|
Yoshida Bluff
Yoshida Bluff () is a flat-topped bluff which rises to 2000 m at the north side of the head of Carlyon Glacier in Cook Mountains. The bluff is midway between Mill Mountain and Kanak Peak and is ice-covered except for rock cliffs at the south and west sides. Named after Yoshio Yoshida of the National Institute of Polar Research, Japan, geochemist with Japanese Antarctic Research Expedition (JARE) in four field seasons in the McMurdo Dry Valleys The McMurdo Dry Valleys are a row of largely snow-free valleys in Antarctica, located within Victoria Land west of McMurdo Sound. The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby ..., 1963–64 to 1973–74. Cliffs of Oates Land {{OatesLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carlyon Glacier
Carlyon Glacier () is a large glacier which flows east-southeast from the névé east of Mill Mountain to the Ross Ice Shelf at Cape Murray. It was mapped in 1958 by the Darwin Glacier party of the Commonwealth Trans-Antarctic Expedition (1956–58), and named by the New Zealand Antarctic Place-Names Committee New Zealand Antarctic Place-Names Committee (NZ-APC) is an adjudicating committee established to authorize the naming of features in the Ross Dependency on the Antarctic continent. It is composed of the members of the New Zealand Geographic Board pl ... for R.A. Carlyon, who with Harry Ayres made up the party. See also * Soyuz-17 Cliff * Yoshida Bluff References * Glaciers of Hillary Coast {{RossDependency-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cook Mountains
The Cook Mountains is a group of mountains bounded by the Mulock and Darwin glaciers in Antarctica. Parts of the group were first viewed from the Ross Ice Shelf by the British National Antarctic Expedition (1901–04). Additional portions of these mountains were mapped by a New Zealand party of the CTAE (1956–58), and they were completely mapped by the USGS from Tellurometer surveys and US Navy air photos, 1959–63. Named by the NZ-APC for Captain James Cook. Cook Mountains landforms include Bowling Green Col, Bowling Green Plateau, Bromwich Terrace, DeZafra Ridge, Soyuz-13 Rock, Schoonmaker Ridge, Wright Hill, and the Brown Hills. See also * Butcher Ridge, near the polar plateau in the west part of the Cook Mountains * Finn Spur, a rock spur northeast of Mount Ayres in the Cook Mountains * Gatson Ridge, a jagged ridge, long, that runs east from the southern part of Bowling Green Plateau Bowling Green Plateau () is a small but prominent ice-covered plateau at the n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mill Mountain
Mill Mountain () is a large flat-topped mountain, high, forming the eastern end of Festive Plateau in the Cook Mountains of Antarctica. This mountain was probably sighted by the British National Antarctic Expedition (1901–04) under Captain Robert F. Scott, who gave the name "Mount Mill," after British Antarctic historian Hugh Robert Mill, to a summit in the nearby Reeves Bluffs. This area was mapped by the United States Geological Survey from surveys and U.S. Navy photography (1959–63). A prominent mountain does not rise from the bluffs, and since the name "Mount Mill" is in use elsewhere in Antarctica, the 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 ... (1965) altered the original name to Mill Mountain and applied it to the prominent mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kanak Peak
The Cook Mountains is a group of mountains bounded by the Mulock and Darwin glaciers in Antarctica. Parts of the group were first viewed from the Ross Ice Shelf by the British National Antarctic Expedition (1901–04). Additional portions of these mountains were mapped by a New Zealand party of the CTAE (1956–58), and they were completely mapped by the USGS from Tellurometer surveys and US Navy air photos, 1959–63. Named by the NZ-APC for Captain James Cook. Cook Mountains landforms include Bowling Green Col, Bowling Green Plateau, Bromwich Terrace, DeZafra Ridge, Soyuz-13 Rock, Schoonmaker Ridge, Wright Hill, and the Brown Hills. See also * Butcher Ridge, near the polar plateau in the west part of the Cook Mountains * Finn Spur, a rock spur northeast of Mount Ayres in the Cook Mountains * Gatson Ridge, a jagged ridge, long, that runs east from the southern part of Bowling Green Plateau Bowling Green Plateau () is a small but prominent ice-covered plateau at the n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Institute Of Polar Research
is the Japanese research institute for Antarctica. This agency manages several research bases on Antarctica. Research centers The NIPR has several research centers on Antarctica topics. Among others there are meteorological, geological, glacier motion, life science, ice dynamics, etc. In 1969, the NIPR started collecting meteorites. Their meteorite collection contains almost 17,000 specimens of meteorites — one of the world's largest meteorite collections. The Antarctic meteorite research in the United States is guided by ANSMET. Antarctic stations * Asuka Station * Dome F * Mizuho Station * Showa Station Planetary science education The NIPR Antarctic Meteorite Research Center loans a set of 30 thin sections of various meteorite types for use in education. The Institute prepared 20 sets of this collection. They were used in several European countries as well, including Hungary, Romania, Denmark, and Belgium. The set includes lunar and Martian meteorites. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Japanese Antarctic Research Expedition
The refers to a series of Japanese Antarctic expeditions for scientific research. The first JARE expedition was launched in 1957 to coordinate with the International Geophysical Year. This was the team which left 15 dogs, including Taro and Jiro, behind after an emergency evacuation in February 1958. Expeditions to the Antarctic took place from 1968 to 1977, and ice core An ice core is a core sample that is typically removed from an ice sheet or a high mountain glacier. Since the ice forms from the incremental buildup of annual layers of snow, lower layers are older than upper ones, and an ice core contains ic ...s were drilled on these expeditions, mostly at Mizuho. A later instance was an ecological expedition studying the ecosystems near Showa Station in Antarctica. The project was first undertaken in February 1986. It was associated with the international BIOTAS program, which also launched in 1986. Taxonomical studies of some organisms (particularly plants and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McMurdo Dry Valleys
The McMurdo Dry Valleys are a row of largely snow-free valleys in Antarctica, located within Victoria Land west of McMurdo Sound. The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby glaciers. The rocks here are granites and gneisses, and glacial tills dot this bedrock landscape, with loose gravel covering the ground. It is one of the driest places on Earth and has not seen rain for nearly two million years. The region is one of the world's most extreme deserts, and includes many features including Lake Vida, a saline lake, and the Onyx River, a meltwater stream and Antarctica's longest river. Although no living organisms have been found in the permafrost here, endolithic photosynthetic bacteria have been found living in the relatively moist interior of rocks, and anaerobic bacteria, with a metabolism based on iron and sulfur, live under the Taylor Glacier. The valleys are located within the McMurdo Valleys Antarc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
