@mastersthesis {83194,
	title = {Cementation and Groundwater Chemistry in Pleistocene Paleodune Deposits of the Central Oregon Coast},
	year = {2023},
	note = {Anyone who has driven along the Oregon coast has seen roadside deposits of light-colored rock close to the soil surface that looks like sand.  These are actually ancient sand dunes. Pleistocene paleodunes have some cementation, but often display slope instability. {\textquotedblleft}Weakening of cementing agents via changes to groundwater conditions due to altered vegetation, climate change, or contamination, for example, could promote slope instability, threatening lives and infrastructure. This study aims to investigate the variability in the type and degree of cementation and to determine how they are affected by changes in groundwater conditions{\textquotedblright} (from the Abstract). This interesting study addresses the Newport dune sheet, extending from Johnson Creek in the north to Yachats in the south. PSU Dissertations and Theses. Paper 6309.},
	pages = {118 p.},
	school = {Portland State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Portland, Or.},
	keywords = {Agate Beach, Alsea Bay, Beaver Creek, Beverly Beach, chemistry, coastal hazards, Driftwood Beach, erosion, geology, Johnson Creek Landslide, landslides, Ona Beach, paleosciences, Seal Rock, sediments, Yaquina Bay},
	doi = {https://doi.org/10.15760/etd.8163},
	url = {https://archives.pdx.edu/ds/psu/39676 },
	author = {Stephens, Adrienne Lynn}
}
@article {83117,
	title = {Differential coastal uplift quantified by luminescence dating of marine terraces, central Cascadia forearc, Oregon},
	journal = {Quaternary Science Reviews},
	volume = {298},
	number = {107853},
	year = {2022},
	note = {At Yaquina Bay, there are marine terraces north and south of the bay. Although these terraces were deposited at the same time, they now have different elevations.  This fact implies differential displacement along a fault in Yaquina Bay.  The authors report on a study using luminescence dating to help determine what is happening in this area.  {\textquotedblleft}Our results confirm that Yaquina Bay has been active during the late Pleistocene, and it also appears that the fault has experienced significant variations in displacement over the last 125 kyrs, and that a significant amount of displacement accrued during a relatively short time period post-106 ka{\textquotedblright} (p.13, section 6.1, {\textquotedblleft}Faulting at Yaquina Bay{\textquotedblright}).},
	month = {2022, Dec.15},
	pages = {16 p.},
	keywords = {coastal hazards, earthquakes, Faults, geology, paleosciences, tsunamis, Yaquina Bay},
	doi = {https://doi.org/10.1016/j.quascirev.2022.107853 },
	author = {McKenzie, K.A. and Kelsey, H.M. and Kirby, E. and Rittenour, T.M. and Furlong, K.P.}
}
@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 {82536,
	title = {Drainage evolution and freshwater fish zoogeography in coastal Oregon and Washington},
	journal = {Northwestern Naturalist },
	volume = {100  },
	number = {2  },
	year = {2019},
	note = {Some of the major events that have affected the evolution of fishes on the Pacific Northwest Coast include Miocene basalt flows, the rise of the Coast Range, glaciation and geographic isolation. This most interesting article examines the evolutionary history and species richness (or lack of it) in freshwater fishes in the region. {\textquotedblleft}My purpose is to describe discrete geographic areas based on geological features, habitat, and distribution discontinuities in coastal freshwater fishes in Oregon and Washington{\textquotedblright} (p.73).},
	month = {2019, Autumn},
	pages = {p.71-89   },
	keywords = {Alsea River, Chehalis River, Chetco River, Columbia River, Coos River, Coquille River, evolutionary biology, fishes, geographic distribution, geography, geology, habitats, Klamath River, Nehalem River, Nestucca River, Olympic mudminnow = Novumbra hubbsi, Oregon chubs = Oregonichthys spp., paleosciences, Puget Sound, Rogue River, salinity, Siletz River, Siuslaw River, Sixes River, Trask River, Umpqua River, Willapa Bay, Yaquina River},
	doi = {https://doi.org/10.1898/NWN-18-18 },
	author = {Markle, Douglas F.}
}
@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.}
}
@mastersthesis {83171,
	title = {Finding Submerged Sites:  An Exploration of Shoreline and Environmental Change in Oregon{\textquoteright}s Yaquina River Basin using GIS Predictive Modeling},
	year = {2018},
	note = {Where is the evidence of early human occupation of coastal Oregon?  Much of it is believed to be underwater, drowned as sea levels have risen.  In this Masters thesis, the author used GIS shoreline mapping and modeling to predict shoreline location at different times in the past 20,000 years.  She found that the sea level was relatively constant from 20,000 to 11,000 years ago, but underwent a dramatic change from 10,000 to 8,000 years ago, as sea levels rose.  Change has been more incremental in the last 8,000 years.  {\textquotedblleft}By increasing our understanding of this landscape through time, this study will aid in our ability to protect submerged archaeological materials that may be contained in these currently offshore areas{\textquotedblright} (from the Abstract).   The thesis is accompanied by a dataset for finding submerged sites using GIS predictive modeling at: https://ir.library.oregonstate.edu/concern/datasets/sn00b3861 . Colored maps.  The major professor was Loren G. Davis.},
	pages = {69 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {School of Language, Culture, and Society. Applied Anthropology},
