@mastersthesis {83185,
	title = {Factors Influencing Streamflow Generation Processes in Rain-dominated, Coastal Watersheds in Oregon},
	year = {2021},
	note = {The water in Oregon coastal streams comes from rainfall. As climate change shifts the timing and quantity of rainfall, already threatened species will be further stressed. This impressive doctoral dissertation examines how factors such as slope, lithology and land cover affect streamflow in watersheds stressed by climate change. Many coastal watersheds were examined. Mary Santelmann and Rebecca Flitcroft were co-major professors.},
	pages = {152 p.},
	school = {Oregon State University},
	type = {Doctoral Dissertation},
	edition = {Ph. D.},
	chapter = {Water Resources Science Program},
	address = {Corvallis, Or.},
	keywords = {Alsea River, climate, Coho salmon = Oncorhynchus kisutch, Drift Creek (Alsea), geology, hydrology, Pacific salmonids = Oncorhynchus spp., precipitation, Salmon River, sediments, Siletz River, Siuslaw River, streamflow, Yachats River, Yaquina River},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/f7623k880 },
	author = {Pazdral, Rosemary}
}
@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 {83029,
	title = {Eocene initiation of the Cascadia subduction zone:  A second example of plume-induced subduction initiation?},
	journal = {Geosphere},
	volume = {15 },
	number = {3},
	year = {2019},
	note = {In this article, the authors postulate a fascinating scenario to explain the development of the Cascadia Subduction Zone. The authors theorize that the Yellowstone mantle plume head {\textquotedblleft}destroyed the existing Cordilleran subduction zone and allowed the new Cascadia subduction zone to form by collapse of thermally weakened oceanic lithosphere over the hot western margin of the plume head.{\textquotedblright} (from the Abstract) This is an elegant approach that solves problems and answers questions. Nicely illustrated.},
	pages = {p.659{\textendash}681},
	keywords = {geology, paleosciences},
	doi = {https://doi.org/10.1130/GES02050.1 },
	url = {https://pubs.geoscienceworld.org/gsa/geosphere/article/15/3/659/569925/Eocene-initiation-of-the-Cascadia-subduction-zone },
	author = {Stern, Robert J. and Dumitru, Trevor A.}
}
@article {83063,
	title = {Winter habitat condition of Oregon coast coho salmon populations, 2007-2014},
	volume = {no.2018-01},
	year = {2018},
	note = {Winter habitat turns out to be an important, indeed, a limiting factor in coho salmon survival.  Nicely complex habitat offers refuges that enable juvenile coho to survive winter freshets as well as providing {\textquotedblleft}a large freshwater survival buffer that may help coho persist though extended periods of poor ocean survival{\textquotedblright} (p.2). It is troubling to note that agricultural land, private forest land and urban lands had the greatest lack of complexity, highlighting the need for more education and other efforts in these areas.},
	pages = {30 p.},
	institution = {ODFW Aquatic Inventories Project},
	address = {Salem, Or.},
	keywords = {Alsea River, American beaver = Castor canadensis, Coho salmon = Oncorhynchus kisutch, Coos Bay, Coquille River, geography, geology, habitats, hydrology, land use, Nehalem River, Nestucca River, population count, Salmon River, sediments, Siletz River, Siuslaw River, Tillamook Bay, Umpqua River, Yaquina River},
	url = {https://tinyurl.com/3nsruf33 },
	author = {Strickland, Matt J. and Anlauf-Dunn, Kara and Jones, Kim and Stein, Charles}
}
@book {80576,
	title = {The Northwest Coastal Explorer:  Your Guide to the Places, Plants, and Animals of the Pacific Coast},
	year = {2016},
