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Springtail Bluff
Springtail Bluff () is the steep, south-facing bluff that borders the eastern half of Mount Hemphill, in the Anare Mountains. So named by the northern party of 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), 1963–64, for the find of small insects (Collembola) in this location. References Cliffs of Victoria Land Pennell Coast {{VictoriaLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Hemphill
The Anare Mountains () are a large group of mainly snow-covered peaks and ridges along the northern coast of Victoria Land, Antarctica. The group is bounded on the north and east by the Pacific Ocean, on the west by Lillie Glacier, and on the south by Robertson Glacier, Ebbe Glacier and Dennistoun Glacier. Kirkby Glacier, in length, drains the central Anare Mountains and flows northwest to the sea from Cape North, and just north of Arthurson Bluff, northern Victoria Land. The mountain range is situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. Mountains in this area were first sighted by Captain James Clark Ross in 1841. They were photographed during United States Navy Operation Highjump (1946–1947) and were surveyed by United States Geological Survey helicopter teams, 1962–63. Named by the northern party of the New Zealand Geological Survey Antarctic Expedition, 1963–64, for the Australian National An ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anare Mountains
The Anare Mountains () are a large group of mainly snow-covered peaks and ridges along the northern coast of Victoria Land, Antarctica. The group is bounded on the north and east by the Pacific Ocean, on the west by Lillie Glacier, and on the south by Robertson Glacier, Ebbe Glacier and Dennistoun Glacier. Kirkby Glacier, in length, drains the central Anare Mountains and flows northwest to the sea from Cape North, and just north of Arthurson Bluff, northern Victoria Land. The mountain range is situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. Mountains in this area were first sighted by Captain James Clark Ross in 1841. They were photographed during United States Navy Operation Highjump (1946–1947) and were surveyed by United States Geological Survey helicopter teams, 1962–63. Named by the northern party of the New Zealand Geological Survey Antarctic Expedition, 1963–64, for the Australian National Antarctic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of Victoria Land
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also feat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
