@article {83047,
	title = {Characteristic scales of drainage reorganization in Cascadia},
	journal = {Geophysical Research Letters},
	volume = {48},
	number = {3},
	year = {2021},
	note = {The organization of river basins varies over geologic time.  Tectonic forces, uplift and erosion can cause a stream to be {\textquotedblleft}captured{\textquotedblright} by a neighboring river basin.  Stream captures are relatively common in the Oregon Coast Range.  In this most interesting article, the authors describe a process of modeling stream networks at different geographic scales. {\textquotedblleft}Integration of these {\textquoteleft}synthetic{\textquoteright} drainage networks into a margin-parallel river system, similar to the modern Willamette Valley, supports field observations of stream capture and river network reorganization. We propose that these methods are useful for predicting future drainage configurations and isolating the relevant tectonic processes responsible for changing river networks{\textquotedblright} (from the Abstract). This is an open-access article.},
	month = {2021, Feb.16 },
	pages = {e2020GL091413},
	keywords = {Columbia River, Cow Creek, geography, geology, Klamath River, mathematical modeling, paleosciences, Rogue River, Siletz River, South Umpqua River, topography, Umpqua River Basin, Yaquina River},
	doi = {https://doi.org/10.1029/2020GL091413},
	url = {https://www.sciencedirect.com/science/article/pii/S1470160X20311067?via\%3Dihub },
	author = {Struble, William T. and Roering, Joshua J. and Dorsey, Rebecca J. and Bendick, Rebecca}
}
@mastersthesis {83071,
	title = {Evolution of Cascadia Landscapes: Drainage Reorganization Inferred from Topographic Transformations and Dendrochronological Dating of Landslide-Dammed Lakes},
	year = {2021},
	note = {This doctoral dissertation begins by examining the question of dating past landslides in the Oregon Coast Range.  Although it is assumed that the famous earthquake of 1700 C.E. caused many landslides, no landslide has been definitely dated to that event.  The author examines two coastal lakes formed by landslides, Wasson and Klickitat Lakes, and using Carbon14 dating and evidence from tree rings, dates them to the winters of 1819/1820 and 1751/1752, respectively.  He also dates other landslides to major precipitation events. The dissertation ends with a look at stream networks and the phenomenon of streams being captured by neighboring basins.},
	pages = {142 p.},
	school = {University of Oregon},
	type = {Doctoral dissertation},
	edition = {Ph. D.},
	chapter = {Dept. of Earth Sciences},
	address = {Eugene, Or.},
	keywords = {coastal hazards, dendrochronology, earthquakes, erosion, geography, geology, Klickitat Lake, landslides, mathematical modeling, North Fork Alsea River, paleosciences, precipitation, Smith River, topography, Umpqua River Basin, Wasson Lake},
	url = {https://scholarsbank.uoregon.edu/xmlui/handle/1794/26189 },
	author = {Struble, William Truin}
}
@article {83103,
	title = {Geologic controls on paleodrainage incision and morphology during sea level lowstands on the Cascadia shelf in Oregon, USA},
	journal = {Marine Geology},
	volume = {434},
	number = {106444},
	year = {2021},
	note = {In late Quaternary glaciation, sea levels were much lower than in the present.  Coastal rivers wound their ways across the gently sloping coastal plain to the Pacific Ocean.  The sediments off the Oregon Coast record traces of these paleorivers as they flowed to the sea.  In this paper, the authors examine the submerged drainage systems of two Oregon paleorivers about 40 kilometers apart, the early Siuslaw and Umpqua rivers.  The two streams made quite different impacts on the land, from the gently winding Siuslaw, with multiple cross-connections between channels to the more deeply incised bed of the early Umpqua River. This is a most interesting look at the pasts of two neighboring streams.},
	pages = {16 p.},
	keywords = {continental shelf, geology, paleosciences, remote sensing, sediments, Siuslaw River, sonar, Umpqua River},
	doi = {https://doi.org/10.1016/jmargeo.2021.106444 },
