Horlick Ice Stream - Revision history

Westarctica at 19:06, 14 September 2021

2021-09-14T19:06:33Z

← Older revision		Revision as of 19:06, 14 September 2021
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	~~[[File:WISCONBSIN RANGE.jpg\|thumb]]~~		The '''Horlick Ice Stream''' (85°17′S 132°00′W) is a large [[Ice Stream\|ice stream]] on the featureless [[ice]] surface to the north of the main mass of the [[Horlick Mountains]] of [[Westarctica]], draining west-southwestward, parallel to these mountains, to enter the lower portion of the [[Reedy Glacier]].
	The '''Horlick Ice Stream''' (85°17′S 132°00′W) is a large ice stream on the featureless ice surface to the north of the main mass of the [[Horlick Mountains]] of Westarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the [[Reedy Glacier]]. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64~~, and~~ was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains.
			==Discovery and name==
			This ice stream was mapped by the U.S. Geological Survey from surveys and [[U.S. Navy]] air photos taken during the years 1960–64. The Horlick Ice Stream was named by the Advisory Committee on [[Antarctic]] Names in association with the Horlick Mountains.

	[[Category: Geography of Westarctica]]		[[Category: Geography of Westarctica]]

Baron of Bastanchury at 04:34, 5 May 2018

2018-05-05T04:34:55Z

← Older revision		Revision as of 04:34, 5 May 2018
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			[[File:WISCONBSIN RANGE.jpg\|thumb]]
	The '''Horlick Ice Stream''' (85°17′S 132°00′W) is a large ice stream on the featureless ice surface to the north of the main mass of the [[Horlick Mountains]] of Westarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the [[Reedy Glacier]]. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains.		The '''Horlick Ice Stream''' (85°17′S 132°00′W) is a large ice stream on the featureless ice surface to the north of the main mass of the [[Horlick Mountains]] of Westarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the [[Reedy Glacier]]. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains.

	[[Category: Geography of Westarctica]]		[[Category: Geography of Westarctica]]

Baron of Bastanchury: Created with content derived from Wikipedia

2018-05-05T04:34:26Z

Created with content derived from Wikipedia

New page

The '''Horlick Ice Stream''' (85°17′S 132°00′W) is a large ice stream on the featureless ice surface to the north of the main mass of the [[Horlick Mountains]] of Westarctica, draining west-southwestward, parallel to these mountains, to enter the lower portion of the [[Reedy Glacier]]. It was mapped by the U.S. Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names in association with the Horlick Mountains.

[[Category: Geography of Westarctica]]