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: 3,371 (including HTML, PDF, and XML)
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2,659
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PDF: 500
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Total: 3,371
Supplement: 207
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Cumulative views and downloads
(calculated since 17 Nov 2023)
Total article views: 2,289 (including HTML, PDF, and XML)
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1,586
496
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2,289
207
159
205
HTML: 1,586
PDF: 496
XML: 207
Total: 2,289
Supplement: 207
BibTeX: 159
EndNote: 205
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Cumulative views and downloads
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Total article views: 1,082 (including HTML, PDF, and XML)
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1,073
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5
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Cumulative views and downloads
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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: 3,371 (including HTML, PDF, and XML)
Thereof 3,293 with geography defined
and 78 with unknown origin.
Total article views: 2,289 (including HTML, PDF, and XML)
Thereof 2,214 with geography defined
and 75 with unknown origin.
Total article views: 1,082 (including HTML, PDF, and XML)
Thereof 1,079 with geography defined
and 3 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...
