Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA
Regina DeWitt
Department of Physics, East Carolina University, 1000 E. 5th St., Greenville, NC 27858-4353, USA
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Total article views: 697 (including HTML, PDF, and XML)
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547
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697
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HTML: 547
PDF: 115
XML: 35
Total: 697
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BibTeX: 26
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Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 862 (including HTML, PDF, and XML)
Thereof 842 with geography defined
and 20 with unknown origin.
Total article views: 697 (including HTML, PDF, and XML)
Thereof 677 with geography defined
and 20 with unknown origin.
Total article views: 165 (including HTML, PDF, and XML)
Thereof 165 with geography defined
and 0 with unknown origin.
Records of the interaction between land and glacial ice movement in the Puget Lowland of Washington State are used to interpret that solid Earth movement provided stability to this marine-terminating glacial ice for at least 500 years. These results are significant because this landscape is similar to parts of the Greenland Ice Sheet and the Antarctic Peninsula, indicating that the interactions seen in this area are applicable to modern glaciated regions.
Records of the interaction between land and glacial ice movement in the Puget Lowland of...