Difference between revisions of "Hudson Mountains"
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[[File:Thurston Island to Jones Mountains - hudson mountains.jpg|thumb|Hudson Mountains are circled in red; image is of the [[Walgreen Coast]] and [[Eights Coast]] areas of [[Westarctica]]]] | |||
The '''Hudson Mountains''' is a group of parasitic cones located at 74°20′S 99°25′W forming [[nunatak]]s just above the Antarctic ice sheet in west [[Ellsworth Land]]. These mountains lie just east of [[Cranton Bay]] and [[Pine Island Bay]] at the eastern extremity of the [[Amundsen Sea]], and are bounded on the north by [[Cosgrove Ice Shelf]] and on the south by the [[Pine Island Glacier]]. | The '''Hudson Mountains''' is a group of parasitic cones located at 74°20′S 99°25′W forming [[nunatak]]s just above the Antarctic ice sheet in west [[Ellsworth Land]]. These mountains lie just east of [[Cranton Bay]] and [[Pine Island Bay]] at the eastern extremity of the [[Amundsen Sea]], and are bounded on the north by [[Cosgrove Ice Shelf]] and on the south by the [[Pine Island Glacier]]. | ||
Revision as of 00:02, 30 April 2018
File:Thurston Island to Jones Mountains - hudson mountains.jpg
Hudson Mountains are circled in red; image is of the Walgreen Coast and Eights Coast areas of Westarctica
The Hudson Mountains is a group of parasitic cones located at 74°20′S 99°25′W forming nunataks just above the Antarctic ice sheet in west Ellsworth Land. These mountains lie just east of Cranton Bay and Pine Island Bay at the eastern extremity of the Amundsen Sea, and are bounded on the north by Cosgrove Ice Shelf and on the south by the Pine Island Glacier.
-Credit: Wikipedia