	note = {Here{\textquoteright}s a guidebook with a difference.  Although suggested Pacific Northwest trips are included, this book is less about destinations and much more about the journey and what will be found along the way.  Packed with beautiful photographs and page-long descriptions of the plants and animals of the Northwest Coast, this book will inform and delight. For succinct descriptions of the life of the region, from the sea palm to the brown pelican, from the mole crab to the Roosevelt elk, this is the place to go for succinct species descriptions at a popular level.},
	pages = {283 p.},
	publisher = {Timber Pr},
	organization = {Timber Pr},
	chapter = {283 p.},
	address = {Portland, Or.},
	keywords = {amphibians, aquatic invertebrates, aquatic plants, biology, birds, general, general ecosystem description, geology, mammals, oceanography, terrestrial plants, tourism},
	author = {Steelquist, Robert}
}
@article {76981,
	title = {Coastal flood hazard study, Lincoln County, Oregon},
	volume = {no.O-15-06},
	year = {2015},
	note = {This is a technical document giving the factors and assumptions behind the flood hazard study. There are some colored maps and discussions of some sites, but it does not give the final maps.  {\textquotedblleft}The objective of the Lincoln County coastal flood hazard project is to develop a digital flood insurance rate map (DFIRM) and flood insurance study (FIS) report for Lincoln County, Oregon. . . DOGAMI has been contracted to perform detailed coastal flood hazard studies for the entire length of the Lincoln County shoreline of the Pacific Ocean.{\textellipsis}{\textquotedblright} (p.1)},
	pages = {351 p.},
	institution = {Oregon Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Alsea Bay, Alsea Spit, climate, coastal hazards, Depoe Bay, erosion, flooding, Fogarty Creek, geography, geology, Lincoln County (Or.), paleosciences, precipitation, Rocky Creek, Salmon River Estuary, Siletz Bay, Siletz Spit, Waldport (Or.), Whale Cove, Yachats (Or.), Yachats River, Yaquina Bay, Yaquina Head},
	url = {https://www.oregongeology.org/pubs/ofr/O-15-06_Lincoln.pdf },
	author = {Allan, Jonathan C. and Ruggiero, Peter and Cohn, Nick and Garcia, Gabriel and O{\textquoteright}Brien, Fletcher E. and Stimely, Laura L. and Roberts, Jed T.}
}
@article {76911,
	title = {A sea-level database for the Pacific coast of central North America},
	journal = {Quaternary Science Reviews},
	volume = {113},
	year = {2015},
	note = {When the glaciers melted at the end of the last ice age, sea levels along the Pacific Coast of North America did not rise uniformly.  Areas where the earth had been pressed down by the weight of glaciers saw relatively little sea level rise, as the land rebounded when the weight was removed.  Sites further away from the great glaciers saw higher sea levels.  In this paper, the authors describe a database of sea levels and reference points for the last 16,000 years in our area.  Appendices give reference points, descriptions, and referenced publications.  Interestingly, Alsea Bay in Appendix 1 is spelled {\textquotedblleft}Alsey Bay.{\textquotedblright}},
	month = {2015, Apr. 1},
	pages = {p.78-92},
	keywords = {Alsea Bay, Coos Bay, Coquille River, geology, Glaciation, Nehalem River, Nestucca Bay, Netarts Bay, paleosciences, Salmon River, sea level, Siletz Bay, Siuslaw River estuary, Yaquina Bay},
	doi = {10.1016/j.quascirev.2014.12.001},
	author = {Engelhart, Simon E. and Vacchi, Matteo and Horton, Benjamin P. and Nelson, Alan R. and Kopp, Robert E.}
}
@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 {11871,
	title = {Coastal subsidence in Oregon, USA, during the giant Cascadia earthquake of A.D. 1700},
	journal = {Quaternary Science Reviews},
	volume = {30},
	year = {2011},
	note = {This article represents an attempt to estimate how much subsidence occurred after the great Cascadia earthquake of 1700.  Stratigraphy is given for 5 rivers in Oregon, with subsidence estimates for each.  The estimate for the Salmon River is 0.6 m plus or minus .29 m},
	pages = {p.364-376},
