@article {83200,
	title = {Earthquake and tsunami impact analysis for coastal Lane, Douglas, and Coos counties, Oregon},
	volume = {no.O-22-06},
	year = {2022},
	note = {This sobering document examines the potential impacts of different scenarios of major earthquakes. Relative distance to high ground is the most important factor in limiting deaths and injuries.  Casualties, economic losses and debris generated are estimated.  This is an honest look at the elephant on the coastline.},
	pages = {75 p.},
	institution = {Oregon. Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Bandon (Or.), Barview, Charleston (OR.), coastal hazards, Coos Bay, Dunes City (Or.), earthquakes, Florence (Or.), geology, landslides, North Bend (Or.), Reedsport (Orr.), tsunamis, Umpqua South Jetty, Winchester Bay (Or.)},
	url = {https://www.oregongeology.org/pubs/ofr/O-22-06/p-O-22-06.htm },
	author = {Allan, Jonathan C. and O{\textquoteright}Brien. Fletcher E.}
}
@article {83204,
	title = {Umpqua River, Douglas County, Oregon},
	volume = {no. 2022-OR-01},
	year = {2022},
	note = {Unless a boat is at sea, if there is a nearshore earthquake triggering a tsunami, there is no time for the owner to get the boat to safer waters.  If the earthquake is distant, however, there will be a minimum of about 4 hours to move the boat offshore.  This publication offers a thorough discussion of issues boat owners face, and what they should do.  Colored maps, colored pictures.},
	pages = {27 p.},
	institution = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, Gardiner (Or.), harbors, Maritime transportation, ports, Reedsport (Or.), tsunamis, Umpqua River estuary, Winchester Bay (Or.)},
	url = {https://www.oregongeology.org/pubs/mtrg/MTRG-2022-OR-01_Port-of-Umpqua.pdf },
	author = {Oregon Department of Geology and Mineral Industries, and Oregon Emergency Management,, and Virginia Institute of Marine Science, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@article {83201,
	title = {Umpqua River Tsunami Modeling: Toward Improved Maritime Planning Response},
	volume = {no.O-22-07},
	year = {2022},
	note = {{\textquotedblleft}Distant tsunamis affecting the West Coast of the United States over the past two decades have resulted in significant damage to ports and harbors as well as to recreational and commercial vessels attempting to escape the tsunami. Although local tsunamis will strike the coast within minutes after the start of earthquake shaking, providing little time to evacuate, distant tsunamis are expected to arrive some four to 12 hours after the event, providing time to respond. This study evaluates new tsunami modeling results completed for both distant and local tsunamis impacting the Umpqua Estuary, including the towns of Winchester Bay and Reedsport{\textquotedblright} (from the Executive Summary).  This report offers a technical background for {\textquotedblleft}Maritime Tsunami Response Guidance (MTRG) publication.{\textquotedblright}  MTRG-2022-OR-01 - Port of Umpqua:  https://www.oregongeology.org/pubs/mtrg/MTRG-2022-OR-01_Port-of-Umpqua.pdf  },
	pages = {76 p.},
	institution = {Oregon. Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, harbors, Maritime transportation, ports, Reedsport (Or.), tsunamis, Umpqua River estuary, Winchester Bay (Or.)},
	url = {https://www.oregongeology.org/pubs/ofr/p-O-22-07.htm },
	author = {Allan, Jonathan C. and Zhang, Joseph and O{\textquoteright}Brien, Fletcher E. and Gabel, Laura L. S.}
}
@mastersthesis {83071,
	title = {Evolution of Cascadia Landscapes: Drainage Reorganization Inferred from Topographic Transformations and Dendrochronological Dating of Landslide-Dammed Lakes},
	year = {2021},
	note = {This doctoral dissertation begins by examining the question of dating past landslides in the Oregon Coast Range.  Although it is assumed that the famous earthquake of 1700 C.E. caused many landslides, no landslide has been definitely dated to that event.  The author examines two coastal lakes formed by landslides, Wasson and Klickitat Lakes, and using Carbon14 dating and evidence from tree rings, dates them to the winters of 1819/1820 and 1751/1752, respectively.  He also dates other landslides to major precipitation events. The dissertation ends with a look at stream networks and the phenomenon of streams being captured by neighboring basins.},
	pages = {142 p.},
	school = {University of Oregon},
	type = {Doctoral dissertation},
	edition = {Ph. D.},
	chapter = {Dept. of Earth Sciences},
	address = {Eugene, Or.},
	keywords = {coastal hazards, dendrochronology, earthquakes, erosion, geography, geology, Klickitat Lake, landslides, mathematical modeling, North Fork Alsea River, paleosciences, precipitation, Smith River, topography, Umpqua River Basin, Wasson Lake},
	url = {https://scholarsbank.uoregon.edu/xmlui/handle/1794/26189 },
	author = {Struble, William Truin}
}
@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.}
}
@mastersthesis {83197,
	title = {Biogeochemical Signals of Mountainous Forested Watersheds{\textquoteright} Response to Disturbance},
	year = {2018},