	address = {Corvallis, Or.},
	keywords = {anthropology, archeology, geography, mathematical modeling, paleosciences, sea level, Shoreline, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/5712mc48k },
	author = {Nuss, Kathryn F.}
}
@article {83166,
	title = {Were they all giants?  Perspectives on late Holocene plate-boundary earthquakes at the northern end of the Cascadia subduction zone},
	journal = {Quaternary Science Reviews},
	volume = {169},
	year = {2017},
	note = {While this article is focused on the northern end of the Cascadia Subduction Zone, it offers an up-to-date look at research on prehistoric tsunamis on the West Coast.  The authors attempt to match buried soils in southwest Washington that show seven different tsunamis with evidence on Vancouver Island.  They also note what can be correlated with earthquake evidence from the entire subduction zone.  The authors found that three earthquakes were definitely caused by a rupture of the entire plate margin.  Three other earthquakes left tsunami evidence in the north, but the deposited soils have not yet been accurately dated.  One earthquake seems to have taken place in the north, but is not well correlated in the south, indicating a possible partial plate rupture.},
	pages = {p.29-49},
	keywords = {coastal hazards, Coos Bay, earthquakes, Ecola Creek, geology, Lagoon Creek, Nestucca Bay, Netarts Bay, paleosciences, Talbot Creek (Coos Bay), tsunamis, turbedites, Vancouver Island, Washington (State), Yaquina Bay},
	doi = {http://dx.doi.org/10.1016/j.quascirev.2017.05.015},
	author = {Hutchinson, Ian and Clague, John J.}
}
@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 {76331,
	title = {Differential drivers of benthic foraminiferal and molluscan community composition from a multivariate record of early Miocene environmental change},
	journal = {Paleobiology},
	volume = {40 },
	year = {2014},
	note = {This is a study of the early Miocene Newport member of the Astoria Formation.  The Newport Member was deposited about 20.26-18 million years ago.  It offers an approximately 2 million year {\textquotedblleft}time series of benthic foraminifera and molluscs from continental shelf depths, allowing investigation of both groups in the same record.{\textquotedblright} (p.399)  Since there was an interval of global warming in this time period, the authors wondered what the sediments would tell researchers about how marine environments reacted to climate change.  The answer is {\textellipsis} complicated. As the authors observe, {\textquotedblleft}Environmental changes are multivariate in nature.{\textquotedblright} (p.414)  A most interesting look at a complex subject.},
	month = {2014, Summer},
	pages = {p. 398-416},
	keywords = {aquatic invertebrates, Beverly Beach State Park, bivalves, carbon, climate change, foraminifera, geology, Jump-Off Joe, molluscs, Moolach Beach, oxygen, paleontology, paleosciences, primary productivity, Schooner Point, sediments, temperature, Wade Creek, Yaquina Head},
	doi = {10.1666/13019},
	author = {Belanger, Christina L. and Villarosa Garcia, Marites}
}
@article {54876,
	title = {Records of trace metals in sediments from the Oregon shelf and slope: Investigating the occurrence of hypoxia over the past several thousand years},
	journal = {Chemical Geology },
	volume = {382},
	year = {2014},
	note = {In recent years, strong coastal winds have caused strong upwelling events, so strong that a layer of low-oxygen seawater has been brought closer to the surface, leading to mass die-offs of marine life, and affecting estuarine waters as well.  A current question about these hypoxic events has to do with whether or not they are related to climate change.  A look at the history of the region is therefore called for.  {\textquotedblleft}A record of past hypoxia occurrence frequency would help distinguish human-induced causes from those related to natural climate changes. . . .  Determining trends in trace metal abundances can serve as an indicator for changes in oxygenation conditions over time.{\textquotedblright} (p.33) The authors look at trace metals in sediments from the Yaquina, Alsea and Siuslaw Rivers and consider other factors possibly influencing their data. {\textquotedblleft}Supplementary data to this article can be found online at http://dx.doi.org/10.1016/j.chemgeo.2014.05.029 .{\textquotedblright} (p.42)},
	month = {2014, Aug.29},
	pages = {p.32{\textendash}43},
	keywords = {Alsea Bay, chemistry, climate change, dissolved oxygen, hypoxia, paleosciences, sediments, Siuslaw Bay, Trace metals, winds, Yaquina Bay},
	doi = {10.1016/j.chemgeo.2014.05.029},
	author = {Erhardt, Andrea M. and Reimers, Clare E. and Kadko, David and Paytan, Adina}
}
@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.}
}
@inbook {34431,
	title = {Lower Columbia and Oregon Coast},
	booktitle = {Oregon Archaeology},
	year = {2011},
	note = {"Rising sea levels and a dynamic, high-energy coast present significant challenges for Oregon coast archeology.  The surviving record is strongly biased to within the last ca. 1,500 years, and it is certain that scores of ancient occupation sites have disappeared due to erosion and rising sea levels.  Human presence along the Oregon coast is confirmed by at least 8,000 years ago, but evidence from Pacific coasts to the north and south (and possible evidence from the Oregon coast itself) assures us that people were present thousands of years earlier." (p.282) A valuable summary of current knowledge of ancient peoples. Maps, line drawings, photographs of artifacts. },
	pages = {p.210-283},