	keywords = {Alsea Bay, coastal hazards, Coos Bay, earthquakes, geology, Nehalem River estuary, Nestucca River estuary, paleosciences, Salmon River Estuary, Siuslaw River estuary, South Slough},
	doi = {10.1016/j.quascirev.2010.11.017},
	url = {https://nora.nerc.ac.uk/id/eprint/13572/1/Hawkes_QSR_2011.pdf},
	author = {Hawkes, A.D. and Horton, B.P. and Nelson, Alan R. and Vane, C.H. and Sawai, Y.}
}
@article {51281,
	title = {Geochemistry and petrology of late Eocene Cascade Head and Yachats Basalt and alkalic intrusions of the central Oregon Coast Range, U.S.A.},
	journal = {Journal of Volcanology and Geothermal Research},
	volume = {198},
	number = {3-4},
	year = {2010},
	note = {Did the volcanic rocks in the Oregon Coast Range originate from {\textquotedblleft}magmetism associated with extension of the coast ranges{\textquotedblright} or did they come from {\textquotedblleft}hot spots associated with mantle plumes,{\textquotedblright} possibly even related to the Yellowstone hot spot? (p.311) The authors of this paper use geochemical and isotopic data to inform their discussion of the probable origins of these deposits. },
	month = {2010, Dec.15},
	pages = {p.311-324},
	keywords = {basalt, Blodgett Peak, Butler Peak, Cannibal Mountain, Cape Perpetua, Cascade Head Basalt, Cougar Mountain, geology, Heceta Head, Horner Ranch, paleosciences, Siletz River Volcanics, Table Mountain, volcanism, Yachats Basalt, Yaquina Head},
	doi = {10.1016/j.jvolgeores.2010.09.016},
	author = {Parker, D. F. and Hodges, F. N. and Perry, A. and Mitchener, M. E. and Barnes, M. A. and Ren, M.}
}
@inbook {51326,
	title = {Impacts of climate change on Oregon{\textquoteright}s coasts and estuaries},
	booktitle = {Oregon Climate Assessment Report},
	year = {2010},
	note = {This is Chapter 6 of the Oregon Climate Assessment Report. Predicts {\textquotedblleft}Increased winter{\textendash}early spring flow of coastal rivers and creeks and reduced flow during summer{\textquotedblright} for the Umpqua River (p.242)},
	pages = {p.211-268},
	publisher = {Oregon State University. College of Oceanic and Atmospheric Sciences. Oregon Climate Change Research Institute,},
	organization = {Oregon State University. College of Oceanic and Atmospheric Sciences. Oregon Climate Change Research Institute,},
	address = {Corvallis, Or.},
	keywords = {Alsea Bay, Alsea Spit, bacteria, Bayocean Spit, climate change, climate precipitation, coastal hazards, Columbia River estuary, Coos Bay, dissolved oxygen, El Nino, erosion, estuaries, geology, landslides, Nehalem Bay, Nehalem Spit, Neskowin (Or.), Netarts Bay, ocean acidification, Rockaway Beach, salinity, Salmon River Estuary, sea level, Siletz Bay, Tillamook Bay, water temperature, wave heights, Yachats River, Yaquina Bay},
	url = {https://digital.osl.state.or.us/islandora/object/osl\%3A637577},
	author = {Ruggiero, Peter and Brown, Cheryl A. and Komar, Paul D. and Allan, Jonathan C. and Reusser, Deborah A. and Lee II, Henry},
	editor = {Dello, Kathie and Mote, Philip W.}
}
@article {11921,
	title = {Rupture area and displacement of past Cascadia great earthquakes from coastal coseismic subsidence},
	journal = {Geological Society of America bulletin.},
	volume = {122},
	number = {11-12},
	year = {2010},
	month = {2010, Nov.},
	pages = {p.2079-2096},
	keywords = {Alsea Bay, Coos Bay, Coquille River, earthquakes, geology, Necanicum River, Nehalem River, Nestucca Bay, Netarts Bay, Salmon River, sediments, Siletz Bay, Siuslaw River, Sixes River, Tillamook Bay, tsunamis, Umpqua River, Yaquina Bay},
	doi = {10.1130/B30108.1},
	author = {Leonard, Lucinda J. and Currie, Claire A. and Mazzotti, Stephane and Hyndman, Roy D.}
}
@mastersthesis {51276,
	title = {Early Oligocene Intrusions in the Central Coast Range of Oregon : Petrography, Geochemistry, Geochronology and Implications for the Tertiary Magmatic Evolution of the Cascadia Forearc},
	year = {2006},
