Regional tectonic deformation of the northern Oregon coast as recorded by Pleistocene marine terraces
Pleistocene marine terraces of the northern Oregon coast are an important factor in understanding the tectonics and paleoseismicity of the central Cascadia subduction zone. The lowest marine terrace, tentatively correlated to 80,000 year old Whiskey Run terrace of southern Oregon, is intermittently...
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| Format: | Others |
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PDXScholar
1992
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| Online Access: | https://pdxscholar.library.pdx.edu/open_access_etds/4433 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=5504&context=open_access_etds |