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The Washington continental margin presents both a classic test of submarine paleoseismology, and an opportunity to explore advancement of the field through analysis of sediment dispersal in a heterogeneous system.

Most “Segment C” ruptures were found to extend further northward to the latitude of Astoria Canyon.

Mean recurrence times are therefore revised to ~ 434 years for the Washington Coast, and ~ 340 years for the central and northern Oregon coast.

► Study area includes 3 US states, with high resolution in major rivers and estuaries.

► Hi-resolution LIDAR-based DEMs are shown to be essential for the inundation study.

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3883 10th ave, im an outgoing guy who doesnt want anmy drama or head games ,im not a angry guy nor am i disrespectfull,ill be into any chik that is into outdoors life ,camping etc... My work keeps me busy so I thought can get online to see who is out there. Within active systems, the turbidite record is modulated by local landsliding and growth of active folds and faults.In the relict systems, the turbidite record begins in the middle canyon reaches, as opposed to the actively recharged systems which have a turbidite record in the more proximal canyon reaches.The model results are shown to be in very good agreement with field observations.The results demonstrate that while negligible at the open coast, the tide–tsunami interaction is solely responsible for inundation around some estuaries and rivers.► We study a trans-oceanic tsunami event with an efficient unstructured grid model.The correlated turbidite sequence suggests deposition of ~ 23 Holocene and 16 post Mazama turbidites in most parts of the canyon systems, with only modest variation, mostly attributable to evidence of bypassing and erosion.


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