	note = {An interesting and thorough look at some of the basalt formations on the Oregon Coast. {\textquotedblleft}The OCRI [Oregon Coast Range Intrusions] represent the final episode of widespread forearc magmatism in Cascadia and record significant changes in tectonic interactions between the Farallon and North America plates. The new data acquired in this study have aided the evaluation of existing hypotheses on the tectonic origins of the OCRI suite and have identified new questions in determining their mantle sources. In future work, isotopic data (SR, Nd, Pb) will be necessary to further evaluate the distinctions in mantle sources between the alkaline and gabbroic OCRI.{\textquotedblright} (p.177) Includes maps, charts, color photographs of thin-sections of rocks. Major professor was Adam Kent.},
	pages = {237 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {basalt, Cape Foulweather, Cascade Head, geochemistry, geology, paleosciences, stratigraphy, theses, Yachats (Or.), Yachats Basalt, Yaquina Head},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/4j03d165r},
	author = {Oxford, Jeremiah}
}
@article {12156,
	title = {Evaluation of coastal erosion hazard zones along dune and bluff backed shorelines in Lincoln County, Oregon : [electronic resource] Cascade Head to Seal Rock},
	volume = {no.04-09},
	year = {2004},
	note = {disc 1. Text, appendices, maps in vector format, USGS digital orthophotos -- disc 2. Georeference orthophotos -- disc 3. Lincoln County 1993 orthophotos.},
	pages = {188 p.},
	address = {Newport, Or.},
	keywords = {coastal hazards, erosion, geology, landslides},
	url = {https://digital.osl.state.or.us/islandora/object/osl\%3A55381},
	author = {Priest, George R.}
}
@article {12161,
	title = {Great earthquakes and tsunamis of the past 2000 years at the Salmon River Estuary, Central Oregon Coast, USA},
	journal = {Bulletin of the Seismological Society of America},
	volume = {94},
	number = {4},
	year = {2004},
	note = {Examines four sets of buried soils at the entrance to the Salmon River. Definitive proof of the great tsunami of 1700; equivocal evidence of 3 earlier sudden subsidence events.},
	month = {2004, Aug.},
	pages = {p.1276-1292},
	keywords = {earthquakes, geology, paleoecology, Salmon River Estuary, tsunamis},
	doi = {10.1785/012003210},
	author = {Nelson, Alan R. and Asquith, Andrew C. and Grant, Wendy C.}
}
@article {12181,
	title = {Cascadia tsunami deposit database [electronic resource]},
	volume = {no.03-13},
	year = {2003},
	pages = {24 p.},
	address = {[Menlo Park, Calif.]},
	keywords = {bibliography, coastal hazards, earthquakes, geology, landslides, tsunamis},
	url = {https://pubs.usgs.gov/publication/ofr0313},
	author = {Peters, Robert and Jaffe, Bruce and Gelfenbaum, Guy and Peterson, Curt}
}
@article {36376,
	title = {Coastal shoreline change study, northern and central Lincoln County, Oregon},
	volume = {no.O-97-11},
	year = {1997},
	note = {This report is related to a series of erosion and flood control maps, Open-file reports no.97-12 {\textendash} 97-30.  It is also related to an earlier series of erosion maps, Open-file reports no.94-11 {\textendash} 94-30, the Chronic geologic hazard maps of coastal Lincoln County, Oregon, and covers the same territory. Readers of this report will probably be interested in Open-file report no.93-10, the Pilot erosion rate data study of the central Oregon coast, Lincoln County., which is a much longer report on erosion issues in this area. This report is concerned with mapping erosion reference features on a 31-mile stretch of the Oregon coast in Lincoln County, and including a 100-year flood zone reference in the maps.  The report touches briefly on erosion at the Siletz Spit, Gleneden Beach, Agate Beach, and Jump-off Joe.  Photocopies of aerial photographs and b+w photographs.},
	month = {1997, Nov.},
	pages = {19 p.},
