@inbook {15951,
	title = {Discrimination of climatic, oceanic, and tectonic mechanisms of cyclic marsh burial, Alsea Bay, Oregon},
	booktitle = {Assessing Earthquake Hazards and Reducing Risk in the Pacific Northwest},
	series = {U.S. Geological Survey Professional Paper},
	volume = {no.1560, v.1},
	year = {1996},
	note = {Alsea Bay sediments show repeated "episodic events of coastal submergence in late Holocene time," characterized by "rapid and persistant subsidence followed by gradual deposition of suspended material and associated marsh emergence."  The explanation that fits this pattern is subsidence associated with major earthquakes. By comparing uplift and subsidence in Alsea with other Oregon marshes, the authors estimate the location of an upper-plate flexure line on the central Oregon coast. The authors estimate the interval between seismic events is between 320 and 410 years.  Maps, charts, bw photographs.Five folded plates accompany the text of v.1. },
	pages = {p.115-146},
	publisher = {U.S. G.P.O.},
	organization = {U.S. G.P.O.},
	address = {Washington, D.C.},
	keywords = {Alsea Bay, earthquakes, geology, sediments, tsunamis},
	url = {https://pubs.usgs.gov/pp/1560vol1/report.pdf},
	author = {Peterson, Curt D. and Darienzo, Mark E.},
	editor = {Rogers, Albert M. and Walsh, Timothy J. and Kockelman, William J. and Priest, George R.}
}
@article {15991,
	title = {Magnitude and frequency of subduction-zone earthquakes along the northern Oregon coast in the past 3,000 years.},
	journal = {Oregon Geology},
	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 E. and Peterson, Curt D.}
}
@article {16041,
	title = {Stratigraphic evidence for great subduction earthquakes at four estuaries in Northern Oregon, U.S.A.},
	journal = {Journal of Coastal Research},
	volume = {10},
	number = {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 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, 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 E. and Peterson, Curt D. and Clough, Charles M.}
}
@article {16136,
	title = {Earthquake hazards in the Pacific Northwest of the United States. C, Discrimination of climatic, oceanic and tectonic mechanisms of cyclic marsh burial from Alsea Bay, Oregon, U.S.A.},
	volume = {no.91-441-C},
	year = {1991},
	note = {This paper will appear collectively with others from report no. 91-441, compiled by A.M. Rogers et al., as U.S. Geological Survey professional paper 1560. Thus, it is sometimes cited as dating from 1996, when professional paper no.1560 was published. Alsea Bay sediments show repeated "episodic events of coastal submergence in late Holocene time," characterized by "rapid and persistant subsidence followed by gradual deposition of suspended material and associated marsh emergence."  The explanation that fits this pattern is subsidence associated with major earthquakes. By comparing uplift and subsidence in Alsea with other Oregon marshes, the authors estimate the location of an upper-plate flexure line on the central Oregon coast. The authors estimate the interval between seismic events is between 320 and 410 years.  Maps, charts, bw photographs.},
	pages = {53 p.},
	institution = {U.S. Geological Survey},
	address = {[Denver, Colorado]},
	keywords = {Alsea Bay, coastal hazards, earthquakes, geology, sediments, tsunamis},
	url = {https://pubs.usgs.gov/of/1991/0441c/report.pdf},
	author = {Peterson, Curt D. and Darienzo, Mark E.}
}
