@article {83249,
	title = {Multi-hazard risk report for Tillamook County, Oregon, including the cities of Bay City, Garibaldi, Manzanita, Nehalem, Rockaway Beach, Tillamook, and Wheeler and the unincorporated communities of Bayside Gardens, Neskowin, Oceanside, Netarts, and Pacific},
	volume = {no.O-23-01},
	year = {2023},
	note = {{\textquotedblleft}The purpose of this project is to provide communities with detailed risk assessment information to enable them to compare hazards and act to reduce their risk. The risk assessment results quantify the impact of natural hazards to each community and enhance the decision-making process in planning for disaster{\textquotedblright} (from the Executive Summary). A GIS data bundle with metadata is included with the report. Colored maps.},
	pages = {111 p.},
	institution = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Bay City (Or.), Bayside Gardens (Or.), coastal hazards, demographics, earthquakes, flooding, forest fires, Garibaldi (Or.), landslides, Manzanita (Or.), Neskowin (Or.), Netarts (Or.), Netarts Bay, Oceanside (Or.), Pacific City (Or.), Rockaway Beach, Sand Lake, Tillamook (Or.), Tillamook Bay, tsunamis, Wheeler (Or.)},
	url = {https://pubs.oregon.gov/dogami/ofr/O-23-01/p-O-23-01.htm },
	author = {Williams, Matt C. and Calhoun, Nancy C.}
}
@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 {83242,
	title = {Earthquake and tsunami impact analysis for coastal Tillamook County, Oregon},
	volume = {no.0-20-14},
	year = {2020},
	note = {This report describes the methods and results of a natural hazard risk assessment performed by the Department of Geology and Mineral Industries for Tillamook, County communities. {\textquotedblright}This report provides an evaluation of the potential impacts of a Cascadia earthquake and accompanying tsunami in coastal Tillamook County. The analyses presented here include an assessment of the numbers of people, businesses, and critical facilities located in three Cascadia tsunami inundation zones (M1, L1, and XXL1). Furthermore, our analyses evaluate local population demographics in each community in order to better understand potential evacuation challenges that could affect different population groups,as well as socioeconomic impacts associated with a Cascadia subduction zone (CSZ) earthquake and resultant tsunami{\textquotedblright} (from the Executive Summary).  The report includes including an appendix of 51 tabloid-page-size community-specific profiles for Manzanita, Nehalem Bay State Park, Nehalem, Wheeler, Rockaway Beach, Barview, Garibaldi, Bay City, Tillamook, Cape Meares, Oceanside, Netarts, Cape Lookout Sate Park, Sand Lake Recreation Area, Tierra Del Mar, Pacific City, and Neskowin. An accompanying spreadsheet gives data tables.},
	pages = {121 p.},
	institution = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Barview (Or.), Bay City (Or.), coastal hazards, demographics, earthquakes, flooding, Garibaldi (Or.), landslides, Manzanita (Or.), Nehalem (Or.), Neskowin (Or.), Netarts (Or.), Netarts Bay, Oceanside (Or.), Pacific City (Or.), Rockaway Beach, Sand Lake, Tierra del Mar (Or.), Tillamook (Or.), Tillamook Bay, Tillamook County, tsunamis, Wheeler (Or.)},
	url = {https://pubs.oregon.gov/dogami/ofr/p-O-20-14.htm },
	author = {Allan, Jonathan C. and O{\textquoteright}Brien, Fletcher E. and Bauer, John M. and Williams. Matthew C.}
}
@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 {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 {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 {13486,
	title = {Oregon Coastal Atlas},
	number = {8/21/07},
	year = {2012},
	keywords = {coastal hazards, erosion data, estuaries, estuarine dynamics, habitats, human impacts, tsunamis, water quality},
	url = {https://www.coastalatlas.net/}
}
@article {36486,
	title = {Tsunami Inundation Maps for Netarts-Oceanside, Tillamook County, Oregon},
	year = {2012},
	note = {no.TIM-Till-09.  Scale 1:10,000 ; Lambert Conformal Conic (W 123{\textdegree}58{\textquoteright}--W 123{\textdegree}56{\textquoteright}/N 45{\textdegree}28{\textquoteright}--N 45{\textdegree}24{\textquoteright}).  Includes text, col. ill., and location map. Relief shown by contours and hill shading. plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Netarts-Oceanside, Oregon -- plate 2. Distant source (Alaska-Aleutian Subduction Zone) tsunami inundation map Netarts-Oceanside, Oregon.  CD-ROM includes onscreen and print versions for both plates and TIM Index map in .pdf format. Includes bibliographical references.  },
