@article {83208,
	title = {Earthquake and tsunami impact analysis for coastal Lincoln County, Oregon},
	volume = {no.O-21-02},
	year = {2021},
	note = {This FEMA-funded report describes the methods and results of a natural hazard risk assessment performed by the Department of Geology and Mineral Industries for Lincoln County communities.{\textquotedblright} The purpose of this project is to provide communities within the study area a detailed risk assessment of the natural hazards that affect them to enable them to compare hazards and act to reduce their risk. The risk assessment contained in this project quantifies the impacts of natural hazards to these communities and enhances the decision-making process in planning for disaster. We arrived at our findings and conclusions by completing three main tasks: compiling an asset database, identifying and using best available hazard data, and performing natural hazard risk assessment{\textquotedblright} (from the Executive Summary). Detailed reports on each community{\textquoteright}s response to a major earthquake and tsunami.},
	pages = {117p.},
	institution = {Oregon. Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, Depoe Bay (Or.), earthquakes, flooding, landslides, Lincoln City (Or.), Lincoln County (Or.), Newport (Or.), Otis (Or.), Rose Lodge (Or.), Siletz (Or.), South Beach (Or.), Toledo (Or.), tsunamis, Waldport (Or.), Yachats (Or.)},
	url = {https://www.oregongeology.org/pubs/ofr/p-O-21-02.htm },
	author = {Allan, Jonathan C. and O{\textquoteright}Brien, Fletcher E.}
}
@mastersthesis {83149,
	title = {Insights into Centennial-Scale Salt Marsh Morphodynamics from the Oregon Coast},
	year = {2021},
	note = {This doctoral dissertation gives a good look at factors causing salt marshes in Oregon to contract or expand.  Two of the seven estuaries studied (Salmon River and Alsea) are drowning, while others are either keeping pace with sea level rise or actually growing. {\textquotedblleft}In particular, the Oregon margin provides an opportunity to compare a number of important drivers of centennial salt marsh morphologic change, including relative sea level rise, suspended sediment supply, basin area, bay morphology, and coseismic <br/>subsidence related to Cascadia Subduction Zone (CSZ) earthquakes, all of which will be discussed in this dissertation.{\textquotedblright} (from the Abstract)},
	pages = {206 p.},
	school = {Oregon State University},
	type = {Doctoral Dissertation},
	edition = {Ph. D.},
	chapter = {College of Earth, Ocean, \& Atmospheric Sciences},
	address = {Corvallis, Or.},
	keywords = {Alsea Bay, climate change, Coquille River estuary, earthquakes, human impacts, land use, Nehalem River estuary, Netarts Bay, Salmon River Estuary, salt marsh, sea levels, sediments, Tillamook Bay, tsunamis, wetland delineation, Youngs Bay},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/h128nn071 },
	author = {Peck, Erin K.}
}
@article {83040,
	title = {GIS data and method for determining maximum-considered local and distant tsunami wave arrival data for the Oregon coast},
	volume = {no.O-20-09},
	year = {2020},
	note = {This is a highly technical report showing the methodology used to develop maps giving arrival times for local and distant earthquake-generated tsunamis.  The report discusses issues leading to misleading or untrue wave arrival times and the techniques used to correct these problems.},
	pages = {23 p.},
	institution = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, geology, Oregon Coast, tsunamis},
	url = {https://www.oregongeology.org/pubs/ofr/O-20-09/O-20-09_report.pdf },
	author = {Gabel, Laura L. S. and O{\textquoteright}Brien, Fletcher and Allan, Jonathan C.}
}
@article {83207,
	title = {Natural hazard risk report for Lincoln County, Oregon, including the Cities of Lincoln City, Depoe Bay, Siletz, Newport, Toledo, Waldport, and Yachats, and the Confederated Tribes of Siletz Indians, and the unincorporated communities of Otis-Rose Lodge...},
	volume = {no.O-20-11},
	year = {2020},
