College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
Cascadia Paleo Consulting, Corvallis, OR 97330, USA
Mark D. Shapley
Continental Scientific Drilling Facility, School of Earth and Environmental Sciences, University of Minnesota, 116 Church St SE, Minneapolis, MN 55455, USA
Daniel G. Gavin
Department of Geography, University of Oregon, Eugene, OR 97403, USA
Alan R. Nelson
Geologic Hazards Science Center, US Geological Survey, Golden, CO 80401, USA
Chris Goldfinger
College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA
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Total article views: 1,684 (including HTML, PDF, and XML)
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1,102
528
54
1,684
110
68
83
HTML: 1,102
PDF: 528
XML: 54
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Supplement: 110
BibTeX: 68
EndNote: 83
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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: 1,900 (including HTML, PDF, and XML)
Thereof 1,802 with geography defined
and 98 with unknown origin.
Total article views: 1,684 (including HTML, PDF, and XML)
Thereof 1,585 with geography defined
and 99 with unknown origin.
Total article views: 216 (including HTML, PDF, and XML)
Thereof 216 with geography defined
and 0 with unknown origin.
Disturbance events from historical sediments from a small lake in Oregon were evaluated to determine if Cascadia megathrust earthquakes are uniquely identifiable. Geochemical provenance data identify two likely Cascadia earthquakes, one from 1700 CE and the other from 1873 CE. A crustal earthquake deposit and flood deposits were also uniquely identified, suggesting that small Cascadia lakes are good recorders of megathrust earthquakes and other disturbances.
Disturbance events from historical sediments from a small lake in Oregon were evaluated to...
