@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 {83114,
	title = {A maximum rupture model for the central and southern Cascadia subduction zone{\textemdash}reassessing ages for coastal evidence of megathrust earthquakes and tsunamis},
	journal = {Quaternary Science Reviews},
	volume = {261 },
	number = {106922},
	year = {2021},
	note = {{\textquotedblleft}A new history of great earthquakes (and their tsunamis) for the central and southern Cascadia subduction zone shows more frequent (17 in the past 6700 yr) megathrust ruptures than previous coastal chronologies.{\textquotedblright} (from the Abstract)  The article contains a link to supplementary data, also accessible through U.S. Geological Survey data releases.},
	month = {2021, Jun.1},
	pages = {19 p.},
	keywords = {Alsea Bay, coastal hazards, Columbia River, Coos Bay, Coquille River, earthquakes, geology, mathematical modeling, Nehalem River, Nestucca Bay, Netarts Bay, paleosciences, Siletz Bay, Siuslaw River, tsunamis, Yaquina Bay},
	doi = {https://doi.org/10.1016/j.quascirev.2021.106922 },
	author = {Nelson, Alan R. and DuRoss. Christopher B. and Witter, Robert C. and Kelsey, Harvey M. and Engelhart, Simon E. and Mahan, Shannon A. and Gray, Harrison J. and Hawkes, Andrea D. and Horton, Benjamin P. and Padgett, Jason S.}
}
@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 {82016,
	title = {Ecological and biological studies of ocean rafting: Japanese tsunami marine debris in North America and the Hawaiian Islands},
	journal = {Aquatic Invasions},
	volume = {13},
	year = {2018},
	note = {{\textquotedblleft}This is one of the papers from the special issue of Aquatic Invasions on {\textquoteleft}Transoceanic Dispersal of Marine Life from Japan to North America and the Hawaiian Islands as a Result of the Japanese Earthquake and Tsunami of 2011.{\textquoteright}{\textquotedblright} (Co-Editors{\textquoteright} Note). This article is an introduction to the special issue of Aquatic Invasions. It summarizes the largest examples of tsunami debris found on the American Pacific coast and recounts the discovery of many new Japanese species identified as a result of research. Includes color photographs. This is an open-access article.},
	month = {2018, Feb.},
	pages = {p.1-9},
	keywords = {Agate Beach, algae, aquatic invertebrates, coastal hazards, Coos Bay, earthquakes, genetics, geographical distribution, Gleneden Beach, introduced species, morphology, Pacific Coast, Seal Rock, species list, taxonomy, tsunamis},
	doi = {https://doi.org/10.3391/ai.2018.13.1.01},
	url = {https://tinyurl.com/2pxmp6e8},
	author = {Carlton, James T. and Chapman, John W. and Geller, Jonathan B. and Miller, Jessica A. and Ruiz, Gregory M. and Carlton, Deborah A. and McCuller, Megan I. and Treneman, Nancy C. and Steves, Brian P. and Breitenstein, Ralph A. and Lewis, Russell and Bilderback, David and Bilderback, Diane and Haga, Takuma and Harris, Leslie H.}
}
@mastersthesis {82956,
	title = {Effects of Estuary Characteristics and Tsunami Waveforms on Transported Sand Sheets},
	year = {2018},
	note = {Major earthquakes can generate tsunamis.  Tsunamis can erode coastal soils and deposit marine sediment far inland.  In this Bachelors thesis, the author asks if it is possible to determine the size and strength of an earthquake that took place far in the past based on the depositional record of sand sheets in estuaries.  The shape of the tsunami wave, the shape of the estuary and the bed roughness of the estuary (grain size, plants, structures on the bed) all contribute to the size of the sand sheet that is deposited.  Here, the author uses a mathematical model to explore what happened in the Alsea estuary after the 1700 C.E. earthquake. Major professor was Andrew Meigs.},
	month = {2018, May 18},
	pages = {24 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, bathymetry, coastal hazards, earthquakes, mathematical modeling, paleosciences, sediment, tsunamis},
	url = {https://ir.library.oregonstate.edu/concern/undergraduate_thesis_or_projects/pz50h218k },
	author = {Armstrong, Emma Maria}
}
@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 {76921,
	title = {Community clusters of tsunami vulnerability in the US Pacific Northwest},
	journal = {Proceedings of the National Academy of Sciences of the United States of America},
	volume = {112},
	number = {17},
	year = {2015},