	author = {Klotsko, Shannon and Skakun, Matthew and Maloney, Jillian and Gusick, Amy and Davis, Loren and Nyers, Alexander and Ball, David}
}
@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.}
}
@article {83018,
	title = {Deep-seated landslides drive variability in valley width and increase connectivity of salmon habitat in the Oregon Coast Range},
	journal = {JAWRA Journal of the American Water Resources Association},
	volume = {54},
	number = {6 },
	year = {2018},
	note = {A significant percentage of land in the Oregon Coast Range is subject to deep-seated landslides. Many landslides have ancient origins, and have been postulated to date as far back as the Pleistocene.  The authors of this paper define deep-seated landslides as cases in which a majority of slopes fail in a given watershed.  {\textquotedblleft}We explore how the presence of extensive deep-seated landsliding affects valley floor width and the quantity and connectivity of seasonal habitat for Coho Salmon by comparing these metrics in five subbasins in the Umpqua River Basin with extensive DSLs to five subbasins in the Umpqua River Basin without deep-seated landsides.  We hypothesize that DSLs promote variable valley width and hence a higher frequency of anomalously wide valleys and that this results in greater connectivity between seasonal habitat types.{\textquotedblright} (p.1326)  This is an open-access article.},
	pages = {p.1325-1340 },
	keywords = {Charlotte Creek, Coho salmon = Oncorhynchus kisutch, Dean Creek, geographic distribution, geology, habitats, Halfway Creek, Herb Creek, landslides, paleosciences, Rock Creek, Sand Creek, Scare Creek, Scholfield Creek, sediments, Sweden Creek, Tyee Formation, Umpqua River, Yellow Creek},
	doi = {https://doi.org/10.1111/1752-1688.12693 },
	url = {https://www.fs.usda.gov/research/treesearch/57786},
	author = {Beeson, Helen W. and Flitcroft, Rebecca L. and Fonstad, Mark A. and Roering, Joshua J.}
}
@article {83021,
	title = {Structural controls on paleodrainage during the last glacial maximum on the Oregon continental shelf [abstract]},
	journal = {American Geophysical Society.  Meeting.  Fall Meeting.},
	volume = {no. OS11F-1461},
	year = {2018},
	note = {This abstract describes a sonar imaging project studying the Siuslaw and Umpqua paleo-rivers at the peak of the last Ice Age, when the sea level was about 120 meters below the present level.  At that time, rivers flowed along what is now the continental shelf.  {\textquotedblleft}The mapped paleochannels are good indicators of potential archaeological sites, as many sites have been documented along the Umpqua and Siuslaw Rivers onshore. . . Detailed mapping of these structures could aid future archaeological investigations and paleochannel modeling in the region.{\textquotedblright}},
	pages = {1 p.},
	keywords = {archeology, bathymetry, geology, paleosciences, Siuslaw River, sonar, Umpqua River},
	url = {https://ui.adsabs.harvard.edu/abs/2018AGUFMOS11F1461K/abstract},
	author = {Klotsko, S. and Maloney, J. M. and Watkins, K. and Gusick, A. E. and Davis, L. G. and Nyers, A. and Braje, T. and Ball, D.}
}
@mastersthesis {77166,
	title = {Lithologic, Climatic, and Biotic Vs. Abiotic Controls on Erosion and Landscape Evolution},
	year = {2015},
	note = {{\textquotedblleft}The triumvirate of tectonics, lithology, and climate control landscape evolution. This study quantifies how lithologic variation and climate-mediated changes in ecosystems perturb steady state processes in the unglaciated, soil-mantled Oregon Coast Range. . .{\textquotedblright} (from the Abstract)  The several chapters of this Ph. D. dissertation offer fascinating looks at several catchments in the Umpqua River Basin, including a reconstruction of paleoclimate over 50,000 years in the Little Lake watershed.},
	pages = {133 p.},
	school = {University of Oregon},
	type = {Doctoral Dissertation},
	edition = {Ph. D.},
	chapter = {Dept. of Geosciences},
	address = {Eugene, Or.},
	keywords = {climate data, erosion, Franklin Creek, geochemistry, geology, Harvey Creek, Little Lake, Lower Umpqua River, paleosciences, sediment data, South Umpqua River, terrestrial vegetation, topography, Triangle Lake},
