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Ice in Antarctic Soils

Ice in Antarctic Soils. Friday, December 26, 2008. The last stop of our field season is Beacon Valley which is an E-W striking Valley of 900 to 1200 m elevation. In the east it is bounded by the Taylor Glacier, in the west it is constraint by mountain ridges e.g. Mount Feather which hold back the ice flows from the Antarctic Ice Sheet. In Beacon Valley surfaces are older than in Victoria Valley and rocks which have been scoured by wind for thousands of years form ventifacts see below. It is much dryer.
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Ice in Antarctic Soils

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Ice in Antarctic Soils. Friday, December 26, 2008. The last stop of our field season is Beacon Valley which is an E-W striking Valley of 900 to 1200 m elevation. In the east it is bounded by the Taylor Glacier, in the west it is constraint by mountain ridges e.g. Mount Feather which hold back the ice flows from the Antarctic Ice Sheet. In Beacon Valley surfaces are older than in Victoria Valley and rocks which have been scoured by wind for thousands of years form ventifacts see below. It is much dryer.

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This web page antarctica-soil.blogspot.com states the following, "Friday, December 26, 2008." We saw that the webpage said " The last stop of our field season is Beacon Valley which is an E-W striking Valley of 900 to 1200 m elevation." It also said " In the east it is bounded by the Taylor Glacier, in the west it is constraint by mountain ridges e. Mount Feather which hold back the ice flows from the Antarctic Ice Sheet. In Beacon Valley surfaces are older than in Victoria Valley and rocks which have been scoured by wind for thousands of years form ventifacts see below."

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