	note = {{\textquotedblleft}We present an analytical framework for understanding community-level vulnerability to tsunamis that integrates population exposure, demographic sensitivity, and evacuation potential. We identify three types of communities along the US Pacific Northwest coast that are directly threatened by tsunamis associated with a Cascadia subduction zone earthquake: (i) demographically diverse with low numbers of exposed people, (ii) high numbers of exposed populations but sufficient time to evacuate, and (iii) moderate numbers of exposed populations but insufficient time to evacuate.{\textquotedblleft} (p.5354) The authors identified Seaside as the most vulnerable community on the Oregon Coast. This is an open-access article.},
	month = {2015, Apr.15},
	pages = {p.5354-55359},
	keywords = {Bay City (Or.), coastal hazards, Coos Bay (Or.), Depoe Bay (Or.), Dunes City (Or.), earthquakes, environmental policy and law, Florence (Or.), Gold Beach (Or.), Lincoln City (Or.), Lincoln County (Or.), Newport (Or.), North Bend (Or.), Port Orford (Or.), Reedsport (Or.), Seaside (Or.), Tillamook (Or.), Toledo (Or.), tsunamis, Waldport (Or.), Yachats (Or.)},
	doi = {www.pnas.org/cgi/doi/10.1073/pnas.1420309112 },
	url = {https://www.pnas.org/content/112/17/5354},
	author = {Wood, Nathan J. and Jones, Jeanne and Spielman, Seth and Schmidtlein, Matthew C.}
}
@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 {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 {52416,
	title = {Adapting to climate change on the Oregon coast:  lines in the sand and rolling easements},
	journal = {Journal of Environmental Law and Litigation},
	volume = {28},
	year = {2013},
	note = {In this important article, the authors argue that Oregon should be working to strengthen its laws now in order to have the flexibility and legal framework to enable it to adapt to a changing climate and sea level rise.  {\textquotedblleft}Processes are needed to decide what infrastructure will be replaced and what will not before these inevitable events occur. . . .  Planning can ensure that shoreline armoring does not eliminate public access along the shore or total loss of sand on Oregon{\textquoteright}s beaches. Planning tools can make clear that the public access boundary does migrate inland, even if the shoreline migrates onto an inland parcel across which the public does not currently have access.{\textquotedblright} (p.514)},
	pages = {p.447-514},
	keywords = {Alsea Bay, Alsea Spit, beaches, Cape Lookout State Park, climate change, coastal hazards, environmental law and policy, environmental policy and law, erosion, flooding, Netarts Bay, New River, physical modifications, riprap, sand spits, shorelines, The Capes, Tillamook Bay, tsunamis, wave heights},
	url = {https://scholarsbank.uoregon.edu/xmlui/handle/1794/17378},
	author = {Johnson, Courtney B. and Schell, Steven R.}
}
@article {36501,
	title = {Tsunami inundation maps for Driftwood Beach, Lincoln County, Oregon},
	number = {TIM-Linc-11},
	year = {2013},
	note = {No. TIM-Linc-11.  2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.   Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Driftwood Beach, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map Driftwood Beach, Oregon.  An interactive map is available at the NANOOS website: http://nvs.nanoos.org/TsunamiEvac  },
	pages = {2 sheets},
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Alsea Bay, coastal hazards, Driftwood Beach, earthquakes, maps, tsunamis, Waldport (Or.)},
	url = {https://www.oregongeology.org/pubs/tim/p-TIM-Linc-11.htm},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@article {36496,
	title = {Tsunami inundation maps for Tidewater, Lincoln County, Oregon},
	number = {TIM-Linc-13},
	year = {2013},
	note = {No. TIM-Linc-13.  2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.  Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Tidewater, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map Tidewater, Oregon.   },
	pages = {2 sheets},
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Alsea River, coastal hazards, earthquakes, maps, Tidewater (Or.), tsunamis},
	url = {https://www.oregongeology.org/pubs/tim/p-TIM-Linc-13.htm},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@article {36506,
	title = {Tsunami inundation maps for Waldport, Lincoln County, Oregon},
	number = {TIM-Linc-12},
	year = {2013},
	note = {No. TIM-Linc-12.  2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.  Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Waldport, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map Waldport, Oregon.  An interactive map is available at the NANOOS website:  http://nvs.nanoos.org/TsunamiEvac },
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Alsea Bay, Alsea River, coastal hazards, Drift Creek, earthquakes, Eckman Slough, Lint Slough, maps, tsunamis, Waldport (Or.)},
	url = {https://www.oregongeology.org/pubs/tim/p-TIM-Linc-12.htm},
	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,}
}