	url = {https://scholarsbank.uoregon.edu/xmlui/handle/1794/19291 },
	author = {Marshall, Jill Ann}
}
@article {54866,
	title = {Debris flows: behaviour and hazard assessment},
	journal = {Geology Today},
	volume = {30},
	year = {2014},
	note = {This is a layperson-friendly explanation of landslides and debris flows {\textendash} what they are, why they happen, and the tools scientists use to model them and predict when they will occur. The article includes an illustration of a potential hazard site on the Umpqua River near Scottsburg.},
	month = {2014, Jan.-Feb.},
	pages = {p.15-20},
	keywords = {coastal hazards. Precipitation, erosion, geology, landslides, paleosciences, Scottsburg (Or.), sediments, Umpqua River},
	doi = {10.1111/gto.12037},
	author = {Iverson, Richard M.}
}
@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.}
}
@mastersthesis {26646,
	title = {The Oregon Coastal Subprovince, a New Biogeographic Subprovince for Primary Freshwater Fishes in Oregon},
	year = {2008},
	note = {"The goals of this study were: 1) to describe fishes in the genera Catostomus and Ptychocheilus in the Oregon Coastal Subprovince using morphological data and mitochondrial cytochrome b sequences; 2) to investigate the relationships of fishes in the Oregon Coastal Subprovince to nearby provinces; and 3) to address competing distribution theories." (from the Abstract)  The author proposes that, based on the endemic distribution of freshwater fishes, the Oregon coast may deserve designation as a biogeographic subprovince, ranging from the Miami River in the north to the Sixes River in the south. Possible explanations for the distribution of these fishes are considered. The major professor was Douglas Markle.},
	pages = {194 p.},
	school = {Oregon State University},
	type = {Doctoral Dissertation},
	edition = {Ph. D.},
	chapter = {Dept. of Fisheries and Wildlife, Fisheries Science},
	address = {Corvallis, Or.},
	keywords = {Colorado pikeminnow = Ptychocheilus lucius, Coos River, Coquille River, genetics, geology, Klamath smallscale sucker = Catostomus rimiculus, Largescale sucker = Catostomus macrocheilus, Nehalem River, Oregon pikeminnow = Ptychocheilus oregonensis, paleosciences, Ptychocheilus grandis = Sacramento pikeminnow, Siuslaw River, Sixes River, spatial distribution, taxonomy, theses, Tyee sucker = Catostomus tsiltcoosensis, Umpqua River, Umpqua River Basin, Umpqua squawfish = Ptychocheilus umpquae},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/76537380b},
	author = {Kettratad, Jes}
}
@mastersthesis {26286,
	title = {The Ecological Legacy of Indian Burning Practices in Southwestern Oregon},
	year = {2005},
	note = {This interesting and wide-ranging dissertation contrasts Native American landscape management practices such as frequent, low-intensity fires with contemporary, densely-spaced  monoculture forest plantations. The 2002 Apple and Tiller Complex fires are also considered. Color illustrations.},
	pages = {181 p.},
	school = {Oregon State University},
	type = {Doctoral Dissertation},
	edition = {Ph. D.},
	chapter = {Dept. of Forest Science},
	address = {Corvallis, Or.},
	keywords = {archeology, Black Creek, Cavitt Creek, Clover Creek, erosion, forest fires, human impacts, Little River, logging, Native Americans, North Umpqua River, paleosciences, sediments, terrestrial vegetation},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/js956k02v},
	author = {Carloni, Kenneth R.}
}
@article {26111,
	title = {Cascadia tsunami deposit database [electronic resource]},
	volume = {no.03-13},
	year = {2003},
	note = {"The Cascadia Tsunami Deposit Database contains data on the location and sedimentological properties of tsunami deposits found along the Cascadia margin." (from the Abstract)},
	pages = {24 p.},
	institution = {U.S. Geological Survey},
	address = {[Menlo Park, Calif.]},
	keywords = {bibliography, coastal hazards, earthquakes, geology, landslides, paleosciences, sediment data, tsunamis},
	url = {https://pubs.usgs.gov/publication/ofr0313},
	author = {Peters, Robert and Jaffe, Bruce and Gelfenbaum, Guy and Peterson, Curt}
