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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1,551
1,515
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3,236
156
152
183
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PDF: 1,515
XML: 170
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EndNote: 183
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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: 4,467 (including HTML, PDF, and XML)
Thereof 4,319 with geography defined
and 148 with unknown origin.
Total article views: 3,236 (including HTML, PDF, and XML)
Thereof 3,089 with geography defined
and 147 with unknown origin.
Total article views: 1,231 (including HTML, PDF, and XML)
Thereof 1,230 with geography defined
and 1 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...
