@booklet {83066,
	title = {Pacific Northwest Littoral Data},
	year = {2021},
	note = {{\textquotedblleft}This document contains five data tables in PDF file formats, that are used to characterize littoral subcell (beach, river mouth, and inner-shelf) conditions in the Pacific Northwest (PNW) region . . . These data have been compiled from pre-existing data sets . . . for the purposes of predicting possible beach erosion from potential future sea level rise (SLR) . . . The five data tables include Heavy-mineral tracers (Table 1), Heavy-mineral data (normalized) (Table 2), Subcell beach profile settings (Table 3), Subcell beach profile parameters (Table 4), and Subcell shelf profile parameters (Table 5){\textquotedblright} (p.1). The data supports the manuscript Peterson, C. D., Doyle, D. L., Rosenfeld, C. L., Kingen, K., (2020). 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 of Geography and Geology. v.12:.2. ( https://pdxscholar.library.pdx.edu/geology_fac/189/ )},
	chapter = {2021, Mar.},
	address = {Portland, Or.},
	keywords = {Agate Beach, Alsea River, bathymetry, beach profiles, climate, Columbia River, Coos River, Coquille River, erosion, Florence, Or., heavy minerals, Lincoln City, Or., Nehalem River, Nestucca River, Netarts, Or., Newport, Or., Nye Beach, Otter Rock, Reedsport, Or., Rogue River, Salmon River, Sand Lake, sea level, Seal Rock, Siletz River, Siuslaw River, Sixes River, South Beach, Or., The Capes, Umpqua Jetty, Umpqua River, Whale Cove, Wilson River},
	doi = {https://doi.org/10.15760/geology-data.01},
	url = {https://pdxscholar.library.pdx.edu/geology_data/1/ },
	author = {Peterson, Curt D. and Kingen, Kara E.P.},
	editor = {Portland State University. Geology Department}
}
@article {52406,
	title = {Impacts of Predicted Global Sea-Level Rise on Oregon Beaches and Tidelands},
	volume = {Paper 45},
	year = {2013},
	note = {This report consists of two sections, one on the impact of climate change and its associated sea level rise on Oregon{\textquoteright}s beaches, and another on the impact on Oregon tidelands and estuaries. {\textquotedblleft}Two background sections on the expected impacts from predicted sea level rise on the Oregon coast were prepared for Oregon Shores Conservation Coalition{\textquoteright}s {\textquoteleft}Coastal Climate Change Adaptation Project . . . . The two sections are developed for broad distribution to coastal residents, community leaders, government agencies, and other interested parties. The two non-technical sections use geometric or gradient change approaches to illustrate potential impacts of shoreline retreat and tideland submergence under conditions of accelerated global sea level rise, as predicted for the next century or two.{\textquotedblright} (from the Introduction)},
	pages = {19 p.},
	institution = {Portland State University. Dept. of Geology,},
	keywords = {beaches, climate change, earthquakes, erosion, estuaries, flooding, general, marshes, Oregon, salinity, sea level, subsidence, wetlands},
	url = {https://pdxscholar.library.pdx.edu/geology_fac/45/},
	author = {Peterson, Curt D.}
}
@article {37971,
	title = {Coastal flooding and beach retreat from coseismic subsidence in the Central Cascadia Margin, USA},
	journal = {Bulletin - Association of Engineering Geologists},
	volume = {6},
	year = {2000},
	note = {Attempts to estimate potential flooding and beach retreat following subsidence from a great earthquake. Uses geological record of paleoearthquakes. "The larger bays of southern Washington and northwest Oregon demonstrate the greatest potential hazard for regional post-seismic flooding of coastal lowlands. Specifically, dikes constructed to 100-year flood levels could be overtopped annually, following coseismic subsidence of 1-2 m." (p.266)},
	pages = {p.255-269},
	keywords = {coastal hazards, earthquakes, erosion, flooding, geology, Nehalem Bay, Nehalem Bay State Park, Nestucca Spit, Nestucca Spit State Park, paleosciences, Siletz Spit},
	author = {Peterson, Curt D. and Doyle, Debra L. and Barnett, Elson T.}
}
@article {38081,
	title = {Magnitude and frequency of subduction-zone earthquakes along the northern Oregon coast in the past 3,000 years.},
	journal = {Oregon Geology},
	volume = {57},
	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 E. and Peterson, Curt D.}
}
@article {38226,
	title = {Stratigraphic evidence for great subduction earthquakes at four estuaries in Northern Oregon, U.S.A.},
	journal = {Journal of coastal research},
	volume = {10},
	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 great subduction zone earthquakes on the north Oregon coast in the last 2,800 years."},
	month = {1994, Fall},
	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, 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 E. and Peterson, Curt D. and Clough, Charles}
}
@mastersthesis {37186,
	title = {Sedimentation in Small Active-Margin Estuaries of the Northwestern United States},
	year = {1983},
	note = {The author finds that the sediment composition of northwest coast estuaries can be "correlated with a hydrographic parameter HR (mean tidal-prism volume: mean fluvial discharge rate x 6 hours) computed for each bay."  Sedimentation is contrasted  in Alsea, Salmon River, Siletz, Siuslaw, and Tillamook bays and Grays Harbor.  An overview of the history of sedimentation in Alsea Bay over the last 10,000 years is given. School of Oceanography. Ph. D. Corvallis, Or.: Oregon State University},
	pages = {158 p.},
	school = {Oregon State University},
	type = {Doctoral dissertation},
	edition = {Ph. D.},
	chapter = {School of Oceanography},
	address = {Corvallis, Or.},
	keywords = {Alsea Bay, bathymetry, geology, Grays Harbor, hydrography, minerals, paleosciences, Salmon River Estuary, sea level, sediment data, sediments, Siletz Bay, Siuslaw Bay, species list, theses, tidal data, Tillamook Bay},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/vm40xw091},
	author = {Peterson, Curt D.}
}