}
@mastersthesis {25301,
	title = {Coastal Crossing of the Elastic Strain Zero-Isobase, Cascadia Margin, South Central Oregon Coast },
	volume = {no.4739},
	year = {1994},
	note = {This thesis is an attempt to define the landward extent of the areas of "abrupt coastal subsidence and uplift" on the southern Oregon coast (p.172). Marsh cores were studied in Siuslaw Bay, the lower Umpqua River area, and Coos Bay.  Diatom assemblages indicated whether sediments were marine or brackish. Includes original photograph of marsh core sample. Maps.},
	pages = {251 p.},
	school = {Portland State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Portland, Or.},
	keywords = {Butler Creek, Coos Bay estuary, Dean Creek, diatoms, earthquakes, Gardiner paper Mill, geology, Harvey Creek, Oar Creek, Otter Slough, paleosciences, Providence Creek, Scholfield Creek, sediment data, Siuslaw estuary, Smith River, Steamboat Island, theses, tsunamis, Umpqua Estuary, Winchester Bay},
	doi = {https://doi.org/10.15760/etd.6623},
	url = {https://archives.pdx.edu/ds/psu/27772},
	author = {Briggs, Gregory George}
}
@mastersthesis {25281,
	title = {Prehistoric Settlement Patterns in Southwest Oregon},
	year = {1993},
	note = {This dissertation describes analysis of 83 sites in the Rogue and Umpqua river basins, 40 of which are in the Umpqua River Basin.  The study describes two different approaches by Native peoples to their environment:  mobile hunter-gatherering and a more sedentary collector approach. The author explores the timeline and possible reasons for this difference. Extensive site descriptions and artifact analysis.},
	pages = {274 p.},
	school = {University of Oregon},
	type = {Doctoral Dissertation},
	edition = {Ph. D.},
	chapter = {Dept. of Anthropology},
	address = {Eugene, Or.},
	keywords = {Apple Creek, archeology, Cavitt Creek, Coffee Creek, Copeland Creek, Dry Creek, Glide, Medicine Creek, Narrows, North Umpqua River, paleosciences, Section Creek, South Umpqua River, Steamboat Creek, Susan Creek, Swiftwater, theses, Winchester},
	url = {https://scholarsbank.uoregon.edu/xmlui/handle/1794/10309},
	author = {Winthrop, Kathryn R.}
}
@inbook {25116,
	title = {Archaeology of Umpqua/Eden (35DO83)},
	booktitle = {Prehistory of the Oregon Coast:  the Effects of Excavation Strategies and Assemblage Size on Archaeological Inquiry},
	year = {1991},
	note = {Chapter 5.  Extensive analysis of mammalian remains. Charts, line drawings, bw photographs. A thorough discussion of this excavation.},
	pages = {p.102-174},
	publisher = {Academic Press, Inc.},
	organization = {Academic Press, Inc.},
	address = {San Diego},
	keywords = {aquatic mammals, archeology, Lower Umpqua River, paleosciences, terrestrial mammals, Winchester Bay},
	author = {Lyman, R. Lee}
}
@inbook {25041,
	title = {Athapaskans of Southwestern Oregon},
	booktitle = {Northwest Coast},
	series = {Handbook of North American Indians},
	volume = {7},
	year = {1990},
	note = {General overview of what was known about the Tillamook people in the late 1980s. Brief treatment of Native American history and culture.  Includes the Upper Umpqua, Upper Coquille, Kwatami (Sixes River), Yukichetunne (Euchre Creek), Chemetunne Tutuni, Mikonotunne, Chasta Costa, Galice, Applegate (Rogue), Chetleshin (Pistol River), Khwaishtunnetunne, and Chetco peoples.},
	pages = {p.580-588},
	publisher = {Smithsonian Institution},
	organization = {Smithsonian Institution},
	address = {Washington, D.C.},
	keywords = {anthropology, Chetco River, geographic distribution, history, Middle Fork Coquille River, North Fork Coquille River, North Umpqua River, paleosciences, Rogue River, Sixes River, South Fork Coquille River, South Umpqua River},
	author = {Miller, Jay and Seaburg, William R.},
	editor = {Suttles, Wayne}
}
@proceedings {25071,
	title = {Climatic change, spring Chinook, and human seasonal movements in the upper basin of the South Umpqua River:  the Times Square Rockshelter model},
	volume = {43rd},
	year = {1990},