	publisher = {Oregon State University Press},
	organization = {Oregon State University Press},
	address = {Corvallis, Or.},
	keywords = {archeology, Bandon Sandspit, bob Creek, Boiler Bay, Cape Blanco, Cape Perpetua, Columbia River, Coos Bay, Coquille River, Ecola Creek, Graveyard Point, K{\textquoteright}ama{\textquoteright}cdun, Necanicum River estuary, Neptune State Park, Netarts Sandspit, paleosciences, Pistol River, Rogue River, Seal Rock, Siltcoos Lake, Siuslaw River, Spencer Bridge, Tahkenitch Lake, Umpqua River, Umpqua-Eden, Whale Cove, Yaquina Falls, Yaquina Head, Yaquina River},
	author = {Aikens, C. Melvin and Connolly, Thomas J. and Jenkins, Dennis L.}
}
@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.}
}
@article {80251,
	title = {Inflorescences and compound leaves of the extinct <i>Platanus neptuni</i> complex in the Oligocene of Oregon, USA},
	journal = {Acta Palaeobotanica},
	volume = {50},
	year = {2010},
	note = {On the central Oregon coast, terrestrial fossils are rarely found.  This article describes the dominant flora species that seems to have flourished about 28 million years ago, on land on a deltaic plain of the ancestral Yaquina River.  The fossils of this extinct species were found between the upper and lower marine tongues of the Yaquina Formation. The article discusses the taxonomy and worldwide distribution of the Platanus genus and mentions associated flora.  The fossils recovered on Yaquina Bay are now housed in the U.S. National Museum.},
	pages = {p.5-15},
	keywords = {fossils, geology, Oligocene, paleosciences, taxonomy, terrestrial vegetation, The Bend, Yaquina Formation, Yaquina River},
	author = {Manchester, Steven R. and Kva{\v c}ek, Zlatko}
}
@inbook {34276,
	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 resemblance 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.  Includes maps showing paleorivers and what was above water before all the ice melted.},
	pages = {p.332-348},
	publisher = {Geological Society of America},
	organization = {Geological Society of America},
	address = {Boulder, Colo.},
	keywords = {archeology, Florence dune sheet, geology, Neptune State Park, Oregon State University Hatfield Marine Science Center, paleosciences, subsidence, tsunamis, Yaquina Bay, Yaquina Head},
	url = {https://www.researchgate.net/publication/290241966_Geoarchaeological_themes_in_a_dynamic_coastal_environment_Lincoln_and_Lane_Counties_Oregon},
	author = {Davis, Loren G. and Jenevein, Steven A. and Punke, Michele L. and Noller, Jay S. and Jones, Julia A. and Willis, Samuel C.}
}
@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}
}
@mastersthesis {33986,
	title = {Geologic Model and Geotechnical Properties of Stratified Paleodune Deposits, Central Oregon Coast, Oregon},
	year = {2005},
	note = {This study found a significant number of weak cements in paleodune deposits, which has significant implications for slope stability for those building on ancient dune deposits.  Pleistocene dune strata was characterized as "brittle." Numerous color photographs, charts and tables.},
	pages = {264 p.},
	school = {Portland State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Portland, Or.},
	keywords = {Beaver Creek, Canary Road, geology, landslides, Lincoln County, Ona Beach, paleosciences, Pinecrest, Siuslaw River, theses},
	url = {https://web.pdx.edu/~i1kc/geolinq/thesis/texts/171-Clough-2005.pdf},
	author = {Clough, Charles M.}
}
@article {33746,
	title = {<i>Simocetus rayi </i>(Odontoceti: Simocetidae, New Family): a bizarre new archaic Oligocene dolphin from the Eastern North Pacific},
	journal = {Smithsonian Contributions to Paleobiology},
	volume = {no.93},
	year = {2002},
	note = {Describes a fossil skull of an unusual archaic dolphin, which "was perhaps a bottom feeder that preyed through suction feeding on soft-bodied invertebrates." This species is believed to have had echolocation abilities. The specimen was found "[near the] intersection of North Yaquina Bay Road and Toledo Road, Lincoln County, USA."},
	pages = {p.185-222},
	keywords = {Alsea Formation, marine mammals, new species description, paleosciences, taxonomy, Yaquina River},
	author = {Fordyce, R. Ewan}
}
@inbook {76661,
	title = {Magnetic stratigraphy and tectonic rotation of the Oligocene Alsea, Yaquina, and Nye Formations, Lincoln County, Oregon},
	booktitle = {Magnetic stratigraphy of the Pacific Coast Cenozoic : a symposium volume based on Proceedings of the 1997 Pacific Section AAPG-SEPM Meeting, Bakersfield, California, and the 2001 Pacific Section AAPG-SEPM-Cordilleran Section GSA Meeting},
	series = {Book (SEPM (Society for Sedimentary Geology). Pacific Section) },
	volume = {91},
	year = {2001},
	note = {{\textquotedblleft}The Alsea Formation, Yaquina Sandstone, and Nye Mudstone make up a sequence of almost 3300 m of Oligocene-Miocene marine strata.  It is one of the thickest and most continuous records of the mid-Cenozoic in Oregon, yet dating of these rocks has been imprecise in the past.{\textquotedblright} (from the Abstract)},
	pages = {p.184-194},
	publisher = {Pacific Section SEPM},
	organization = {Pacific Section SEPM},
	address = {Fullerton, CA},
	keywords = {Alsea Bay, Alsea Formation, geology, Magnetism, microfossils, Nye Mudstone, paleosciences, plankton, stratigraphy, Yaquina Bay, Yaquina Sandstone},
	author = {Prothero, Donald R. and Bitboul, Clio Z. and Moore, George W. and Niem, Alan R. and American Association of Petroleum Geologists. Pacific Section, and Geological Society of America. Cordilleran Section,}
}
@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 {33071,
