@article {80326,
	title = {Were they all giants?  Perspectives on late Holocene plate-boundary earthquakes at the northern end of the Cascadia subduction zone},
	journal = {Quaternary Science Reviews},
	volume = {169},
	year = {2017},
	note = {While this article is focused on the northern end of the Cascadia Subduction Zone, it offers an up-to-date look at research on prehistoric tsunamis on the West Coast.  The authors attempt to match buried soils in southwest Washington that show seven different tsunamis with evidence on Vancouver Island.  They also note what can be correlated with earthquake evidence from the entire subduction zone.  The authors found that three earthquakes were definitely caused by a rupture of the entire plate margin.  Three other earthquakes left tsunami evidence in the north, but the deposited soils have not yet been accurately dated.  One earthquake seems to have taken place in the north, but is not well correlated in the south, indicating a possible partial plate rupture.},
	pages = {p.29-49},
	keywords = {Vancouver Island, Washington (State), Ecola Creek, Netarts Bay, Nestucca Bay, Yaquina Bay, Coos Bay, Talbot Creek (Coos Bay), Lagoon Creek, coastal hazards, earthquakes, tsunamis, paleosciences, geology, turbedites},
	doi = {http://dx.doi.org/10.1016/j.quascirev.2017.05.015},
	author = {Hutchinson, Ian and Clague, John J.}
}
@article {76951,
	title = {Maximum-recorded overland run-ups of major nearfield paleotsunamis during the past 3000 years along the Cascadia margin, USA, and Canada},
	journal = {Natural Hazards},
	volume = {77},
	year = {2015},
	note = {What does the past tell us about how far inland tsunamis might strike after a great earthquake in the Pacific Northwest?  This paper recounts a study of tsunami run-ups over the past 3,000 years in our region.  The authors estimate that the central part of the Cascadia region might expect {\textquotedblleft}shoreline inundation heights of up to 14{\textendash}15 {\textpm} 2 m.{\textquotedblright} (p.2023)  They warn that, {\textquotedblleft}Coastal communities should plan for the maximum paleotsunami run-ups as recorded at the nearest reliable run-up  localities.{\textquotedblright} (from the Abstract)},
	month = {2015, Jul.},
	pages = {p.2005-2026},
	keywords = {Alsea Bay, Beaver Creek, Bradley Creek, Cannon Beach, coastal hazards, earthquakes, geology, Moore Creek, Netarts Bay, paleosciences, Seaside (Or.), tsunamis},
	doi = {10.1007/s11069-015-1689-7},
	author = {Peterson, Curt D. and Carver, Gary A. and Clague, John J. and Cruikshank, Kenneth M}
}