	note = {This FEMA-funded report describes the methods and results of a natural hazard risk assessment performed by the Department of Geology and Mineral Industries for Lincoln County communities.{\textquotedblright} The purpose of this project is to provide communities within the study area a detailed risk assessment of the natural hazards that affect them to enable them to compare hazards and act to reduce their risk. The risk assessment contained in this project quantifies the impacts of natural hazards to these communities and enhances the decision-making process in planning for disaster. We arrived at our findings and conclusions by completing three main tasks: compiling an asset database, identifying and using best available hazard data, and performing natural hazard risk assessment{\textquotedblright} (from the Executive Summary). Detailed reports on each community{\textquoteright}s response to a major earthquake and tsunami.  The full title of this report is:  Natural hazard risk report for Lincoln County, Oregon, including the Cities of Lincoln City, Depoe Bay, Siletz, Newport, Toledo, Waldport, and Yachats, and the Confederated Tribes of Siletz Indians, and the unincorporated communities of Otis-Rose Lodge, Salishan-Lincoln Beach, Otter Rock, Seal Rock-Bayshore, and Wakonda Beach.},
	pages = {99p.},
	institution = {Oregon. Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, Depoe Bay (Or.), earthquakes, erosion, landslides, Lincoln City (Or.), Lincoln County (Or.), looding, Newport (Or.), Otis (Or.), Rose Lodge (Or.), Siletz (Or.), South Beach (Or.), Toledo (Or.), tsunamis, Waldport (Or.), Yachats (Or.)},
	url = {https://www.oregongeology.org/pubs/ofr/O-20-11/O-20-11_report.pdf },
	author = {Williams, Matt C. and Appleby, Christina A. and Anthony, Lowell H. and O{\textquoteright}Brien, Fletcher E.}
}
@article {82966,
	title = {Revising estimates of spatially variable subsidence during the A.D. 1700 Cascadia Earthquake using a Bayesian foraminiferal transfer function},
	journal = {Bulletin of the Seismological Society of America },
	volume = {108 },
	number = {2},
	year = {2018},
	note = {This article is about subsidence following the 1700 C.E. earthquake on the western coast of the United States.  {\textquotedblleft}We developed four transfer functions of increasing complexity to explore how and why the composition of the modern dataset and the choice of transfer-function type affects subsidence reconstructions. . . Our reconstructions support a heterogeneous rupture model for the A.D. 1700 earthquake, but indicate that slip estimates in patches from Alsea Bay to Netarts Bay (Oregon) and from Netarts Bay to Vancouver Island should be increased.{\textquotedblright} (from the Abstract)},
	pages = {p.654-673},
	keywords = {Alsea Bay, coastal hazards, earthquakes, foraminifera, mathematical modeling, paleosciences, Salmon River Estuary, sea level, Siletz Bay, Siuslaw Bay, subsidence, tsunamis},
	doi = {https://doi.org/10.1785/0120170269 },
	author = {Kemp, Andrew C. and Cahill, Niamh and Engelhart, Simon E. and Hawkes, Andrea D. and Wang, Kelin}
}
@mastersthesis {82971,
	title = {Up-Estuary Extent and Lithologic Characteristics of Tsunami Deposits Attributed to the 1700 Cascadia Earthquake within Alsea Bay, OR},
	year = {2018},
	note = {Major earthquakes generate tsunamis.  Tsunamis leave behind deposits of marine sand.  Previously, there was a lack of information about how far inland these deposits could be found on the central Oregon coast.  To fill in this gap, the author drilled 81 cores around Alsea Bay.  He found identifiable tsunami deposits in 56 cores, extending up to 7 kilometers inland. The author profiles the sand sheet{\textquoteright}s thickness at different locations and compares his finding at Alsea Bay with what is known at the Salmon River estuary. {\textquotedblleft}The location, thickness, and other lithological properties can be used [to] validate inundation maps as well as possible rupture scenarios and magnitudes if flow capable of suspending sediments is directly related to uplift of the seafloor in earthquakes.{\textquotedblright} (p.15)  Well illustrated.  B.S. thesis. Major professor was Andrew J. Meigs.},
	pages = {18 p.},
	school = {Oregon State University},
	type = {Bachelors Thesis},
	edition = {B.S.},
	chapter = {College of Earth, Ocean, and Atmospheric Sciences},
	address = {Corvallis, Or.},
	keywords = {Alsea Bay, coastal hazards, earthquakes, paleosciences, Salmon River Estuary, sediments, tsunamis},
	url = {https://ir.library.oregonstate.edu/concern/undergraduate_thesis_or_projects/mk61rn90f },
	author = {Spruell, John T.}
}
@article {76891,
	title = {Stratigraphic and microfossil evidence for a 4500-year history of Cascadia subduction zone earthquakes and tsunamis at Yaquina River estuary, Oregon, USA},