	institution = {Oregon. Dept. of Geology and Mineral Industries,},
	address = {Portland, Or. },
	keywords = {Agate Beach, Alsea River, Beaver Creek, Cascade Head, coastal hazards, erosion, flooding, geology, Gleneden Beach, historical, Jump-Off Joe, landslides, Lincoln County (Or.), paleosciences, Salmon River, Seal Rock, Siletz River, Siletz Spit, Yaquina River},
	url = {https://pubs.oregon.gov/dogami/ofr/O-97-11.pdf},
	author = {Priest, George R.}
}
@article {12411,
	title = {Geologic map of the Cascade Head area, northwestern Oregon Coast Range: (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 minute quadrangles)},
	year = {1996},
	note = {Open-file report no.96-0534},
	publisher = {The Survey},
	address = {Reston, VA},
	keywords = {Cascade Head, Geologic formations, geology, map},
	url = {https://pubs.er.usgs.gov/publication/ofr96534},
	author = {Parke D. Jr. Snavely and Niem, Alan and Wong, Florence L. and Macleod, Norman S. and Calhoun, Tracy K. and U.S.  Geologial Survey,}
}
@article {12436,
	title = {Salmon River estuary hydrographic survey and analysis},
	year = {1995},
	note = {This is an engineer{\textquoteright}s review of several projects in the Salmon River area, including the Salmon Creek dike and possible dike removal, the Y Dike Ditch, Pixieland, Frazer Creek, basin lands and Knight Park.  Extensive work was done on tidal datums. Includes maps and author{\textquoteright}s notes.},
	keywords = {climate, Crowley Creek, Deer Creek, flooding, Frazer Creek, geology, hydrography, hydrology, precipitation, Salmon Creek, Salmon River, sediments, soils, streamflow, tides},
	url = {https://ir.library.oregonstate.edu/concern/technical_reports/gm80hw13k},
	author = {Coulton, Kevin G. and Crane \& Merseth and Philip Williams \& Associates and Siuslaw National Forest}
}
@article {36361,
	title = {Pilot erosion rate data study of the central Oregon coast, Lincoln County: Final report to the Federal Emergency Management Agency},
	volume = {no.O-93-10},
	year = {1993},
	note = {This report is related to Open-file reports nos. 94-11 - 94-30, the  Chronic geologic hazard maps of coastal Lincoln County, Oregon.  It also relates to a follow-up series of erosion and flood control maps, Open-file reports no.97-12 {\textendash} 97-30. Each segment of the coastline from Cascade Head to Seal Rock is described, along with the assumptions about the rate of erosion for that segment.  Appendices address the use of historical photographs to document shoreline change. Maps, charts, rather poor photocopies of b+w photographs.},
	month = {1993},
	pages = {228 p.},
	institution = {State of Oregon. Department of Geology and Mineral Industries},
	address = {Portland, OR},
	keywords = {Agate Beach, Alsea River, Beaver Creek, Cascade Head, coastal hazards, erosion, flooding, geology, historical, Jump-Off Joe, landslides, Lincoln County (Or.), Nye Beach, paleosciences, Salmon River, Seal Rock, Siletz River, Siletz Spit, Yaquina River},
	url = {https://digital.osl.state.or.us/islandora/object/osl:26613},
	author = {Priest, George R. and Saul, Ingmar and Diebenow, Julie}
}
@article {12511,
	title = {Petrology of Late Eocene basaltic lavas at Cascade Head, Oregon Coast Range},
	journal = {Journal of volcanology and geothermal research},
	volume = {52},
	number = {1-3},
	year = {1992},
	pages = {157-170},
	keywords = {Cascade Head, Geologic formations, geology},
	author = {Barnes, Melanie A. and Barnes, Calvin G.}
}
@article {12551,
	title = {The Salmon River Formation: a lower Eocene sequence in the central Oregon Coast Range.},
	journal = {U.S. Geological Survey Bulletin},
	volume = {no.1935},
	year = {1991},
	note = {Originally interpreted as part of the Siletz River Volcanics, the Salmon River Formation consists of rocks "eroded from, and deposited adjacent to, oceanic islands or seamounts formed by extrusion of the Siletz River Volcanics." The full bulletin can be viewed online by downloading a plug-in from USGS.  },