	note = {A large quantity of small particles of organic matter in rivers comes from small mountainous streams. Thus, small mountainous watersheds play a critical role in the carbon cycle. Some organic matter export is driven by natural causes: fire, landslides, floods, while in recent years most particulate export has come from anthropogenic causes such as logging and road-building. {\textquotedblleft}In this dissertation, we studied patterns of POM [particulate organic matter] mobilization, transport, and deposition to understand better how fundamental biogeochemical processes in forested mountainous watersheds respond to disturbances triggered by natural and human forcings{\textquotedblright} (from the Abstract).  Different watersheds respond to disturbances in different ways, and the author advocates for understanding a watershed{\textquoteright}s history in order to understand how the watershed responds to environmental changes. },
	pages = {152 p.},
	school = {Oregon State University},
	type = {Doctoral Dissertation},
	edition = {Ph. D.},
	chapter = {Water Resources Science Program and College of Forestry. Sustainable Forest Management Program},
	address = {Corvallis, Or.},
	keywords = {Alsea River, carbon, chemistry, coastal hazards, earthquakes, floods, forest fires, geography, geology, human impacts, hydrology, isotopes, landslides, logging, nitrogen, Umpqua River},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/dj52wb24f },
	author = {Guerrero-Bola{\~n}o, Francisco J.}
}
@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 {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 {36531,
	title = {Tsunami inundation maps for East Gardiner, Douglas County, Oregon},
	volume = {no.TIM-Doug-05},
	year = {2013},
	note = {2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.  Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map East Gardiner, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map East Gardiner, Oregon. May be viewed online at the NANOOS website:  http://nvs.nanoos.org/TsunamiEvac  .},
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Bolton Island, Bolton Island Tideway State Park, coastal hazards, earthquakes, Gardiner (Or.), maps, Reedsport (Or.), Smith River, tsunamis, Umpqua River},
	url = {https://digital.osl.state.or.us/islandora/object/osl:32940},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@article {36521,
	title = {Tsunami inundation maps for Gardiner, Douglas County, Oregon},
	volume = {no.TIM-Doug-03},
	year = {2013},
	note = { 2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.  Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Gardiner, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map Gardiner, Oregon.May also be viewed online at the NANOOS website:  http://nvs.nanoos.org/TsunamiEvac .},
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, Gardiner (Or.), Lower Umpqua River, maps, tsunamis},
	url = { https://www.oregongeology.org/pubs/tim/p-TIM-Doug-03.htm},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@article {36526,
	title = {Tsunami inundation maps for Reedsport, Douglas County, Oregon},
	volume = {TIM-Doug-04},
	year = {2013},
	note = {2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.  Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Reedsport, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map Reedsport, Oregon. May also be viewed online at the NANOOS website:  http://nvs.nanoos.org/TsunamiEvac . },
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Bolton Island, Bolton Island Tideway State Park, coastal hazards, earthquakes, Henderson Cove, Hunt Cove, Jerden Cove, Lower Umpqua River, Macey Cove, maps, Reedsport (Or.), tsunamis, Winchester Bay, Windy Cove County Park},
	url = {https://www.oregongeology.org/pubs/tim/p-TIM-Doug-04.htm},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@article {36541,
	title = {Tsunami inundation maps for Sulphur Springs, Douglas County, Oregon},
	volume = {no.TIM-Doug-07},
	year = {2013},
	note = {2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.  Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Sulphur Springs, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map , Sulphur Springs, Oregon. May be viewed online at the NANOOS website:  http://nvs.nanoos.org/TsunamiEvac ..},
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, maps, Smith River, Sulphur Springs, tsunamis},
	url = {https://www.oregongeology.org/pubs/tim/p-TIM-Doug-07.htm},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@article {36546,
	title = {Tsunami inundation maps for Umpqua River East, Douglas County, Oregon},
	volume = {no.TIM-Doug-08},
	year = {2013},
	note = {2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.  Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Umpqua River East, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map , Umpqua River East, Oregon. May be viewed online at the NANOOS website (click on DOGAMI to access, then increase size to view map).  May also be viewed online at the NANOOS website:  http://nvs.nanoos.org/TsunamiEvac .},
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, maps, tsunamis, Umpqua River},
	url = {https://www.oregongeology.org/pubs/tim/p-TIM-Doug-08.htm},
	author = {Oregon. Dept. of Geology and Mineral Industries, and National Tsunami Hazard Mitigation Program (U.S.),}
}
@article {36536,
	title = {Tsunami inundation maps for Umpqua River West, Douglas County, Oregon},
	volume = {no.TIM-Doug-06},
	year = {2013},
	note = {No. TIM-Doug-06.  2 maps : col. ; 84 x 133 cm., on sheet 86 x 135 cm.  Plate 1. Local source (Cascadia Subduction Zone) tsunami inundation map Umpqua River West, Oregon -- Plate 2. Distance source (Alaska-Aleutian Subduction Zone) tsunami inundation map , Umpqua River West, Oregon. May be viewed online at the NANOOS website:  http://nvs.nanoos.org/TsunamiEvac . },