	title = {A century and a half of change in the climate of the NE Pacific},
	journal = {Fisheries Oceanography},
	volume = {4},
	number = {4},
	year = {1995},
	note = {Concentrates mostly on British Columbia},
	month = {1995},
	pages = {267-277},
	keywords = {air temperature, climate, El Nino, paleosciences, physical, Yaquina Bay},
	author = {Ware, D. M.}
}
@article {33026,
	title = {Preliminary reconnaissance survey of Cascadia paleotsunami deposits in Yaquina Bay, Oregon},
	journal = {Oregon Geology},
	volume = {57},
	number = {2},
	year = {1995},
	month = {March_1995},
	pages = {33-40},
	keywords = {coastal hazards, geological, Grassy Point, Idaho Flats, King Slough, paleosciences, Parker Slough, Pooles Slough, Sally{\textquoteright}s Bend, sediment data, tsunamis, Yaquina Bay},
	url = {https://pubs.oregon.gov/dogami/og/OGv57n02.pdf},
	author = {Peterson, Curt D. and Priest, George R.}
}
@article {32886,
	title = {Stratigraphic evidence for great subduction-zone earthquakes at four estuaries in northern Oregon, USA},
	journal = {Journal of Coastal Research},
	volume = {10},
	number = {4},
	year = {1994},
	month = {Fall_1994},
	pages = {850-876},
	keywords = {Boone Slough, Butler Bridge, coastal hazards, geological, Idaho Flats, Mill Creek, Necanicum River estuary, Nestucca River estuary, paleosciences, Pooles Slough, Siletz River estuary, Yaquina Bay},
	author = {Darienzo, Mark E. and Peterson, Curt D. and Clough, Charles}
}
@mastersthesis {52026,
	title = {Late Quaternary Crustal Deformation on the Central Oregon Coast as Deduced from Uplifted Wave-Cut Platforms},
	year = {1993},
	note = {This thesis examines marine terraces on the central Oregon Coast to see what they can tell us about uplift and deformation processes in the recent geologic past.  {\textquotedblleft}The primary purpose of this project is to study the characteristics, age, and distribution of uplifted marine terraces along 65 km of the central Oregon coast between Otter Rock and Searose beach.  . . . Quaternary deformation of marine terraces is used to determine the rate and variability of uplift.{\textquotedblright} (p.1) Includes geologic maps.},
	pages = {70 p.},
	school = {Western Washington University},
	type = {Masters Thesis},
	edition = {M. S.},
	address = {Bellingham, Wash.},
	keywords = {Alsea Bay, earthquakes, geology, Moolach Beach, Otter Rock, paleosciences, sea level, Searose Beach, soils, theses, Yachats River, Yaquina Bay},
	author = {Ticknor, Robert}
}
@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}
}
@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}
}
@inbook {32556,
	title = {Alseans},
	booktitle = {Northwest Coast},
	series = {Handbook of North American Indians},
	volume = {7},
	year = {1990},
	note = {General overview of what was known about the Alsean people in the late 1980s. Brief treatment of Native American history and culture. "...the Alseans being the southernmost people to have set their dead above the ground, in canoes or charnel houses." (p.568)},
	pages = {p.568-571},
	publisher = {Smithsonian Institution},
	organization = {Smithsonian Institution},
	address = {Washington, D.C.},
	keywords = {Alsea Bay, anthropology, Beaver Creek, geographic distribution, historical, Native Americans, paleosciences, Yachats River, Yaquina Bay},
	author = {Zenk, Henry B.}
}
@article {80211,
	title = {The Jump-Off Joe landslide at Newport, Oregon: history of erosion, development and destruction},
	journal = {Shore and Beach },
	volume = {v.56 },
	year = {1988},
	note = {In the winter of 1942-1943, a block of about 15 acres of land on which 15 houses were located, slumped and slid towards the sea.  This happened in the {\textquotedblleft}Jump-Off Joe{\textquotedblright} area of Newport, a location that has the highest rate of erosion on the Oregon Coast.  In 1982, developers built a condominium in the same area.  The project was approved by Newport city government, and some geologists claimed that it was safe, although it was next to an active landslide.  Environmentalists objected.  Nature settled the argument.  This article gives a good history of the area and is an excellent cautionary tale.  Good map, lots of photographs.},
	month = {1988, Jul.},
	pages = {p.15-21},
	keywords = {coastal hazards, erosion, geology, Jump-Off Joe, landslides, Newport (Or.), Nye Beach, paleosciences},
	author = {Sayre, William O. and Komar, Paul D.}
}
@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.}
}
@inbook {30926,
	title = {Beach processes and erosion problems on the Oregon Coast},
	booktitle = {Geologic field trips in Western Oregon and Southwestern Washington},
	series = {Bulletin (Oregon. Dept. of Geology and Mineral Industries)},
	volume = {no.101},
	year = {1980},
	note = {Includes road trip log for the Jumpoff Joe area of Newport, Siletz Spit, and Taft area of Lincoln City.},
	month = {March_1980},
	pages = {p.169-173},
	publisher = {Oregon Department of Geology and Mineral Industries},
	organization = {Oregon Department of Geology and Mineral Industries},
	keywords = {coastal dunes, coastal hazards, environmental education, erosion, geological, Jump-Off Joe, Lincoln City (Or.), paleosciences, Salishan Spit, Siletz Bay, Siletz Spit, Taft (Or.)},
	url = {https://www.oregongeology.org/pubs/B/B-101.pdf},
	author = {Komar, Paul D. and Schlicker, Herb}
}
@article {30851,
	title = {Geologic field trips in Western Oregon and Southwestern Washington},
	volume = {no.101},
	year = {1980},
	month = {March_1980},
	pages = {232 p.},
	institution = {Oregon Department of Geology and Mineral Industries},
