Evans Knoll
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Evans Knoll
The Hudson Mountains are a mountain range A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arise ... in western Ellsworth Land just east of Cranton Bay and Amundsen Sea#Pine Island Bay, Pine Island Bay at the eastern extremity of Amundsen Sea. They are of volcanic origin, consisting of low scattered mountains and nunataks that protrude through the West Antarctic Ice Sheet. The Hudson Mountains are bounded on the north by Cosgrove Ice Shelf and on the south by Pine Island Glacier. Geology The Hudson Mountains contain slightly eroded parasitic cones that overlie three extensively eroded Miocene stratovolcanoes: Mount Manthe, Teeters Nunatak and Mount Moses. Potential steam was reported in 1974 and an unconfirmed report of an eruption detected by satellite was made in 1985, indicating that th ...
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Mount Moses
Mount Moses () is, at , the highest and most prominent of the Hudson Mountains of Antarctica, located near the center of the group, about north-northeast of Mount Manthe. It was mapped from air photos taken by U.S. Navy Operation Highjump in 1946–47, and was named by the Advisory Committee on Antarctic Names for Robert L. Moses, a geomagnetist and seismologist at Byrd Station in 1967. See also * Mountains in Antarctica This is a list of all the Ultra prominent peaks (with topographic prominence greater than 1,500 metres) in Antarctica. Some islands in the South Atlantic have also been included and can be found at the end of the list. Antarctica South Atl ... References Hudson Mountains Mountains of Ellsworth Land Volcanoes of Ellsworth Land Miocene stratovolcanoes Stratovolcanoes of Antarctica {{EllsworthLand-geo-stub ...
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