	pages = {p.1-4},
	keywords = {Geologic formations, geology, Salmon River Formation},
	url = {https://tinyurl.com/38jzukvj},
	author = {Parke D. Jr. Snavely}
}
@article {77181,
	title = {Paleogeographic evolution of the United States Pacific Northwest during Paleogene time},
	journal = {Canadian Journal of Earth Sciences},
	volume = {24},
	number = {8},
	year = {1987},
	note = {The period from 66-23.03 million years ago is known as the Paleogene.  It is the time when mammals experienced rapid evolution.  So did the Pacific Northwest.  This article summarizes the recent evolution of the region, from plate collisions to vulcanism, from faulting to sedimentation.},
	month = {08/1987},
	pages = {p.1652-1667},
	keywords = {general, geology, Pacific Northwest, paleosciences, Yachats Basalt},
	author = {Heller, Paul L. and Tabor, Rowland W. and Suczek, Christopher A.}
}
@mastersthesis {12676,
	title = {The stratigraphy and structure of the Columbia River basalt group in the Salmon River area, Oregon},
	year = {1986},
	note = {Maps, some colored.},
	pages = {108 p.},
	school = {Portland State University Dept. of Geology},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	keywords = {Columbia River basalts, Geologic formations, geology, map, paleosciences, theses},
	url = {https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=4592\&context=open_access_etds},
	author = {Burck, Martin Stuart}
}
@mastersthesis {12741,
	title = {Sedimentation in Small Active-Margin Estuaries of the Northwestern United States},
	year = {1983},
	note = {The author finds that the sediment composition of northwest coast estuaries can be "correlated with a hydrographic parameter HR (mean tidal-prism volume: mean fluvial discharge rate x 6 hours) computed for each bay."  Sedimentation is contrasted  in Alsea, Salmon River, Siletz, Siuslaw, and Tillamook bays and Grays Harbor.  An overview of the history of sedimentation in Alsea Bay over the last 10,000 years is given. },
	pages = {158 p.},
	school = {Oregon State University},
	type = {Doctoral dissertation},
	edition = {Ph. D.},
	chapter = {School of Oceanography},
	address = {Corvallis, Or.},
	keywords = {Alsea Bay, bathymetry, geology, Grays Harbor, hydrography, minerals, paleosciences, Salmon River Estuary, sea level, sediment data, sediments, Siletz Bay, Siuslaw Bay, species list, theses, tidal data, Tillamook Bay},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/vm40xw091},
	author = {Peterson, Curt D.}
}
@article {51261,
	title = {The relationship of morphology and material to landslide occurrence along the coastline in Lincoln County, Oregon},
	journal = {Oregon Geology},
	volume = {44},
	year = {1982},
	note = {{\textquotedblleft}The exact locations of 153 landslides were delineated within a 2. I-km-wide strip along the Lincoln County, Oregon, coastline.{\textquotedblright} (from the Abstract)  Map, tables, bw photographs of landslides, mostly from the Newport area.  A good read for anyone considering buying property on the coast.},
	month = {1982, Sep.},
	pages = {p.99-102},
	keywords = {Agate Beach, Alsea Bay, Bayshore Spit, Beaver Creek, Beverly Beach, Cape Foulweather, Cape Perpetua, Cascade Head, coastal hazards, erosion, geology, landslides, Lincoln City (Or.), Lincoln County (Or.), Newport (Or.), Nye Beach, Otter Crest, Siletz Bay, Waldport (Or.), Yachats (Or.), Yaquina Bay, Yaquina Head},
	url = {https://pubs.oregon.gov/dogami/og/OGv44n09.pdf},
	author = {Gentile, John Richard}
}
@mastersthesis {12786,
	title = {The geology of Cascade Head, an Eocene volcanic center},
	year = {1981},
	note = {Maps, 1 folded in pocket.},
	pages = {93 p.},
	school = {University of Oregon},
	type = {Masters Thesis},
	edition = {M. S.},
	chapter = {Dept. of Geology},
	address = {Eugene, Or.},
