Pacific storms, El Nino and tsunamis: Competing mechanisms for sand deposition in a coastal marsh, Euchre Creek, Oregon

During the past 600 years, 4 well-sorted sand beds, each with abrupt lower contacts, were deposited in the Euchre Creek marsh by storm waves and a tsu nami. Brackish-marine diatoms preserved within the sand indicate a marine o rigin, but nonunique physical characteristics of the sand beds otherwise pr event the distinction of the depositional mechanism. However, a 150 year av erage recurrence interval for the sand beds is significantly smaller than t he 500 to 540 year inferred recurrence interval for Cascadia subduction zon e earthquakes, indicating that not all of the sand beds record local tsunam is. We consider storm-wave runup during extreme ocean levels and remote tsu namis generated elsewhere in the Pacific Rim, in addition to Cascadia tsuna mis, as potential sand depositional mechanisms in washover settings of the Oregon coast. Magnitude-frequency analyses of tide gage and weather buoy da ta, along with historic records of remote tsunamis, indicate that storm-wav e runup superimposed on extreme ocean levels attain heights >5 m every 10 y ears and may exceed 7 in every century, whereas remote tsunamis of similar magnitudes recur over periods of several hundred years. The best candidate for a tsunami deposit associated with the A.D. 1700 Cascadia earthquake is the thickest sand deposit which consists of multiple, fining-upward beds. T he other sand deposits most likely record multiple episodes of storm-wave w ashover or possibly, but less likely, a remote tsunami. A simple model of r elative sea-level response to the seismic cycle predicts that lower runup e levations were necessary for marine inundation of the marsh at times during the past 600 years due to coseismic subsidence.