	note = {Print of paper given at conference. It is not known if this paper was ever published. Relates history of human use of the Times Square Rockshelter over almost 4,000 years to what is known about the climate. Unfortunately, not enough was known about the climate in the region of the rockshelter to definitely link patterns of use to fluctuations between xeric and mesic climate regimes, but the author believes that the data from the rockshelter can help to "serve as a basis for model building." (p.3). Maps, charts, tables.},
	pages = {15 p.},
	address = {Eugene, Or.},
	keywords = {archeology, Chinook salmon = Oncorhynchus tshawytscha, climate, general ecosystem description, human impacts, paleosciences, South Umpqua River},
	author = {Spencer, Lee}
}
@inbook {25076,
	title = {Siuslawans and Coosans},
	booktitle = {Northwest Coast},
	series = {Handbook of North American Indians},
	volume = {7},
	year = {1990},
	note = {General overview of what was known about the Siuslawan and Coosan peoples in the late 1980s. Brief treatment of Native American history and culture. Note that these were the coastal peoples - for example, the Upper Umpqua and Upper Coquille peoples were Athapaskans, with a different cultural heritage."The most important resource of the area was salmon, which were taken from canoes in deep water, dipnetted, harpooned, clubbed, and trapped at upriver weirs or in rapids and shallow water. Additionally, the estuaries and rivers supported major runs of herring, smelt, lampreys, and less seasonally limited supplies of various saltwater and freshwater fish." (p.573) This group includes the Siuslaw, Lower Umpqua, Hanis (Coosan), South Slough Miluk and Lower Coquille Miluk. },
	pages = {p.572-579},
	publisher = {Smithsonian Institution},
	organization = {Smithsonian Institution},
	address = {Washington, D.C.},
	keywords = {anthropology, Coos Bay, Coos River, geographic distribution, history, Lower Coquille River, Lower Umpqua River, Millicoma River, paleosciences, Siltcoos Creek, Siuslaw Bay, Siuslaw River, South Slough, Tahkenitch Creek, Tenmile Creek, Umpqua Estuary},
	author = {Zenk, Henry B.},
	editor = {Suttles, Wayne}
}
@inbook {25036,
	title = {Takelma},
	booktitle = {Northwest Coast},
	series = {Handbook of North American Indians},
	volume = {7},
	year = {1990},
	note = {General overview of what was known about the Takelma people in the late 1980s. Brief treatment of history and culture. "In the Umpqua drainage Takelma territory included at least upper Cow Creek, ... possibly the whole of Cow Creek, Myrtle Creek, and a portion of the main stem of the South Umpqua..."},
	pages = {p.589-592},
	publisher = {Smithsonian Institution},
	organization = {Smithsonian Institution},
	address = {Washington, D.C.},
	keywords = {anthropology, Cow Creek, geographic distribution, history, Myrtle Creek, paleosciences, Rogue River Basin, South Umpqua River, Umpqua River Basin},
	author = {Kendall, Daythal L.},
	editor = {Suttles, Wayne}
}
@mastersthesis {38636,
	title = {Geochemical Evolution of the Roseburg Formation Basaltic Rocks, Southern Oregon Coast Range},
	year = {1988},
	note = {Discusses the Roseburg Formation basalts, their relationship to other basalt flows in Oregon, their chemical composition and likely geologic origin (oceanic ridge / hotspot). Charts, tables, geologic maps. {\textquotedblleft}The basalt flows in the Roseburg region are mostly thick and massive with pillowed margins. Lateral gradation into pillows and pillow breccias is common. Pillows are usually 0.5 to 1.0 m in diameter and, in some areas along the North Umpqua River, they make up entire flows up to 10 m thick.{\textquotedblright} (p.28) The major professor was E. Julius Dasch.},
	pages = {142 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {chemistry, Drain Or., geology, Horseshoe Bend, Jack Creek, North Umpqua River, paleosciences, Roseburg Or., theses},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/st74cs86z},
	author = {Pyle, Douglas G.}
}
@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 {24471,
	title = {Geology and Mineralization of the Banfield and Rowley Volcanogenic Massive Sulfide Deposits, Douglas Co., Oregon},
	year = {1981},
