@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 {14061,
	title = {Field trip guide to Cascadia paleoseismic evidence along the northern Oregon coast: Evidence of subduction zone seismicity in the central Cascadia margin.},
	volume = {55},
	number = {no.5},
	year = {1993},
	note = {This scientific article describes geologic evidence of subduction zone seismicity on the northern half of the Oregon coastline.  Field trip covers territory from the Columbia River to Gleneden Beach near the Siletz estuary.  Photographs, maps, charts.},
	pages = {p.99-114},
	keywords = {coastal processes, earthquakes, geology, Millport Slough, Neawanna Creek, Necanicum River, Neskowin Creek, Nestucca Bay, Netarts Bay, Netarts Marsh, Salishan Spit, sediments, Siletz Bay, tsunamis, Wee Willie{\textquoteright}s},
	url = {https://library.state.or.us/repository/2010/201009071430032/1993-05.pdf},
	author = {Peterson, C.D. and Darienzo, Mark Edward}
}
@mastersthesis {14116,
	title = {Late Holocene Paleoseismicity along the Northern Oregon Coast},
	year = {1991},
	note = {Maps, drawings of core samples. Describes studies on the Necanicum, Nestucca, Siletz and Yaquina bays, which were correlated with earlier work he did on Netarts and Alsea Bays.  Found up to six paleoseismic events in the last 2600 years, most of which could be correlated from bay to bay. This work suggests that the magnitude of prehistoric earthquakes in the region was around 8.1. },
	pages = {167 p.},
	school = {Portland State Univeristy},
	type = {Doctoral Dissertation},
	edition = {Ph. D.},
	chapter = {Environmental Sciences and Resources:  Geology},
	address = {Portland, Or.},
	keywords = {Alsea Bay, coastal hazards, earthquakes, geology, Necanicum River estuary, Nestucca Bay, Netarts Bay, paleosciences, sediment data, sediments, Siletz Bay, theses, tsunamis, Yaquina Bay},
	doi = {https://doi.org/10.15760/etd.1146},
	url = {https://pdxscholar.library.pdx.edu/open_access_etds/1147/},
	author = {Darienzo, Mark Edward}
}
@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.}
}
@article {14276,
	title = {Coastal neotectonic field trip guide for Netarts Bay, Oregon},
	volume = {50},
	number = {no.9/10},
	year = {1988},
	note = {This scientific article summarizes the geologic evidence of episodic abrupt coastal subsidence that is recorded in the late Holocene salt marshes and in uplifted Pleistocene terrace deposits of Netarts Bay. Photographs, charts, maps.  Includes rough road log with stops and descriptions of different sites.},
	pages = {p.99-106},
	keywords = {coastal processes, geology},
	url = {https://library.state.or.us/repository/2010/201009071430032/1988-09-10.pdf},
	author = {Peterson, C.D. and Darienzo, Mark Edward}
}
@mastersthesis {14306,
	title = {Late Holocene Geologic History of a Netarts Bay Salt Marsh, Northwest Oregon Coast and its Relationship to Relative Sea Level Changes},
	year = {1987},
	note = {University of Oregon M. S. thesis, 1987.  Compared seismic events at Necanicum, Nestucca, Netarts, Siletz, Yaquina and Alsea bays. Found evidence of 5-6 paleoseismic events in the last 2600 years. The author found a complex but consistent history for the evolution of the Netarts Bay salt marsh, with repetitive cycles of salt marsh growth, submergence, and re-establishment relating either to tectonic events or gradual sea level rise. },
	month = {1987},
	pages = {94 p},
	school = {University of Oregon},
	address = {Eugene},
	keywords = {Alsea Bay, earthquakes, environmental change, geology, Necanicum River estuary, Nestucca Bay, Netarts Bay, Netarts Marsh, paleosciences, Siletz Bay, theses, tidal processes, tsunamis, wetlands, Yaquina Bay},
	author = {Darienzo, Mark Edward}
}
