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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 | antarctica-soil.blogspot.com Reviews

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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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Ice in Antarctic Soils | antarctica-soil.blogspot.com Reviews

https://antarctica-soil.blogspot.com

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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antarctica-soil.blogspot.com

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Ice in Antarctic Soils: Beacon Valley

http://antarctica-soil.blogspot.com/2008/12/beacon-valley.html

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).

2

Ice in Antarctic Soils: First stop: Taylor Valley

http://antarctica-soil.blogspot.com/2008/11/first-stop-taylor-valley.html

Ice in Antarctic Soils. Thursday, November 13, 2008. First stop: Taylor Valley. At November 11th we arrived at our first location in the Dry Valleys. We flew in with a two 12 Helicopter and it took two trips, one with a sling load to get all of our equipment out. Our destination is Taylor Valley where we stay close to the coast at New Harbor. We set up the tents and get settled in. Now we are finally ready to start with our research. Posted by Ron, Birgit, David, and Tom. More from Taylor Valley.

3

Ice in Antarctic Soils: December 2008

http://antarctica-soil.blogspot.com/2008_12_01_archive.html

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.

4

Ice in Antarctic Soils: Packing

http://antarctica-soil.blogspot.com/2008/11/packing.html

Ice in Antarctic Soils. Friday, November 7, 2008. Today we are pulling our food. The food that is available for field camps is displayed on shelfs. Here we have to select the kind and quantity of food we want to eat for the next 5 weeks. This is not so easy, since it has. After the food pull we go in our cage where personnel. From the Berg Field Center ( BFC. Stored our camping equipment. The BFC. Posted by Ron, Birgit, David, and Tom. Subscribe to: Post Comments (Atom). More from Taylor Valley. Getting ...

5

Ice in Antarctic Soils: More from Taylor Valley

http://antarctica-soil.blogspot.com/2008/11/more-from-tayor-valley.html

Ice in Antarctic Soils. Thursday, November 20, 2008. More from Taylor Valley. Working all day outside in this cold environment consumes a lot of energy. A good breakfast like butter-fried bagels with jam, peanut butter, or Nutella is a good start for the day. Posted by Ron, Birgit, David, and Tom. Subscribe to: Post Comments (Atom). From left to right: Kyle, Glen, Ron, Birgit, David and Tom. More from Taylor Valley. First stop: Taylor Valley. Leaving Christchurch and Arrival on the ICE.

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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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