	keywords = {coastal dunes, environmental education, geological, paleosciences},
	url = {https://www.oregongeology.org/pubs/B/B-101.pdf},
	editor = {Oles, Keith F. and Johnson, J. Granville and Niem, Alan R. and Niem, Wendy A.}
}
@inbook {31016,
	title = {Geology of the west-central part of the Oregon Coast Range},
	booktitle = {Geologic field trips in Western Oregon and Southwestern Washington},
	series = {Bulletin / State of Oregon, Department of Geology and Mineral Industries},
	volume = {no.101},
	year = {1980},
	note = {Includes field trip log.  Day 1:  From Toledo to Yaquina Bay Road to Newport, then south to Cape Perpetua.  Day 2:  From Newport north to Siletz Bay, then east to Siletz gorge area, back to Newport.},
	month = {March_1980},
	pages = {p.39-76},
	publisher = {Oregon Department of Geology and Mineral Industries},
	organization = {Oregon Department of Geology and Mineral Industries},
	keywords = {coastal dunes, environmental education, geological, paleosciences},
	url = {https://www.oregongeology.org/pubs/B/B-101.pdf},
	author = {Parke D. Jr. Snavely and NMacLeod, N. S. and Wagner, H. C. and Lander, D. L.}
}
@mastersthesis {36636,
	title = {The Delineation of Landslides in the Lincoln County, Oregon Coastal Zone},
	year = {1978},
	note = {{\textquotedblleft}A study conducted along the Lincoln County, Oregon coast delineated the exact location of 153 landslides. The landslides were found through the interpretation of aerial photographs.{\textquotedblright} The slides were mapped, analyzed and classified as ancient, historic or recent.  {\textquotedblleft}It was found that most landslides occur in conjunction with silt stone materials of Tertiary age. Areas with similar morphology but of sandstone materials are less likely to have landslides. Structurally, landslides occur in areas with steeply dipping Tertiary bedding planes or in areas with steep slopes such as river valleys. A large portion of the landslides in the study area occur at contact zones between Tertiary and Quaternary materials. Most of these slides are ancient, stable slides and are larger than other slides in the study area. The only active ancient landslides in the coastal zone take place in the Nye mudstones near Beverly Beach State Park.{\textquotedblright} (from the Abstract) Appendices list slides, summarize their characteristics and show them on a map of the county.  This is a research paper taking the place of a thesis, {\textquotedblleft}in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE.{\textquotedblright} },
	pages = {36 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geography},
	address = {Corvallis, Or.},
	keywords = {Agate Beach, Alsea Bay, Beaver Creek, Beverly Beach, Big Creek, Boiler Bay, Cape Foulweather, Cape Perpetua, coastal hazards, Depoe Bay (Or.), erosion, geography, geology, Jump-Off Joe, landslides, Lincoln City (Or.), Lincoln County (Or.), Lint Slough, Newport (Or.), Otter Rock, paleosciences, physical, Roads End, Seal Rock, Siletz Bay, theses, Waldport (Or.), Yachats (Or.), Yachats River, Yaquina Head},
	url = {https://ir.library.oregonstate.edu/concern/graduate_projects/x633f166m},
	author = {Gentile, John Richard}
}
@mastersthesis {80316,
	title = {Paleobotany and Stratigraphy of the Yaquina Flora (Latest Oligocene-Earliest Miocene) of Western Oregon},
	year = {1978},
	note = {The Yaquina Formation was deposited in Western Oregon at the end of the Oligocene period and the beginning of the Miocene.  There were three major depositional events, two in shallow marine environments, and one on land.  The later deposits were formed on a delta of the ancestral Yaquina River, and provide a unique look at what life was like on land about 25 million years ago.  Although there are a few animal fossils in this Middle Non-Marine Member, the overwhelming majority of fossils are of plants, and they are the subject of this most interesting Master{\textquoteright}s thesis.  The fossil record points to a major warming event at the time, and the author finds the Yaquina flora resembles {\textquotedblleft}a marginally subtropical evergreen broad-leaved forest{\textquotedblright} with abundant climbing vines (p.65).},
	pages = {192 p.},
	school = {University of Maryland},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Botany},
	address = {College Park, Md.},
	keywords = {botany, general ecosystem description, geology, paleosciences, taxonomy, theses, Yaquina Bay, Yaquina Formation, Yaquina River},
	author = {McClammer, James Upsher, Jr.}
}
@article {30256,
	title = {Water resources of Lincoln County coastal area, Oregon},
	volume = {no.76-90},
	year = {1977},
	note = {Excellent data.  Map in back pocket},
	pages = {63 p.},
	keywords = {chemical, climate, demographics, general ecosystem description, geological, Lincoln County, paleosciences, physical, precipitation data, sediment data, water quality data, Yaquina Bay, Yaquina River, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/defaults/5425kb57g},
	author = {Frank, F. J. and Laenen, Antonius and Oregon. Water Resources Dept. and U.S. Geological Survey. Water Resources Division,}
}
@mastersthesis {51286,
	title = {Drainage Basin Morphology in the Central Coast Range of Oregon},
	year = {1976},
	note = {This is a fascinating look back at the origins of the ancestral Siletz-Luckiamute and Yaquina-Mary{\textquoteright}s Rivers.  {\textquotedblleft}The wind gaps, barbed drainages, valley sizes, and scale of the large meanders suggest that each pair of streams in the central Coast Range (one pair consists of one westward-flowing stream and one eastward-flowing stream) represents a single ancient stream system which was severed during uplift of the Coast Range.{\textquotedblright} (from the Abstract)  Maps, color photographs. Major professor was James F. Lahey. },
