T134 Coastal Hazards from Minutes to Millennia (Posters)
Monday, 2 November 2015
9:00 AM - 6:30 PM
Exhibit Hall
AMS 14C TESTS OF CORRELATIONS OF GREAT EARTHQUAKES ALONG THE CASCADIA SUBDUCTION ZONE, COASTAL OREGON
Paper number: T134-1
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Simon E. EngelhartUniversity of Rhode Island, Kingston, RI
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Robert WitterU.S.G.S., Anchorage, AK
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Christopher B. DuRossU.S. Geological Survey, Golden, CO
Abstract
We consider 180 (72 unpublished) AMS 14C ages from the 12 best-dated sequences along 350 km of the Oregon coast to test along-strike correlations of stratigraphic contacts inferred to mark subsidence during great earthquakes and(or) inundation by their accompanying tsunamis during the past 2000 years. At each coastal site we selected the highest quality (least ambiguous stratigraphic context) plant macrofossils providing the closest maximum- and minimum-limiting ages for each contact predating the ~M9 AD 1700 earthquake. Comparison of OxCal-calculated age models for contacts at each site suggests three closely spaced earthquakes from 700-1200 cal yr BP, an interval previously considered to include coastal evidence for only two earthquakes. If accurate, the comparison implies incomplete stratigraphic records for some great earthquakes at some sites. Product means (with 2s uncertainties) of OxCal age probability distribution functions yield great earthquakes at 798±55(6 sites), 933±59(3 sites), 1124±59(6 sites), 1264±26(5 sites), and 1546±23(11 sites) cal yr BP.