surveying applied in 1993 by New Zealand Geographic Board (NZGB). Named from spheroid, a mathematical figure formed by revolving an ellipse about its minor axis.
Lacroix Glacier is a glacier between Suess Glacier and Matterhorn Glacier, which flows southeast into Taylor Valley in Victoria Land, Antarctica. It was mapped by the British Antarctic Expedition, 1910–13, under Robert Falcon Scott, and named after Alfred Lacroix, as was Mount Lacroix.
The Lanterman Range is a mountain range about 35 nautical miles (60 km) long and 12 nautical miles (22 km) wide, forming the southwest part of the Bowers Mountains in Antarctica. It is bounded by the Rennick, Sledgers, Black and Canham Glaciers. The range was mapped by United States Geological Survey from surveys and U.S. Navy air photos, 1960–62, and was named by the Advisory Committee on Antarctic Names for Commander William Lanterman, an aerological officer for U.S. Navy Operation Deep Freeze, 1959–62.
The United States 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 has four major science disciplines, concerning biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility.
The Geographic Names Information System (GNIS) is a database that contains name and locative information about more than two million physical and cultural features located throughout the United States of America and its territories. It is a type of gazetteer. GNIS was developed by the United States Geological Survey in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names.
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