	pages = {112 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geography},
	address = {Corvallis, Or.},
	keywords = {Beaver Creek (Siletz), Boulder Creek, geography, geology, hydrology, Luckiamute River, Mary{\textquoteright}s River, paleosciences, sediments, Siletz River, South Fork Siletz River, theses, Warnick Creek, Yaquina River},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/q811kn699},
	author = {Niem, Wendy A.}
}
@article {52036,
	title = {Fossil marine mammals of Oregon},
	journal = {Systematic Zoology},
	volume = {25},
	year = {1976},
	note = {This interesting article gives a history of the discovery of marine mammal fossils in Oregon.  Most of the article is concerned with a remarkable and extensive collection of fossils amassed by Douglas Emlong, of Lincoln City, Oregon, {\textquotedblleft}who has already secured a special place in the history of vertebrate paleontology by collecting more marine mammal fossils of more kinds and more ages than anyone,{\textquotedblright} (p.433) and who gave his collection to the Smithsonian.},
	month = {1976, Dec. },
	pages = {p. 420-436},
	keywords = {aquatic mammals, Beaver Creek, Cape Blanco, Coos Bay, Fossil Point, fossils, geology, historical, Johnson Creek, Lincoln Beach, Lincoln City (Or.), Myrtle Point, Newport (Or.), paleontology, paleosciences, Schooner Creek, Spencer Creek, Sunset Bay, Tillamook Bay, Yachats (Or.), Yaquina Bay, Yaquina River},
	author = {Ray, Clayton E.}
}
@article {36121,
	title = {Rock units and coastal landforms between Newport and Lincoln City, Oregon},
	journal = {Ore Bin},
	volume = {36},
	number = {5},
	year = {1974},
	note = {Although our understanding of vulcanism on the Oregon Coast has evolved since this article was written, it is still a useful guide for the interested layperson.  Includes bw photographs and geological maps.},
	month = {1974, May},
	pages = {p.69-90},
	keywords = {Boiler Bay, Cape Foulweather, coastal hazards, Depoe Bay, Devil{\textquoteright}s Punchbowl, erosion, Fogarty Creek, geology, Jump-Off Joe, Lincoln Beach, Otter Rock, paleosciences, Siletz Bay, Siletz River, Siletz Spit, Whale Cove, Yaquina Bay, Yaquina Head, Yaquina River},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/2f75rd38k},
	author = {Lund, Ernest H.}
}
@article {29531,
	title = {Environmental geology of Lincoln County, Oregon},
	volume = {no.81},
	year = {1973},
	note = {Map packet available},
	month = {September_1973},
	pages = {171 p.},
	institution = {State of Oregon.  Department of Geology and Mineral Industries},
	address = {Portland, OR},
	keywords = {Alsea River estuary, coastal hazards, environmental policy and law, general ecosystem description, geological, human impacts, hydrology, industrial development, land use, natural resource management, paleosciences, Salmon  River estuary, sediment data, Siletz River estuary, urban development, water quality, water rights, Yaquina Bay, Yaquina River, Yaquina River Basin},
	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.}
}
@mastersthesis {29426,
	title = {Stratigraphy and Sedimentation of the Yaquina Formation, Lincoln County, Oregon},
	year = {1973},
	note = {Major professor was Dr. Alan R. Niem. Masters thesis.},
	month = {1973},
	pages = {121 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {geological, paleosciences, sediment data, theses, Yaquina Bay, Yaquina River, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/m326m632g},
	author = {Goodwin, Clinton J.}
}
@inbook {29481,
	title = {Volcanics and intrusive rocks of the central part of the Oregon coast range},
	booktitle = {Geologic field trips in northern Oregon and southern Washington},
	series = {Bulletin (Oregon. Dept. of Geology and Mineral Industries)},
	volume = {no.77},
	year = {1973},
	note = {Good local field trips.},
	month = {March_1973},
	pages = {p.47-74},
	publisher = {Oregon Department of Geology and Mineral Industries},
	organization = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {chemical, environmental education, geological, paleosciences, sediment data, Yaquina River, Yaquina River Basin},
	url = {https://www.oregongeology.org/pubs/B/B-077.pdf},
	author = {Macleod, Norman S. and Snavely, Parke D.},
	editor = {Beaulieu, John D.}
}
@article {36116,
	title = {Coastal landforms between Yachats and Newport, Oregon},
	journal = {Ore Bin},
	volume = {34},
	number = {5},
	year = {1972},
	note = {Still useful after all these years, this guide offers a road log, geological maps and bw photographs.},
	month = {1972, May},
	pages = {p.73-91},
	keywords = {Alsea Bay, Alsea River, Beaver Creek, Big Creek, erosion, geology, Ona Beach, paleosciences, Seal Rock, Yachats River, Yaquina Bay. Yaquina River},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/v692tb779},
	author = {Lund, Ernest H.}
}
@mastersthesis {55391,
	title = {Stratigraphy and Sedimentation of the Yaquina Formation, Lincoln County, Oregon},
	year = {1972},
	note = {Master{\textquoteright}s thesis.  Major professor was Alan R. Niem.  While other formations in the Newport area (e.g., Alsea Formation, Nye Mudstone) indicate that the region was in the deeper ocean, the Oligocene Yaquina Formation was deposited in shallow seas, or on land. Several layers were deposited in river deltas. This thesis describes the regional geology, stratigraphy, lithology, petrology, age, depositional ecology and economic potential of the formation. It includes color photographs and microscopic photographs of thin-sections of rocks. It is accompanied by two plates: a colored geologic map and columnar sections.},
