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: 1,380 (including HTML, PDF, and XML)
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1,085
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48
1,380
72
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76
HTML: 1,085
PDF: 247
XML: 48
Total: 1,380
Supplement: 72
BibTeX: 62
EndNote: 76
Views and downloads (calculated since 17 Nov 2023)
Cumulative views and downloads
(calculated since 17 Nov 2023)
Total article views: 1,215 (including HTML, PDF, and XML)
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EndNote
920
247
48
1,215
72
62
76
HTML: 920
PDF: 247
XML: 48
Total: 1,215
Supplement: 72
BibTeX: 62
EndNote: 76
Views and downloads (calculated since 10 Apr 2024)
Cumulative views and downloads
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Total article views: 165 (including HTML, PDF, and XML)
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165
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165
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Views and downloads (calculated since 17 Nov 2023)
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: 1,380 (including HTML, PDF, and XML)
Thereof 1,358 with geography defined
and 22 with unknown origin.
Total article views: 1,215 (including HTML, PDF, and XML)
Thereof 1,193 with geography defined
and 22 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...