	keywords = {Cascade Head, Geologic formations, geology, theses},
	author = {Barnes, Melanie Ames Weed}
}
@article {13046,
	title = {Coastal landforms between Roads End and Tillamook Bay, Oregon},
	journal = {The Ore bin},
	volume = {36},
	number = {11},
	year = {1974},
	month = {1974},
	pages = {173-196},
	keywords = {Geologic formations, geology, guides},
	isbn = {0148-1827},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/c821gq001},
	author = {Lund, Ernest H. and Oregon. Department of Geology and Mineral Industries,}
}
@book {13076,
	title = {Geologic hazards inventory of the Oregon coastal zone},
	series = {Miscellaneous paper (Oregon. Dept. of Geology and Mineral Industries) },
	volume = {no.17},
	year = {1974},
	note = {Includes 2 folded color maps in pocket.},
	publisher = {[Oregon Department of Geology and Mineral Industries]},
	organization = {[Oregon Department of Geology and Mineral Industries]},
	address = {Portland, OR},
	keywords = {coastal hazards, erosion, geology, landslides},
	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,}
}
@article {13111,
	title = {Environmental geology of Lincoln County, Oregon},
	volume = {no.81},
	year = {1973},
	note = {Map packet available},
	institution = {Oregon Dept. of Geology \& Mineral Industries},
	address = {Portland, OR},
	keywords = {Alsea River, coastal hazards, Depoe Bay, engineering, geography, Geologic formations, geology, ground water, Lincoln County, minerals, Salmon River, Siletz River, Yachats River, Yaquina River},
	url = {https://www.oregongeology.org/pubs/B/B-081.pdf},
	author = {Schliker, Herbert G. and Deacon, Robert J. and Olcott, Gordon W. and Beaulieu, John D.}
}
@article {13256,
	title = {Technical Letter NASA-16: Geological evaluation of radar imagery, Oregon coast},
	year = {1966},
	note = {Work performed under NASA Contract No. R-09-020-015},
	month = {May_1966},
	institution = {United States Geological Survey},
	address = {Menlo Park, CA},
	keywords = {geology, remote sensing},
	author = {Snavely, Parke D. Jr. and Wagner, Holly C.}
}
@article {51271,
	title = {USDA Report on Water and Related Land Resources, Middle Coast Drainage Basin, Oregon:  Based on a Cooperative Survey by the State Water Resources Board of Oregon and the United States Department of Agriculture},
	year = {1964},
	note = {{\textquotedblleft}The State Water Resources Board of Oregon is making a survey and investigation of the Middle Coast Drainage Basin to develop information needed for planning the coordinated development of the area{\textquoteright}s water resources. The information needed for its study includes: (1) the kind and location of desirable water resource developments; (2) the amounts of water required; (3) the physical opportunities for developments to meet water needs; and (4) the broad economic aspects of possible development.{\textquotedblright} (from the Introduction) Includes b+w photographs, colored maps, tables. Nice overview of soils data.},
	pages = {138 p.},
	keywords = {agricultural, Alsea River Basin, Beaver Creek, climate, dams, demographics, Devils Lake, Duncan Slough, fishes, Five Rivers, flooding, general ecosystem description, geography, geology, historical, Lake Creek, land ownership, land use, logging, Otter Rock, recreation, Salmon River, Siltcoos Lake, Siuslaw River Basin, soils, terrestrial vegetation, water quality, water use, Wildcat Creek, wildlife, Yachats River, Yaquina River},
	url = {https://ir.library.oregonstate.edu/concern/defaults/1z40kx71v}
}
@article {13301,
	title = {Tertiary geologic history of western Oregon and Washington},
	volume = {no.22},
	year = {1963},
	month = {1963},
	address = {Olympia, WA},
	keywords = {geology, paleosciences, sediment data},
	url = {https://www.dnr.wa.gov/Publications/ger_ri22_tert_geol_west_or_wa.pdf},
	author = {Snavely, Parke D. Jr. and Wagner, Holly C. and Washington. Division of Mines and Geology,}
}