	note = {"The overall purpose of the study was to optimize exploration of the Banfield-Rowley area by establishing the principal geologic features and controls of mineralization. Specific considerations included: 1) the structural, stratigraphic and geometric relationships of the mineral deposits to their host rocks, 2) the distribution, texture and mineralogy of sulfIde and alteration assemblages, 3) the post-mineralization metamorphic and structural effects, and 4) the origin of mineralization." (p.2) The major professor was Cyrus W. Field.},
	month = {1982},
	pages = {131 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {Drew Creek, geology, mining, paleosciences, South Umpqua River, sulphides, theses, Umpqua River Basin},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/rj430709m},
	author = {Fifarek, Richard H.}
}
@article {24441,
	title = {Evaluation of water resources in the Reedsport area, Oregon},
	volume = {no.80-444},
	year = {1980},
	note = {Examines possible water sources for Reedsport:  Clear Lake and an aquifer.  Estimates there is enough water in the dune aquifer to supply Reedsport "in the year 2000." Considers Clear Lake "a moderately nutrient-enriched lake.  Clear Lake, however, has the potential to rapidly become eutrophic if phosphorus loadings were increased above present levels." (p.30) },
	month = {1980.},
	pages = {37 p.},
	institution = {U.S. Geological Survey},
	address = {[Reston, Va.?]},
	keywords = {algae, bacteria, carbon, Clear Lake, climate, dissolved oxygen, geology, hydrology, Lower Umpqua River, nitrogen, paleosciences, pH data, phosphorus, precipitation, Reedsport, sediments, water temperature},
	url = {https://pubs.usgs.gov/of/1980/0444/report.pdf},
	author = {Rinella, Joseph F. and Frank, F. J. and Leonard, A. R.}
}
@article {36416,
	title = {Prospects for oil and gas in the Coos Basin, Western Coos, Douglas, and Lane Counties, Oregon},
	volume = {no.6},
	year = {1980},
	note = {Discusses the general geology and potential for finding oil or gas deposits in the Coos Basin.  Discusses geology around Florence, Oregon, and the geology of southwestern Oregon. Includes geological maps of the area.},
	pages = {74 p.},
	institution = {Oregon Dept. of Geology and Mineral Industries,},
	address = {Portland, Or.},
	keywords = {geology, Lower Siuslaw River, Lower Umpqua River, natural gas, paleosciences, petroleum, Siltcoos Lake, Tenmile Lake, Winchester Bay},
	url = {https://www.oregongeology.org/pubs/ogi/OGI-06.pdf},
	author = {Newton, Vernon C.}
}
@book {24046,
	title = {Environmental geology of Western Coos and Douglas Counties, Oregon},
	series = {Bulletin (Oregon Dept. of Geology and Mineral Industries)},
	number = {no.87},
	year = {1975},
	note = {Colored maps in pocket.},
	month = {1975},
	publisher = {Oregon Dept. of Geology and Mineral Industries},
	organization = {Oregon Dept. of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, erosion, geology, minerals, paleosciences, sediments, soils},
	url = {https://www.oregongeology.org/pubs/B/B-087.pdf},
	author = {Beaulieu, John D.}
}
@mastersthesis {50556,
	title = {Chemical Composition Studies of Oregon and Washington Coastal Basalts},
	year = {1974},
	note = {Discusses the chemical similarity of coastal basalts to inland formations and speculates on their origins. {\textquotedblleft}The three groups of Miocene basalts from the coast have been shown to be nearly identical chemically to three chemical types defined in the Columbia River Plateau basalts as follows: Depoe Bay Basalt = Lower Yakima Basalt (high and low Mg types), Cape Foulweather Basalt = Frenchman Springs Basalt, and the Basalt of Pack Sack Lookout = Pomona Basalt. Possible models for the origin of these basalts erupted from vents over 500 km apart are also discussed. The Eocene basalts from the Oregon coast are found to be most similar to the basalts from the Hawaiian Islands, whereas the Metchosin Formation basalts on southern Vancouver Island are found to be more similar to ocean ridge tholeiites.{\textquotedblright}  (from the Abstract) The major professor was Roman A. Schmitt.},
	pages = {99 p.},