	pages = {121 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M. S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {Beaver Creek, Depoe Bay, fossils, geology, Johnson Creek, North Depoe Bay Creek, Oligocene, Oneatta Point, paleosciences, Rocky Creek, Seal Rock, Siletz Bay, South Depoe Bay Creek, species list, theses, Thiel Creek, Yaquina Bay, Yaquina Formation},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/m326m632g},
	author = {Goodwin, Clinton John}
}
@article {28781,
	title = {Geology of the Newport area, Oregon. Part I - geologic sketch of the Newport Area, Oregon},
	journal = {The Ore Bin},
	volume = {31},
	number = {2},
	year = {1969},
	note = {Part 1 of a field trip guide to the Newport area, "Geologic Sketch of the Newport Area, Oregon."  Part II is the road trip guide.},
	month = {February_1969},
	pages = {p.25-71},
	keywords = {aquatic invertebrates, foraminifera, geological, paleosciences, sediment data, Yaquina Bay, Yaquina River, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/6969z5023},
	author = {Snavely, Parke D. Jr. and Macleod, Norman S. and Rau, Weldon W.}
}
@article {83155,
	title = {Geology of the Newport area, Oregon: Part II. geologic field trip guide, Newport area, Oregon},
	journal = {The Ore Bin},
	volume = {31},
	number = {3},
	year = {1969},
	note = {{\textquotedblleft}The field trip consists of two geologic tours. On Tour 1, the Tertiary sedimentary rocks exposed along the Yaquina River between Newport and Toledo, Oregon, will be examined. .. Tour 2 is primarily concerned with volcanic rocks of early Eocene, late Eocene, and middle Miocene age that form important stratigraphic units in the Oregon Coast Range.{\textquotedblright} (p.49) Tour 1 runs west-to-east from Newport to Toledo; Tour 2 runs south-to-north from Cape Foulweather to Siletz Bay, then east along the Siletz River, ending at a private quarry. Maps, colored geologic maps and black-and-white photographs are included.},
	month = {1969, Mar.},
	pages = {p.49-71},
	keywords = {aquatic invertebrates, Boiler Bay State Park, Cape Foulweather, Depoe Bay, Fogarty Creek State Park, foraminifera, geological, Government Point, Kernville (Or.), Newport (Or.), paleosciences, sediment data, Siletz Bay, Siletz River, Toledo (Or.), volcanism, Yaquina Bay, Yaquina River, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/3t945w39p},
	author = {Snavely, Parke D. Jr. and Macleod, Norman S. and Rau, Weldon W.}
}
@article {28566,
	title = {A preliminary investigation of the heavy mineral suites of the coastal rivers and beaches of Oregon and northern California},
	journal = {The Ore Bin},
	volume = {30},
	number = {9},
	year = {1968},
	month = {September_1968},
	pages = {p.165-180},
	keywords = {Alsea River, Chetco River, Coos River, Coquille River, geological, heavy minerals, hydrology, Kilchis River, Little Nestucca River, Miami River, Millicoma River, Necanicum River, Nehalem River, Nestucca River, North Fork, paleosciences, physical, Rogue River, Salmon River, sediment data, Siletz River, Siuslaw River, Sixes River, Tillamook River, Trask River, Umpqua River, Wilson River, Yaquina River, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/p26770670},
	author = {Kulm, Laverne D. and Scheidegger, K. F. and Byrne, John V. and Spigai, J. J.}
}
@mastersthesis {28511,
	title = {An Evaluation of Grain Size, Shape, and Roundness Parameters in Determining Depositional Environment in Pleistocene Sediments from Newport, Oregon},
	year = {1967},
	note = {Map in pocket in the back. Masters thesis},
	month = {December_1967},
	pages = {77 p.},
	school = {University of Oregon},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Eugene, Or.},
	keywords = {geological, paleosciences, sediment data, theses, Yaquina Bay, Yaquina River, Yaquina River Basin},
	author = {Stewart, Richard Lee}
}
@article {28291,
	title = {Preliminary data on compositional variations of Tertiary volcanic rocks in the central part of the Oregon Coast Range},
	journal = {The Ore Bin},
	volume = {27},
	number = {6},
	year = {1965},
	month = {June_1965},
	pages = {p.101-117},
	keywords = {geological, paleosciences, Yaquina Bay, Yaquina River, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/4t64gs70t},
	author = {Snavely, Parke D. Jr. and Wagner, Holly C. and Mcleod, Norman S.}
}
@article {28156,
	title = {Geologic interpretation of reconnaissance gravity and aeromagnetic surveys in northwestern Oregon},
	volume = {no.1181-N},
	year = {1964},
	note = { BOUND IN WITH: Geologic sketch of Northwestern Oregon  Map packet in the back},
	institution = {United States Government Printing Office},
	address = {Washington, D.C.},
	keywords = {geology, gravity, paleosciences, physical, Yaquina Bay},
	url = {https://pubs.usgs.gov/bul/1181m-n/report.pdf},
	author = {Bromery, R. W. and Snavely, Parke D. Jr. and U.S. Geological Survey,}
}
@article {28201,
	title = {Miocene stratigraphy of the Yaquina Bay area, Newport, Oregon},
	journal = {The Ore Bin},
	volume = {26},
	number = {8},
	year = {1964},
	month = {August_1964},
	pages = {p.133-151},
	keywords = {aquatic invertebrates, foraminifera, geological, paleosciences, sediment data, Yaquina Bay, Yaquina River, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/administrative_report_or_publications/0z7091860},
	author = {Snavely Jr., Parke D. and Rau, Weldon W. and Wagner, Holly C.}
}
@article {28146,
	title = {Tertiary geologic history of western Oregon and Washington},