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, maps, Netarts (Or.), Netarts Bay, Netarts Spit, Oceanside (Or.), tsunamis, Whiskey Creek},
	url = {https://www.oregongeology.org/pubs/tim/p-TIM-Till-09.htm},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@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 {13571,
	title = {Rupture area and displacement of past Cascadia great earthquakes from coastal coseismic subsidence},
	volume = {122},
	number = {no.11-12},
	year = {2010},
	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 {13581,
	title = {Coastal geomorphology, hazards, and management issues along the Pacific Northwest coast of Oregon and Washington},
	booktitle = {Volcanoes to vineyards : geologic field trips through the dynamic landscape of the Pacific Northwest},
	volume = {no.15},
	year = {2009},
	note = {One stop (Stop 4)  on this tour is Cape Lookout State Park, where the increase in storm intensitites and wave heights and major El Ninos have caused the erosion of Netarts Spit. Revetment at Cape Lookout is discussed, as are erosion issues for the area around it.  The authors feel that a breach of the Netarts Spit is likely in the next decade. A copy of this article is available from the authors via ResearchGate.},
	pages = {p.495-519},
	keywords = {Cape Lookout State Park, El Nino, erosion, geological, landslides, Netarts Bay, Netarts Spit, sediments, tsunamis},
	doi = {10.1130/2009.fld015(24)},
	author = {Allan, Jonathan C. and Witter, Robert C. and Ruggiero, Peter and Hawkes, Andrea D.}
}
@article {13736,
	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://www.usgs.gov/publications/cascadia-tsunami-deposit-database},
	author = {Peters, Robert and Jaffe, Bruce and Gelfenbaum, Guy and Peterson, Curt D.}
}
@mastersthesis {13771,
	title = {Communities and Catastrophe: Tillamook Response to the AD 1700 Earthquake and Tsunami, Northern Oregon Coast},
	volume = {Ph.D.},
	year = {2002},
	note = {Extensive examination of responses of the Tillamook peoples of Netarts and Nehalem Bays to the earthquake and tsunami of 1700 C.E. Valuable resource.},
	month = {2002},
	pages = {636 p.},
	school = {University of Oregon},
	type = {Doctoral Dissertation},
	edition = {Ph.D.},
	chapter = {Department of Anthropology},
	address = {Eugene, Or.},
	keywords = {archeology, coastal hazards, Cronin Point, earthquakes, Elk Meadow, Nehalem Bay, Nehalem Bay Dune, Netarts Bay, Netarts Spit, North Fork Site, North Trail House, Spruce Tree, theses, tsunamis},
	author = {Losey, Robert. J.}
}
@article {13901,
	title = {Tidal marsh stratigraphy, sea-level change and large earthquakes-II: submergence events during the last 3500 years at Netarts Bay, Oregon, USA},
	volume = {17},
	number = {no.4},
	year = {1998},
	note = {Investigates "peat-mud couplets" - alternating layers of peat and mud. Finds three peat-mud couplets showing gradual sedimentation changes and four couplets showing rapid subsidence indicative of large earthquakes on the Cascadia subduction zone. Examines hypotheses regarding the details of these cycles.},
	month = {1998},
	pages = {p.365-393},
	abstract = {This is the second investigation where we apply the methods and scientific framework common to sea-level investigations in northwest Europe to test a model of coseismic land subsidence followed by land uplift during interseismic strain accumulation, used to explain alternating peat-mud couplets of late Holocene age found in many of the estuaries of the Pacific Northwest of the USA and Canada. Recent studies in this region interpret such couplets as the product of repeated large (magnitude 8 or 9) earthquakes on the Cascadia subduction zone. Stratigraphic investigations of the intertidal sediments at Netarts Bay, Oregon, using lithological, pollen and diatom analyses reveal different types of submergence associated with peat-mud couplets during the last 3500yr. Three peat-mud couplets record gradual sedimentation changes within an infilling body of water. Four other couplets record rapid submergence, burial