@inbook {36371,
	title = {U.S. Pacific Northwest coastal hazards:  tectonic and climate controls},
	booktitle = {Coastal Hazards},
	series = {Coastal Research Library},
	volume = {6},
	year = {2012},
	note = {This is a comprehensive, up-to-date and important discussion of coastal hazards. There{\textquoteright}s an excellent discussion of historic problems, a good look at current issues, and a chilling discussion of the implications of rising sea levels and climate change.  Charts, b+w and color photographs.  Anyone considering purchasing property at the coast should read this first.},
	publisher = {Springer Science Media},
	organization = {Springer Science Media},
	chapter = {Chapter 21},
	address = {Dordrecht Netherlands},
	keywords = {Alsea Bay, Alsea Spit, Bayocean Spit, Cape Lookout State Park, climate change, coastal hazards, Columbia River, dunes, earthquakes, El Nino, erosion, flooding, geology, Gleneden Beach, historical, jetties, Lincoln City (Or.), Lincoln City Littoral Cell, minerals, Neskowin (Or.), Nestucca River, Nestucca Spit, Netarts Bay, Netarts Spit, Newport (Or.), Pacific City (Or.), Rockaway (Or.), sea level, sediments, Siletz Bay, Siletz Spit, tidal data, Tillamook Bay, tsunamis, wave heights, Willapa Bay, Yaquina Bay},
	isbn = { 9789400752344},
	doi = {10.1007/978-94-007-5234-4},
	author = {Komar, Paul D. and Allan, Jonathan C. and Ruggiero, Peter}
}
@article {15411,
	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},
	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 {15441,
	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.}
}
@inbook {15471,
	title = {Geoarchaeological themes in a dynamic coastal environment, Lincoln and Lane Counties, Oregon},
	booktitle = {Volcanoes to Vineyards:  Geologic Field Trips Through the Dynamic Landscape of the Pacific Northwest},
	series = {Field Guide (Geological Society of America)},
	volume = {15},
	year = {2009},
	note = {"In many ways, the modern Oregon coastline bears little resemblence to that associated with prehistoric coastal peoples prior to 3000 years ago..." (from the abstract).  Examines how geological forces (earthquakes, sea level rise) have changed the landscape and obscured early peoples{\textquoteright} occupations of the area.  First stop on the tour is at the main HMSC parking lot, and the second stop is at Yaquina Head. Mentions Siletz, Yaquina, Alsea, Yachats and Siuslaw paleorivers.},
	pages = {p.331-348},
	publisher = {Geological Society of America},
	organization = {Geological Society of America},
	address = {Boulder, Colo.},
	keywords = {archeology, Florence dune sheet, Neptune State Park, Oregon State University Hatfield Marine Science Center, subsidence, tsunamis, Yaquina Bay, Yaquina Head},
	doi = {https://doi.org/10.1130/2009.fld015(16)},
	url = {https://tinyurl.com/yxre8xh2},
	author = {Davis, Loren G. and Jenevein, Steven A. and Punke, Michele L. and Noller, Jay S. and Jones, Julia A. and Willis, Samuel C.},
	editor = {O{\textquoteright}Connor, Jim E. and Dorsey, Rebecca J. and Madin, Ian (eds.)}
}
@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 {15501,
	title = {Great-earthquake paleogeodesy and tsunamis of the past 2000 years at Alsea Bay, central Oregon coast, USA},
	journal = {Quaternary Science Reviews},
	volume = {27},
	number = {7-8},
	year = {2008},
	note = {Studies four sheets of tsunami-deposited sands between tidal mud and peat in Alsea Bay. "Sampling at Alsea Bay is too limited and transfer functions too imprecise to argue for preseismic subsidence.""Apparant high rates of postseismic uplift inferred from the most reliable reconstructions at Alsea Bay suggest uplift was almost as large as coseismic subsidence."  Supplementary data available at doi:10.1016/j.quascirev.2008.01.001.},
	pages = {p.747-768},
	keywords = {Alsea Bay, earthquakes, sediment data, tsunamis},
	doi = {10.1016/j.quascirev.2008.01.001},
	author = {Nelson, Alan R. and Sawai, Yuki and Jennings, Anne E. and Bradley, Lee-Ann and Gerson, Linda and Sherrod, Brian L. and Sabean, Jennifer and Horton, Benjamin P.}
}
@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}
}
@inbook {76691,
	title = {Oral tradition of earthquakes and tsunamis on the central Cascadia coast:  variation of accounts and relations to historically observed patterns across the Northwest coast},
	booktitle = {Changing Landscapes : "Telling Our Stories" : Poceedings of the Fourth Annual Coquille Cultural Preservation Conference, 2000},
	year = {2001},
	note = {This is an intriguing overview of Native American traditional tales about earthquakes and tsunamis from British Columbia to Northern California.  Interestingly, the Oregonian stories emphasize tsunamis, not earthquakes. An Alsean tale is included.},
