@article {83246,
	title = {Catastrophic beach sand losses due to erosion from predicted future sea level rise (0.5{\textendash}1.0 m), based on increasing submarine accommodation spaces in the high-wave-energy coast of the Pacific Northwest, Washington, Oregon, and Northern California, USA},
	journal = {Marine Geology},
	volume = {439},
	number = {106555},
	year = {2021},
	note = {At some point in the next hundred years, long walks on a natural beach will be more of a fantasy than a reality. Areas in the inner continental shelf and in estuaries will become sand sinks, or holding areas for beach sand as sea level rise (SLR) covers beach sands. {\textquotedblleft}The existing subcell beach sand volumes and computed new beach sand supplies (rivers and longshore transport) were subtracted from the estimated sand volumes lost to submarine accommodation spaces to establish potential beach sand deficits from near-future SLR. Of the 26 surveyed active-beaches, some 60\% and 80\% (by length) are predicted to be lost, respectively, from the 0.5 m and 1.0 m SLR or equivalent littoral sand sedimentation in submarine accommodation spaces. Projected losses reach 90\% for all PNW beaches (~900 km total length) from 1.0 m SLR{\textquotedblright} (from the Abstract).},
	month = {2021, Sep.},
	keywords = {climate, coastal hazards, coastal processes, erosion, Littoral, Nehalem Bay, Netarts Bay, sea level, Tillamook Bay},
	doi = {https://doi.org/10.1016/j.margeo.2021.106555 },
	url = {https://archives.pdx.edu/ds/psu/36497 },
	author = {Peterson, Curt D. and Pettit, Don J. and Kingen, Kara and Vanderburgh, Sandy and Rosenfeld, Chuck}
}
@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}
}
@article {13736,
	title = {Cascadia tsunami deposit database [electronic resource]},
	volume = {no.03-13},
	year = {2003},
	pages = {24 p.},
	address = {[Menlo Park, Calif.]},
	keywords = {bibliography, coastal hazards, earthquakes, geology, landslides, tsunamis},
	url = {https://www.usgs.gov/publications/cascadia-tsunami-deposit-database},
	author = {Peters, Robert and Jaffe, Bruce and Gelfenbaum, Guy and Peterson, Curt D.}
}