	volume = {no.22},
	year = {1963},
	note = {Bw photographs, geologic maps.},
	month = {1963},
	pages = {25 p.},
	address = {Olympia, WA},
	keywords = {Eocene, geological, Miocene, Oligocene, paleosciences, Pliocene, sediment data},
	url = {https://www.dnr.wa.gov/publications/ger_ri22_tert_geol_west_or_wa.pdf},
	author = {Snavely Jr., Parke D. and Wagner, Holly C. and Washington Division of Mines and Geology,}
}
@article {27956,
	title = {Coastal sand dunes of Oregon and Washington},
	volume = {no.72},
	year = {1958},
	note = {Fold out maps},
	month = {June_1958},
	pages = {193 p.},
	institution = {Geological Society of America},
	address = {New York, NY},
	keywords = {Alsea River estuary, climate, coastal dunes, Columbia River estuary, Coos River estuary, general, general ecosystem description, geographical distribution, historical, human impacts, hydrology, Nehalem River estuary, Nestucca River estuary, Netarts estuary, paleosciences, physical, Sand Lake Estuary, Siletz River estuary, Siuslaw River estuary, Sixes River estuary, terrestrial vegetation, Tillamook estuary, Umpqua River estuary, wind, Yaquina Bay},
	url = {https://ir.library.oregonstate.edu/concern/defaults/hq37vs212},
	author = {Cooper, William S.}
}
@article {27846,
	title = {Fossil localitites of Lincoln County Beaches, Oregon},
	journal = {The Ore Bin},
	volume = {16},
	number = {4},
	year = {1954},
	note = {This is an early, brief account of marine fossils from northern Lincoln County.},
	month = {April_1954},
	pages = {p.21-28},
	keywords = {Agate Beach, Depoe Bay, Fogarty Creek, fossils, geological, Otter Rock, paleosciences, physical, Sally{\textquoteright}s Bend, Spencer Creek, Yaquina Bay},
	url = {https://pubs.oregon.gov/dogami/og/OBv16n04.pdf},
	author = {Steere, Margaret L.}
}
@mastersthesis {27791,
	title = {Stratigraphy of the Miocene Agate Beach Formation in Lincoln County, Oregon},
	year = {1953},
	note = {Major professor was Harold A Boyd Jr. Masters thesis.},
	month = {June_1953},
	pages = {73 p.},
	school = {Oregon State College},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {Agate Beach, aquatic invertebrates, Depoe Bay, foraminifera, fossils, geological, Jump-Off Joe, Nye Beach, Otter Rock, paleosciences, Schooner Creek, theses, Yaquina Head},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/pc289p42z},
	author = {Herron, John E.}
}
@mastersthesis {27761,
	title = {Stratigraphy and Foraminifera of the Upper Part of the Nye Formation, Yaquina Bay, Oregon},
	year = {1952},
	note = {Major professor was Harold A. Boyd Jr. Masters thesis.},
	month = {June_1952},
	pages = {47 p.},
	school = {Oregon State College},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {aquatic invertebrates, foraminifera, geological, paleosciences, theses, Yaquina Bay, Yaquina River Basin},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/pz50gz46z},
	author = {Heacock, Robert L.}
}
@article {27671,
	title = {Pleistocene history of the Newport, Oregon region},
	journal = {Geological News Letter},
	volume = {16},
	year = {1950},
	note = {This article gives a concise summary of Baldwin{\textquoteright}s work on the area in the 1940s. It includes a hand-drawn map. There is an interesting speculation about a shift in the mouth of the Yaquina River. "The former mouth of the Yaquina River probably lies somewhat south of its present mouth beneath the dune area where evidence is buried. At present, the dunes have been encroaching northward and driving the river against the resistant Astoria sandstone along the north bank," (p.79)},
	month = {October_1950},
	pages = {p.77-81},
	keywords = {geological, kitchen middens, paleosciences, Yaquina Bay, Yaquina River, Yaquina River Basin},
	url = {https://www.gsoc.org/s/1950-NEWSLETTERS.pdf},
	author = {Baldwin, Ewart M.}
}
@article {27596,
	title = {Five papers on foraminifera from the Tertiary of western Oregon: Part VI:  Upper Eocene foramanifera from the Toledo formation, Toledo, Lincoln County, Oregon},
	journal = {Bulletin (Oregon Department of Geology and Mineral Industries)},
	volume = {36},
	year = {1947},
	note = {Part VI published October_1949},
	month = {July_1947},
	keywords = {aquatic invertebrates, foraminifera, geological, paleosciences, Toledo, Yaquina River},
	url = {https://www.oregongeology.org/pubs/B/B-036_vol2.pdf},
	author = {Cushman, Joseph A. and Stewart, Roscoe E. and Stewart, Katherine C.}
}
@article {27561,
	title = {An investigation of the sea cliff landslide [of March 30, 1943] at Newport, [Lincoln County,]Oregon},
	year = {1943},
	month = {[1943]},
	institution = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {Agate Beach, coastal hazards, erosion, geology, landslides, paleosciences, sediments},
	author = {Allen, John Eliot and Lowry, Wallace D.}
}
@article {27556,
	title = {A  pollen study of a fossil peat  deposit on the Oregon coast},
	journal = {Northwest Science},
	volume = {16},
	number = {4},
	year = {1942},
	month = {1942},
	pages = {p.86-92},
	keywords = {coastal dunes, community ecology, ecological succession, geological, Nye Beach, paleosciences, terrestrial vegetation},
	author = {Hansen, Henry P. and Allison, Ira S.}
}
@proceedings {27426,
	title = {A new cetothere from the Miocene Astoria Formation of Newport, Oregon},
	volume = {no.447},
	year = {1934},
	note = {excellent photographs and drawings},
	publisher = {Carnegie Institution of Washington},
	keywords = {cetaceans, Desmatophoca oregonensis, geological, marine mammals, paleosciences, Yaquina Bay, Yaquina River, Yaquina River Basin},
	author = {Packard, Earl L. and Kellogg, Remington}
}