	journal = {Geological Society of America Bulletin, },
	volume = {127},
	number = {1-2},
	year = {2015},
	note = {There{\textquoteright}s a freshwater spruce swamp buried near the northeastern shore of Sally{\textquoteright}s Bend in Yaquina Bay.  Sediment cores show 8-10 different soil sequences buried there, going back about 4500 years before the present.  Each sequence terminates abruptly with a sandy deposit and then over 10 centimeters of mud.  The authors of this paper infer that {\textquotedblleft}each buried soil represents a Cascadia subduction zone earthquake{\textellipsis}{\textquotedblright} (from the Abstract)  The article includes maps of the bay, and show locations of previous research by other scientists. The Yaquina Bay sequence is compared with sequences from other Oregon estuaries.},
	pages = {p.211-226},
	keywords = {Alsea Bay, Cannon Beach, coastal hazards, Coos Bay, Coquille River, earthquakes, geology, Netarts Bay, paleosciences, Sally{\textquoteright}s Bend, Salmon River, sediments, Sixes River, South Slough, tsunamis, Yaquina Bay, Yaquina River Estuary},
	doi = {10.1130/B31074.1},
	author = {Graehl, Nicholas A. and Kelsey, Harvey M. and Witter, Robert C. and Hemphill-Haley, Eileen and Engelhart, Simon E.}
}
@article {54886,
	title = {Tsunami impact to Washington and northern Oregon from segment ruptures on the southern Cascadia subduction zone},
	journal = {Natural Hazards},
	volume = {72},
	year = {2014},
	note = {All who live on the West Coast of the United States should be aware of the possibility of a major  earthquake occurring.  But what if only a part of the subduction zone ruptures?  This article examines a possible rupture in the southern half of the Cascadia Subduction Zone (south of Alsea Bay, Oregon).  The authors ask important questions. How quickly does tsunami wave height decline north of the southern rupture areas?  How much time do communities north of the southern rupture areas have to evacuate before the first inundation and the largest inundation occur? How far north of the southern rupture areas will felt shaking likely trigger evacuation of a populace trained to evacuate for a local earthquake? (p.851) The authors address these questions using a 10,000-year record of offshore turbedite deposits and  a ~4,600-year record of tsunami deposits at Bradley Lake.},
	month = {2014, Jun.},
	pages = {p.849-870},
	keywords = {Bandon (Or.), Brookings (Or.), Cannon Beach (Or.), Cape Blanco, coastal hazards, Columbia River, Coos Bay, Crescent City (Cal.), Depoe Bay (Or.), earthquakes, Florence (Or.), geology, Gold Beach (Or.), Grays Harbor (Wa.), Lincoln City (Or.), Long Beach (Wa.), Manzanita (Or.), Netarts Bay, Newport (Or.), Pacific City (Or.), paleosciences, Port Orford (Or.), Rockaway (Or.), Seaside (Or.), Tillamook Bay, tsunamis, Waldport (Or.), Winchester Bay},
	doi = {10.1007/s11069-014-1041-7},
	author = {Priest, George R. and Zhang, Yinglong and Witter, Robert C. and Wang, Kelin and Goldfinger, Chris and Stimely, Laura L.}
}
@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 {36471,
	title = {Tsunami inundation maps for Lincoln City North, Lincoln County, Oregon},
	year = {2013},
	note = {No. TIM-Linc-01.  2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm. Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Lincoln City North, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map Lincoln City North, Oregon. May be viewed online at the NANOOS website (click on DOGAMI to access).  },
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, Devil{\textquoteright}s Lake, earthquakes, Knight County Park, Lincoln City (Or.), maps, Otis (Or.), Rowdy Creek, Salmon River, tsunamis},
	url = {https://pubs.oregon.gov/dogami/tim/Linc01_LincolnCityNorth_Plate2_print.pdf},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program(U.S.).,}
}
@article {54631,
	title = {Tsunami inundation scenarios for Oregon},
	volume = {no. O-13-19},
	year = {2013},
	note = {This technical document accompanies the 2013 tsunami inundation map series for coastal Oregon.  It describes the methodology used to produce the maps.  In addition to the report, the CD includes GIS shapefiles with embedded metadata.},
	pages = {17 p.},
	institution = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, general, maps, mathematical modeling, Oregon, tsunamis},
	url = {https://www.oregongeology.org/pubs/ofr/O-13-19.pdf},