	school = {Oregon State University},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Chemistry},
	address = {Corvallis, Or.},
	keywords = {Cape Foulweather Basalt, chemistry, Depoe Bay Basalt, geology, Pack Sack Lookout Basalt, paleosciences, Siletz River Volcanics, theses, Tillamook Volcanics, Umpqua Volcanics},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/b8515r77k},
	author = {Hill, Dale Wayne}
}
@book {23891,
	title = {Geology \& mineral resources of Douglas County, Oregon},
	series = {Bulletin (Oregon. Dept. of Geology and Mineral Industries) },
	number = {75},
	year = {1972},
	note = {Includes colored map.},
	month = {1972},
	publisher = {Oregon Dept. of Geology and Mineral Industries},
	organization = {Oregon Dept. of Geology and Mineral Industries},
	chapter = {106 pp.},
	address = {Portland, Or.},
	keywords = {coastal hazards, Douglas County, erosion, geology, heavy minerals, landslides, mining, Or., paleosciences, sediments},
	url = {https://www.oregongeology.org/pubs/B/B-075.pdf},
	author = {Ramp, Len}
}
@article {23706,
	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 = {1968},
	pages = {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},
	isbn = {0148-1827},
	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.}
}
@article {23541,
	title = {Tertiary geologic history of western Oregon and Washington},
	volume = {no.22},
	year = {1963},
	note = {Maps, bw photographs.},
	month = {1963},
	pages = {25 p.},
	address = {Olympia, WA},
	keywords = {geological, paleosciences, sediment data},
	url = {https://file.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,}
}
@book {23381,
	title = {Coastal sand dunes of Oregon and Washington},
	series = {Memoir (Geological Society of America)},
	volume = {no.72},
	year = {1958},
	note = {Fold out maps.},
	month = {1958, Jun.},
	publisher = {Geological Society of America},
	organization = {Geological Society of America},
	address = {New York, NY},
	keywords = {Alsea River estuary, climate, coastal dunes, Columbia River estuary, Coos Bay, general, general ecosystem description, geographical distribution, history, human impacts, hydrology, Nehalem River estuary, Nestucca River estuary, Netarts Bay, paleosciences, physical, Sand Lake Estuary, Siletz River estuary, Siuslaw River estuary, Sixes River estuary, terrestrial vegetation, Tillamook Bay, Umpqua River estuary, wind, Yaquina Bay},
	author = {Cooper, William S.}
}
@mastersthesis {83005,
	title = {Geology of the Northeast Quarter of Camas Valley Quadrangle, Douglas County, Oregon},
	year = {1957},
	note = {This M.S. thesis describes part of a quadrangle in Douglas County.  The northwestern portion of the area falls into the Coos River drainage, while the eastern part drains into the South Umpqua River.  Lithography, structural and historical geology are given.  The author{\textquoteright}s geologic map is included.  The major professor was Harold A. Boyd.},
	pages = {95 p.},
	school = {Oregon State College},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {Champagne Creek, Coos River, geology, Henry Creek, Lookingglass Creek, paleosciences, Reston (Or.), South Umpqua River, stratigraphy, theses},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/x920g1524 },
	author = {Moore, James Francis, Jr.}
}
@mastersthesis {83004,
	title = {Geology of the Southeast One-Quarter of the Camas Valley Quadrangle Douglas County, Oregon},
	year = {1957},
	note = {This M.S. thesis describes a 54-square mile area in the Olalla Creek drainage in Douglas County.  Lithography, structural and historical geology are given.  Interestingly, the author notes that the drainage shows signs of stream piracy.  The major professor was Harold A. Boyd.},
	pages = {70 p.},
	school = {Oregon State College},
	type = {Masters Thesis},
	edition = {M.S.},
	chapter = {Dept. of Geology},
	address = {Corvallis, Or.},
	keywords = {fossils, geology, Olalla (Or.), Olalla Creek, paleosciences, Porter Creek (Or.), Shields Creek, South Umpqua River, species list, stratigraphy, Tenmile (Or.), Tenmile Creek, theses},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/cc08hk94m },
	author = {Harms, James Edward}
}
