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Storm Peak
Storm Peak () is a flat-topped peak, 3,280 m, standing 3.5 nautical miles (6 km) north of Blizzard Peak in the Marshall Mountains, Queen Alexandra Range. So named by the New Zealand Geological Survey Antarctic Expedition The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957 ... (NZGSAE) (1961–62) because of the stormy conditions experienced in the area. See also * Peterson Ridge, extends north from the west part of Storm Peak References External links * Mountains of the Ross Dependency Shackleton Coast :{{ShackletonCoast-geo-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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Blizzard Peak
Blizzard Peak () is, at , the highest peak in the Marshall Mountains, Queen Alexandra Range, standing northwest of Mount Marshall and southeast of Blizzard Heights, from which they are separated by a broad snow col It was so named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957 ... (1961–62) because a blizzard prevented them from reaching it for several days. Features * Lindsay Peak, standing 4 nautical miles (7 km) west-northwest of Blizzard Peak References External links * Mountains of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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Marshall Mountains
The Marshall Mountains () are a group of mountains overlooking Beardmore Glacier in the Queen Alexandra Range, Antarctica. They are bounded on the north by Berwick Glacier, and on the south by Swinford Glacier. The mountains were discovered by the South Polar Party of the British Antarctic Expedition (1907–09), and named for Dr. Eric Marshall, surgeon and cartographer to the expedition, a member of the Polar Party. Mountains * Blizzard Peak, at 3,375 metres (11,070 ft), the highest peak in the Marshall Mountains *Kenyon Peaks The Kenyon Peaks () are a small group of basalt peaks northwest of Storm Peak, in the Marshall Mountains of Antarctica. They were named by the Ohio State University The Ohio State University, commonly called Ohio State or OSU, is a public ..., located northwest of Storm Peak, in the Marshall Mountains * Mayeda Peak, at 2,890 metres (9,480 ft) high, in the Marshall Mountains * Storm Peak, standing 3.5 nautical miles (6 km) north of Blizzar ...
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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 publication ...
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New Zealand Geological Survey Antarctic Expedition
The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957–1958 expedition The 1957–1958 expedition went to the Ross Dependency and named the Borchgrevink Glacier. Other features named include: * Carter Ridge * Felsite Island * Halfway Nunatak * Hedgehog Island * Moraine Ridge 1958–1959 expedition * Cadwalader Beach * Cape Hodgson * Carter Ridge * Isolation Point * Mountaineer Range * Mount Aurora * Mount Hayward * Mount Henderson (White Island) * Mount Bird. 1960–1961 expedition * Deverall Island * Lonewolf Nunataks 1961–1962 expedition * Aurora Heights * The Boil * Ford Spur * Graphite Peak * Half Century Nunatak * Half Dome Nunatak * Hump Passage * Last Cache Nunatak * Lookout Dome * Montgomerie Glacier * Mount Fyfe * Mount Macdonald * Snowshoe Pass * Turret ...
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Peterson Ridge
Peterson Ridge () is a high rock ridge that extends north from the west part of Storm Peak massif, in Queen Alexandra Range. Named by the Ohio State University Geological Expedition Ohio () is a state in the Midwestern region of the United States. Of the fifty U.S. states, it is the 34th-largest by area, and with a population of nearly 11.8 million, is the seventh-most populous and tenth-most densely populated. The sta ..., 1969–70, for Donald N. Peterson, party member who collected basalt lavas from the ridge for petrologic and paleomagnetic studies. Ridges of the Ross Dependency Shackleton Coast {{ShackletonCoast-geo-stub ...
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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 ...
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