	author = {Priest, George R. and Witter, Robert C. and Zhang, Y. Joseph and Wang, Kelin and Goldfinger, Chris and Stimely, Laura L. and English, John T. and Pickner, Sean G. and Hughes, Kaleena L. B. and Wille, Taylore E. and Smith, Rachel L. and Oregon. Department of Geology and Mineral Industries,}
}
@article {11871,
	title = {Coastal subsidence in Oregon, USA, during the giant Cascadia earthquake of A.D. 1700},
	journal = {Quaternary Science Reviews},
	volume = {30},
	year = {2011},
	note = {This article represents an attempt to estimate how much subsidence occurred after the great Cascadia earthquake of 1700.  Stratigraphy is given for 5 rivers in Oregon, with subsidence estimates for each.  The estimate for the Salmon River is 0.6 m plus or minus .29 m},
	pages = {p.364-376},
	keywords = {Alsea Bay, coastal hazards, Coos Bay, earthquakes, geology, Nehalem River estuary, Nestucca River estuary, paleosciences, Salmon River Estuary, Siuslaw River estuary, South Slough},
	doi = {10.1016/j.quascirev.2010.11.017},
	url = {https://nora.nerc.ac.uk/id/eprint/13572/1/Hawkes_QSR_2011.pdf},
	author = {Hawkes, A.D. and Horton, B.P. and Nelson, Alan R. and Vane, C.H. and Sawai, Y.}
}
@article {11886,
	title = {The application of intertidal foraminifera to reconstruct coastal subsidence during the giant Cascadia earthquake of AD 1700 in Oregon, USA},
	journal = {Quaternary International},
	volume = {221},
	number = {1-2},
	year = {2010},
	note = {"Changes in species assemblages of intertidal foraminifera can be used to estimate the amount of earthquake-related subsidence during plate-boundary earthquakes at the Cascadia subduction zone." (from the Abstract)},
	pages = {116-140},
	keywords = {Alsea Bay, coastal hazards, Coos Bay, Coquille River, earthquakes, Nehalem River, Salmon River, Siuslaw River, tsunamis},
	doi = {10.1016/j.quaint.2009.09.019},
	author = {Hawkes, A.D. and Horton, B.P. and Nelson, A.R. and Hill, D.F.}
}
@article {11921,
	title = {Rupture area and displacement of past Cascadia great earthquakes from coastal coseismic subsidence},
	journal = {Geological Society of America bulletin.},
	volume = {122},
	number = {11-12},
	year = {2010},
	month = {2010, Nov.},
	pages = {p.2079-2096},
	keywords = {Alsea Bay, Coos Bay, Coquille River, earthquakes, geology, Necanicum River, Nehalem River, Nestucca Bay, Netarts Bay, Salmon River, sediments, Siletz Bay, Siuslaw River, Sixes River, Tillamook Bay, tsunamis, Umpqua River, Yaquina Bay},
	doi = {10.1130/B30108.1},
	author = {Leonard, Lucinda J. and Currie, Claire A. and Mazzotti, Stephane and Hyndman, Roy D.}
}
@article {36356,
	title = {Lincoln County:  Multi-Jurisdictional Natural Hazards Mitigation Plan},
	year = {2009},
	note = {{\textquotedblleft}Prepared for: Lincoln County, Depoe Bay, Lincoln City, Newport, Siletz, Toledo, Waldport and Yachats{\textquotedblright} Maps, charts, tables, appendices.  {\textquotedblleft}This natural hazard mitigation plan is intended to assist Lincoln County, Lincoln City, Depoe Bay,  Newport, Toledo, Waldport and Yachats to reduce the risk from natural hazards by identifying resources, information, and strategies for risk reduction. It will also help guide and coordinate mitigation activities throughout the County.{\textquotedblright} (p.4)},
	pages = {501 p.},
	keywords = {climate, coastal hazards, Depoe Bay (Or.), earthquakes, environmental policy and law, erosion, flooding, forest fires, landslides, Lincoln City (Or.), Lincoln County (Or.), Newport (Or.), planning, precipitation, Siletz (Or.), Toledo (Or.), tsunamis, Waldport (Or.), weather, wind, Yachats (Or.)},
	url = {https://scholarsbank.uoregon.edu/xmlui/handle/1794/9439},
	author = {Lincoln County (Or.). Dept. of Planning and Development, and University of Oregon. Community Service Center, and Oregon Partnership for Disaster Resilience,}
}
@article {12161,
	title = {Great earthquakes and tsunamis of the past 2000 years at the Salmon River Estuary, Central Oregon Coast, USA},
	journal = {Bulletin of the Seismological Society of America},
	volume = {94},
	number = {4},
	year = {2004},
	note = {Examines four sets of buried soils at the entrance to the Salmon River. Definitive proof of the great tsunami of 1700; equivocal evidence of 3 earlier sudden subsidence events.},
	month = {2004, Aug.},
	pages = {p.1276-1292},
	keywords = {earthquakes, geology, paleoecology, Salmon River Estuary, tsunamis},
	doi = {10.1785/012003210},