	pages = {p.3-15},
	publisher = {Coquille Tribe of Oregon},
	organization = {Coquille Tribe of Oregon},
	address = {North Bend, Or},
	keywords = {Alsea Bay, anthropology, coastal hazards, Coos Bay, earthquakes, historical, Native Americans, Nehalem Bay, tsunamis},
	author = {Losey, Robert J.}
}
@inbook {51446,
	title = {Geologic hazards of development on sand dunes along the Oregon Coast},
	booktitle = {Environmental, Groundwater and Engineering Geology:  Applications from Oregon},
	series = {Special Publication / Association of Engineering Geologists},
	volume = {no.11},
	year = {1998},
	note = {{\textquotedblleft}There are many geologic hazards associated with development on sand dunes. These include wind erosion and deposition, water erosion and flooding from storm waves and rip currents, water erosion and flooding from tsunamis, and contamination of freshwater aquifers with associated pollution of beaches and rivers.{\textquotedblright} (p.436) Lists areas vulnerable to coastal hazards due to unwise development in dune areas.},
	pages = {p.429-438},
	address = {Belmont, Cal.},
	keywords = {Alsea Spit, American dune grass = Leymus mollis, coastal hazards, Coquille River Spit, earthquakes, erosion, European beachgrass = Ammophila arenaria, flooding, Florence (Or.), Gearhart (Or.), Gold Beach (Or.), human impacts, Nedona Beach, Pacific City (Or.), sand dunes, Seaside (Or.), Siletz River Spit, South Beach (Or.), tsunamis, urban development, winds, Yaquina River},
	author = {Reckendorf, Frank},
	editor = {Burns, Scott}
}
@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 {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 {16011,
	title = {Tsunami hazard map of the Waldport quadrangle, Lincoln County, Oregon : [cartographic material]},
	volume = {no.O-95-31},
	year = {1995},
	note = {Blue line print based on provisional 1984 map of Waldport quadrangle.  Red lines indicate probable inundation zones.},
	pages = {1 sheet},
	institution = {State of Oregon Dept. of Geology and Mineral Industries,},
	address = {Portland, Or.},
	keywords = {coastal hazards, flooding, tsunamis},
	url = {https://pubs.oregon.gov/dogami/ofr/95-31-waldport.pdf},
	author = {Priest, George R.}
}
@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 {16071,
	title = {Tsunamis affecting the west coast of the United States 1806-1992},
	volume = {no. 29},
	year = {1993},
	note = {Good data graphs},
	institution = {United States Department of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, National Geophysical Data Center},
	address = {Boulder, CO},
	keywords = {Alsea River estuary, coastal hazards, Columbia River estuary, Coos River estuary, Coquille River estuary, Depoe Bay, Nehalem River estuary, Netarts estuary, physical, Port Orford, Rogue River estuary, Siuslaw River estuary, Tillamook estuary, tsunamis, Umpqua River estuary, Yaquina Bay},
	url = {https://www.ngdc.noaa.gov/hazard/data/publications/Kgrd-29.pdf},
	author = {Lander, James F. and Lockridge, Patricia A. and Kozuch, Michael J. and U. S. Department of Commerce. National Oceanic and Atmospheric Administration, and National Geophysical Data Center,}
}
@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.}
}
@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 {17056,
	title = {Geologic hazards inventory of the Oregon coastal zone},
	volume = {no.17},
	year = {1974},
	note = {Hazards covered include: erosion, deposition, mass wasting (landslides, rockfalls), groundwater, soils, flooding and earthquakes.},
	month = {1974},
	pages = {96 p.},
	institution = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, environmental policy and law, erosion, general, hydrology, land use, physical, sediments, tsunamis},
	url = {https://www.oregongeology.org/pubs/mp/MP-17.pdf},
	author = {Beaulieu, John D. and Hughes, Paul W. and Mathiot, R. Kent and Oregon. Dept. of Geology and Mineral Industries,}
}
@mastersthesis {17661,
	title = {Source and Characteristics of the Tsunami Observed along the Coast of the Pacific Northwest on March 28, 1964},
	year = {1965},
	note = {Photographs of damage at Waldport, Tillamook Bay, a beach near Coos Bay, and wave height at Paradise Cove on the Nehalem River.Chart shows wave heights for 9 locations in Oregon. Major professor was June G. Pattulo.},
	month = {1965},
	pages = {39 p.},
	school = {Oregon State University },
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Oceanography},
	address = {Corvallis, Or.},
	keywords = {Alsea Bay, Coos Bay, earthquakes, Nehalem River, Paradise cove, theses, Tillamook Bay, tsunamis},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/ng451m492},
	author = {Schatz, Clifford Eugene}
}