	publisher = {Oregon. Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, maps, Smith River, tsunamis, Umpqua River},
	url = {https://www.oregongeology.org/pubs/tim/p-TIM-Doug-06.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,}
}
@article {26786,
	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},
	note = {"Coastal marshes record a 6500 yr history of coseismic displacements in great earthquakes at the Cascadia subduction zone. We compiled estimates of coseismic displacement for past megathrust events based on correlations with megathrust-triggered turbidites, and estimated megathrust slip based on comparisons of marsh displacements with dislocation model predictions." (from the Abstract)},
	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 {26111,
	title = {Cascadia tsunami deposit database [electronic resource]},
	volume = {no.03-13},
	year = {2003},
	note = {"The Cascadia Tsunami Deposit Database contains data on the location and sedimentological properties of tsunami deposits found along the Cascadia margin." (from the Abstract)},
	pages = {24 p.},
	institution = {U.S. Geological Survey},
	address = {[Menlo Park, Calif.]},
	keywords = {bibliography, coastal hazards, earthquakes, geology, landslides, paleosciences, sediment data, tsunamis},
	url = {https://pubs.usgs.gov/publication/ofr0313},
	author = {Peters, Robert and Jaffe, Bruce and Gelfenbaum, Guy and Peterson, Curt}
}
@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 {25451,
	title = {Tsunami hazard map of the Winchester Bay quadrangle, Douglas County, Oregon [cartographic material]},
	volume = {no. O-95-40},
	year = {1995},
	note = {A later version of this map is available online at https://www.oregongeology.org/pubs/ofr/97-31-winchester_bay.pdf .},
	month = {1995},
	institution = {State of Oregon, Dept. of Geology and Mineral Industries},
	type = {Scale 1:24,000 ; Transverse Mercator proj. (W 124{\textdegree}15?00?--W 124{\textdegree}07?30?/N 43{\textdegree}45?00?--N 43{\textdegree}37?30?)},
	address = {Portland, Or},
	keywords = {coastal hazards, earthquakes, map, tsunamis},
	author = {Priest, George R.}
}
@mastersthesis {25301,
	title = {Coastal Crossing of the Elastic Strain Zero-Isobase, Cascadia Margin, South Central Oregon Coast },
	volume = {no.4739},
	year = {1994},
	note = {This thesis is an attempt to define the landward extent of the areas of "abrupt coastal subsidence and uplift" on the southern Oregon coast (p.172). Marsh cores were studied in Siuslaw Bay, the lower Umpqua River area, and Coos Bay.  Diatom assemblages indicated whether sediments were marine or brackish. Includes original photograph of marsh core sample. Maps.},
	pages = {251 p.},
	school = {Portland State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Portland, Or.},
	keywords = {Butler Creek, Coos Bay estuary, Dean Creek, diatoms, earthquakes, Gardiner paper Mill, geology, Harvey Creek, Oar Creek, Otter Slough, paleosciences, Providence Creek, Scholfield Creek, sediment data, Siuslaw estuary, Smith River, Steamboat Island, theses, tsunamis, Umpqua Estuary, Winchester Bay},
	doi = {https://doi.org/10.15760/etd.6623},
	url = {https://archives.pdx.edu/ds/psu/27772},
	author = {Briggs, Gregory George}
}
@book {24046,
	title = {Environmental geology of Western Coos and Douglas Counties, Oregon},
	series = {Bulletin (Oregon Dept. of Geology and Mineral Industries)},
	number = {no.87},
	year = {1975},
	note = {Colored maps in pocket.},
	month = {1975},
	publisher = {Oregon Dept. of Geology and Mineral Industries},
	organization = {Oregon Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, erosion, geology, minerals, paleosciences, sediments, soils},
	url = {https://www.oregongeology.org/pubs/B/B-087.pdf},
	author = {Beaulieu, John D.}
}
@mastersthesis {24111,
	title = {Shoreline Changes and Physiographic Hazards on the Oregon Coast},
	year = {1975},
	note = {Comprehensive overview of coastal hazards in 1975. Maps, photographs.  Comments on the relative stability of this part of the Oregon Coast.},
	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.}
}
@mastersthesis {23606,
	title = {Source and Characteristics of the Tsunami Observed along the Coast of the Pacific Northwest on March 28, 1964},
	year = {1965},
	note = {Thesis (M.S.). 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, including the Umpqua River. June G. Pattulo was the major professor.},
	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, earthquakes, theses, tsunamis},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/ng451m492},
	author = {Schatz, Clifford Eugene}
}
@article {23571,
	title = {Tsunamis on the Oregon coast},
	journal = {Ore Bin},
	volume = {26},
	number = {12},
	year = {1964},
	note = {Discusses the effects of the March, 1964 tsunami for different locations in Oregon.  "At Reedsport, about 10 miles up the Umpqua River only negligible indications existed of the 14-foot wave that was measured at the entrance. The meandering river with its wide tidal flats quickly dissipated the wave{\textquoteright}s energy." (p.232)},
	month = {1964, Dec.},
	pages = {231-232},
	keywords = {coastal hazards, earthquakes, tsunamis},
	isbn = {0148-1827},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/9s161b56x},
	author = {Schatz, Clifford E. and Curl Jr., Herbert and Burt, Wayne V.}
}