	author = {Nelson, Alan R. and Asquith, Andrew C. and Grant, Wendy C.}
}
@article {12181,
	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://pubs.usgs.gov/publication/ofr0313},
	author = {Peters, Robert and Jaffe, Bruce and Gelfenbaum, Guy and Peterson, Curt}
}
@article {12321,
	title = {Surviving a tsunami--lessons from Chile, Hawaii, and Japan},
	volume = {no.1187},
	year = {1999},
	note = {URL is link to revised and reprinted version of 2005.  Includes a color photograph of a bank cut from the Salmon River showing a layer of sand deposited by the 1700 tsunami on top of Native American fire pits from a fishing camp.},
	pages = {18 p.},
	institution = {U.S. Dept. of the Interior U.S. Geological Survey,},
	keywords = {archeology, earthquakes, Salmon River, sediments, tsunamis},
	url = {https://coast.noaa.gov/data/digitalcoast/pdf/tsunami-survivor-stories.pdf},
	author = {Atwater, Brian F. and Cistemas, Marco V. and Bourgeois, Joanne and Dudley, Walter C. and Hendley II, James W. and Stauffer, Peter H. (compilers)}
}
@article {12406,
	title = {Earthquake-induced subsidence and burial of late Holocene archaeological sites, Northern Oregon Coast},
	journal = {American antiquity},
	volume = {61},
	number = {4},
	year = {1996},
	note = {Why does the archeological record along the North Pacific Coast consist of "relatively young sites?"  Rising sea level is not the only factor: subsidence following major earthquakes has buried some sites. Extensive discussion of sites along Nehalem and Salmon rivers. Also discusses site at Netart Bay. Schematic diagrams of Nehalem and Salmon hearths.},
	pages = {p.772-781},
	keywords = {archeology, earthquakes, Netarts Bay, r Nehalem River, Salmon Rive, tsunamis},
	author = {Minor, Rick and Grant, Wendy C.}
}
@article {49781,
	title = {Legislative Fellowship Final Report, 1995},
	year = {1995},
	note = {This document details the work done by the 1995 Oregon Sea Grant / Oregon Coastal Zone Management Association Legislative Fellow. {\textquotedblleft}The Oregon Sea Grant/OCZMA Legislative Fellowship Program began in 1987 primarily to provide students from the Oregon State University Marine Resource Management Program (MRM) with a means with which to apply academic knowledge gained in science or public policy to the real-world arena of legislative politics.{\textquotedblright}  (p.1)  The author was assigned to State Senator Stan Bunn{\textquoteright}s office, and worked for him, for Sea Grant and for OCZMA.  The document includes summaries of legislation important to coastal communities, and brief interviews with Oregon legislators.},
	month = {1995, Aug.},
	pages = {59 p.},
	institution = {Oregon Coastal Zone Management Association,},
	address = {Salem, Or. },
	keywords = {coastal hazards, Coos Bay, Coquille River estuary, dungeness crab=Metacarcinus magister (Cancer magister), earthquakes, environmental law and policy, fish screens, general, Lower Smith River, marine mammals, Pacific salmonids=Oncorhynchus spp., salmon hatcheries, tsunamis, Vincent Creek, wild salmonids},
	url = {https://ir.library.oregonstate.edu/concern/defaults/8910jz376},
	author = {Coontz, Julie and Oregon Coastal Zone Management Association and Oregon State University. Sea Grant College Program}
}
@article {12451,
	title = {Tsunami hazard map of the Neskowin quadrangle, Tillamook and Lincoln counties, Oregon},
	year = {1995},
	month = {1995},
	publisher = {State of Oregon, Department of Geology and Mineral Industries},
	address = {Portland, OR},
	keywords = {coastal hazards, earthquakes, map, Salmon River, tsunamis},
	url = {http://www.oregongeology.org/pubs/ofr/95-24-neskowin.pdf},
	author = {Priest, George R. and Oregon. Dept. of Geology and Mineral Industries,}
}
@mastersthesis {13036,
	title = {Shoreline changes and physiographic hazards on the Oregon coast},
	year = {1975},
	note = {Comprehensive overview of coastal hazards in 1975. Maps, photographs.  Notes that Cascade Head "and the smaller unnamed headland south of the Salmon River" have had major landslides, but that most property in the area is owned by "vaiours public and quasi-public agencies" so homes not threatened.},
	pages = {201 p.},
	school = {University of Oregon},
	type = {Doctoral dissertation},
	edition = {Ph. D.},
	chapter = {Dept. of Geography},
	address = {Eugene, Or.},
	keywords = {coastal hazards, earthquakes, erosion, geological, landslides, sediments, theses},
	author = {Stembridge, James Edward, Jr.}
}
