@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 {83064,
	title = {Predicted responses of beaches, bays, and inner-shelf sand supplies to potential sea level rise (0.5-1.0 m) in three small littoral subcells in the high-wave-energy northern Oregon coast, USA},
	journal = {Journal of Geography and Geology},
	volume = {12},
	number = {no.2},
	year = {2020},
	note = {{\textquotedblleft}Three small subcells (Nehalem, Tillamook, and Netarts) totaling ~55 km shoreline length in the high-wave energy northern Oregon coast are evaluated for potential beach sand loss from sea level rise (SLR) of 0.5{\textendash}1.0 m during the next century{\textquotedblright} (from the Abstract).  It doesn{\textquoteright}t look good.  The authors propose that there is {\textquotedblleft}accommodation space{\textquotedblright} offshore where beach sand can go.  They point out that, {\textquotedblleft}The accommodation space approach used to predict beach sand volume loss from future SLR should have broad applicability in complex littoral systems worldwide{\textquotedblright} (from the Abstract).  The data file accompanying this paper, Pacific Northwest Littoral Data (2021), may be found at: https://pdxscholar.library.pdx.edu/geology_data/1/  .},
	pages = {p.1-27},
	keywords = {bathymetry, beach profiles, Cannon Beach, Cape Falcon, Cape Lookout, Cape Meares, climate, erosion, heavy minerals, mathematical modeling, Nehalem Bay, Netarts Bay, sea level, Tillamook Bay},
	doi = {10.5539/jgg.v12n2p1  },
	url = {https://ccsenet.org/journal/index.php/jgg/article/download/0/0/43637/45834 },
	author = {Peterson, Curt D. and Doyle, Debra L. and Rosenfeld, Charles L. and Kingen, Kara E. P.}
}
@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 {13976,
	title = {Magnitude and frequency of subduction-zone earthquakes along the northern Oregon coast in the past 3,000 years.},
	volume = {57},
	number = {1},
	year = {1995},
	note = {Correlates subsided marsh sediments and evidence of tsunamis among several Oregon estuaries to show record of past earthquakes in Oregon.},
	pages = {3-12},
	keywords = {Alsea Bay, Ecola Creek, Necanicum Bay, Nestucca Bay, Netarts Bay, Siletz Bay, South Slough (Coos Bay), Yaquina Bay},
	url = {https://library.state.or.us/repository/2010/201009071430032/1995-01.pdf},
	author = {Darienzo, Mark Edward and Peterson, Curt D.}
}
@article {14051,
	title = {Stratigraphic evidence for great subduction earthquakes at four estuaries in Northern Oregon, U.S.A.},
	volume = {10},
	number = {no.4},
	year = {1994},
	note = {The authors describe in detail marsh sediments indicating major deposition from tsunamis from the Necanicum, Nestucca, Siletz and Yaquina Rivers, and correlate them with sediments from Netarts Bay, Alsea Bay and Coos Bay. This evidence supports the view that there have been six major subduction zone earthquakes on the north Oregon coast in the last 2,800 years.},
	pages = {p.850-876},
	keywords = {Alder, Alsea Bay, Conser, Coos Bay, Drift Creek, earthquakes, Hatfield Marine Science Center, King Slough, Little Nestucca River, Millport Slough, Neacoxie Creek, Neawanna Creek, Necanicum River, Nestucca Bay, Nestucca River, Netarts Bay, Oysterville, Poole Slough, Salishan Spit, salt marsh, Seaside Spit, sediment data, Siletz Bay, Siletz River, Siletz Spit, South Slough (Coos Bay), Stanley Lake, Toledo, tsunamis, Yaquina Bay, Yaquina River},
	author = {Darienzo, Mark Edward and Peterson, Curt D. and Clough, Charles}
}
@article {14166,
	title = {Episodic tectonic subsidence of late Holocene salt marshes, northern Oregon Central Cascadia margin},
	volume = {9},
	number = {1},
	year = {1990},
	note = {Describes evidence of six earthquake events revealed in buried salt marsh soils of Netarts Bay. Uplift and subsidence cycle shown. Five of six events show evidence of tsunamis.},
	pages = {1-22},
	keywords = {earthquakes, Netarts Bay, subsidence, tsunamis},
	author = {Darienzo, Mark Edward and Peterson, Curt D.}
}
