Difference between revisions of "Hudson Mountains"

From Encyclopedia Westarctica
Jump to navigation Jump to search
(Created page with "The '''Hudson Mountains''' is a group of parasitic cones, forming nunataks just above the Antarctic ice sheet in west Ellsworth Land. These mountains lie just east of...")
 
Line 1: Line 1:
The '''Hudson Mountains''' is a group of parasitic cones, 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]].
The '''Hudson Mountains''' is a group of parasitic cones, 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]].


-Credit: Wikipedia
-Credit: Wikipedia


[[Category: Geography of Antarctica]]
[[Category: Geography of Antarctica]]

Revision as of 00:24, 29 April 2018

The Hudson Mountains is a group of parasitic cones, 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