Vertical Strain at Siple Dome, Antarctica, 1999-2002

Abstract: At the Siple Dome area of Antarctica, much of the ice flow is vertical, which causes vertical ice deformation. To measure this phenomenon, the investigators used a method known as vertical strain rate. This project was a part of the West Antarctic Ice Sheet Cores (WAISCORES) project for de...

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Bibliographic Details
Main Authors: Harrison, William, Morack, James, Waddington, Edwin D., Pettit, Erin, Zumberge, Mark, Elsberg, Daniel
Format: Dataset
Language:unknown
Published: IEDA: US Antarctic Program Data Center 2007
Subjects:
Online Access:http://get.iedadata.org/metadata/iso/609214