of tidal marshes and their replacement by low marsh environments. In three of the events rapid submergence is small, 0-0.5m. The most recent marsh submergence event, around AD 1700, was 0.4+/-0.3m. Most of the buried peats contain microfossil evidence for a gradual increase in marine influence before the rapid change from organic to minerogenic sedimentation. Similar gradual changes are common in comparable pale environments on non-seismic coasts and are strong evidence against a simple interseismic strain accumulation-coseismic subsidence model. One hypothesis is that the gradual increase in marine influence before each submergence represents pre-seismic relative sea-level rise caused by a reduction in the rate of land uplift. The microfossil analyses provide evidence of three stages within an earthquake deformation cycle: coseismic subsidence; interseismic land uplift; and pre-seismic reduction in the rate of land uplift. At present the microfossil data do not differentiate between rapid post-seismic land uplift and rapid sedimentation.},
	keywords = {coastal hazards, geology, tsunamis},
	author = {Shennan, I. and Long, A. and Rutherford, M. M. and Innes, J.B. and Green, F.M. and Walker, K.J.}
}
@article {13936,
	title = {Earthquake-induced subsidence and burial of late Holocene archaeological sites, Northern Oregon Coast},
	volume = {61},
	number = {no.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, Nehalem River, Netarts Bay, Salmon River, tsunamis},
	author = {Minor, Rick and Grant, Wendy C.}
}
@article {13956,
	title = {Tsunami hazard map of the Netarts quadrangle, Tillamook County, Oregon},
	volume = {no.O-95-20},
	year = {1996},
	month = {1996},
	publisher = {Oregon Department of Geology and Mineral Industries},
	address = {Portland},
	keywords = {coastal hazards, earethquakes, map, tsunamis},
	url = {https://oregonexplorer.info/data_files/OE_location/northcoast/documents/NorthCoastPDFs/95-20-netarts.pdf},
	author = {Priest, George R. and Oregon. Department of Geology and Mineral Industries,}
}
@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}
}
@book {14016,
	title = {Improving natural hazards management on the Oregon coast},
	series = {ORESU-T},
	volume = {no.94-002},
	year = {1994},
	note = {This report addresses 23 issues, organized in four categories: hazard identification, beach and shore protection, land use, and disaster preparedness and response. The group makes 79 recommendations and suggests those actions and agencies, organizations, or institutions that could best implement each recommendation.},
	pages = {162 p},
	publisher = {Oregon Sea Grant. Oregon State University,},
	organization = {Oregon Sea Grant. Oregon State University,},
	address = {Corvallis, OR},
	keywords = {coastal hazards, coastal processes, earthquakes, environmental policy and law, erosion, geology, land use, landslides, tsunamis},
	url = {http://library.state.or.us/repository/2012/201204021625351/},
	author = {Coastal Natural Hazards Policy Working Group, and U.S. National Oceanic and Atmospheric Administration, and Oregon State University. Sea Grant College Program and Oregon. Legislative Assembly,}
}
@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}
}
@book {14096,
	title = {Coastal Natural Hazards: Science, Engineering, and Public Policy},
	series = {ORESU-B},
	volume = {no.92-001},
	year = {1992},
	pages = {162 p},
	publisher = {Oregon Sea Grant, Oregon State University},
	organization = {Oregon Sea Grant, Oregon State University},
	address = {Corvallis, OR},
	keywords = {coastal hazards, coastal processes, earthquakes, environmental policy and law, erosion, landslides, tsunamis},
	author = {Good, James W. and Ridlington, Sandy S.}
}
@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.}
}
@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}
}
@article {14931,
	title = {Geologic hazards inventory of the Oregon coastal zone},
	volume = {no.17},
	year = {1974},
	pages = {103 p.},
	institution = {[Oregon Department of Geology and Mineral Industries]},
	address = {Portland, OR},
	keywords = {coastal hazards, earthquakes, environmental policy and law, erosion, flooding, general, hydrology, land use, landslides, 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 Department of Geology and Mineral Industries,}
}
