@article {51996,
	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},
	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.}
}
@mastersthesis {51921,
	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. },
	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, Yachats (Or.), Yachats Basalt, Yaquina Head},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/4j03d165r},
	author = {Oxford, Jeremiah}
}
@article {51766,
	title = {Petrology of late Eocene lavas erupted in the forearc of central Oregon},
	volume = {no.95-40},
	year = {1995},
	note = {This study contrasts two late-Eocene basalt flows in coastal Oregon, with particular emphasis on geochemistry. Extensive charts, maps. },
	pages = {58 p.},
	keywords = {Cape Perpetua, Cascade Head, Cascade Head Basalt, chemistry, geology, paleosciences, petrography, Siletz River Volcanics, volcanism, Yachats Basalt},
	url = {https://pubs.usgs.gov/of/1995/0040/report.pdf},
	author = {Davis, A. S. and Snavely, Parke D. and Gray, Leda-Beth and Minasian, D. L. and Geological Survey (U.S.),}
}
@inbook {51786,
	title = {Tertiary facies and paleoenvironments along the Coast Range and Western Cascade margin, western Oregon Fritsche, A. Eugene},
	booktitle = {Cenozoic Paleogeography of the Western United States.  II:  Pacific Section},
	series = {Book / Pacific Section, SEPM (Society for Sedimentary Geology)},
	volume = {75},
	year = {1995},
	note = {The Yachats Basalt is not a uniform mass of volcanic material. Rather, it is inter-bedded with sedimentary deposits, many of which are fossiliferous. The environment in which these volcanic and sedimentary deposits were laid down is discussed. Uses Devil{\textquoteright}s Elbow as an example site. Includes a schematic diagram of an idealized representative vertical sequence. The Eugene Formation of the Willamette Valley and the Western Cascades is also discussed. BW photographs.},
	pages = {p.257-273},
	publisher = {Society for Sedimentary Geology.  Pacific Section,},
	organization = {Society for Sedimentary Geology.  Pacific Section,},
	address = {Fullerton, Cal.},
	keywords = {Devil{\textquoteright}s Elbow State Park, geology, paleontology, paleosciences, sediments, volcanism, Yachats Basalt},
	author = {Shroba, Cynthia S. and Orr, William N. and SEPM (Society for Sedimentary Geology). Pacific Section,},
	editor = {Fritsche, A. Eugene}
}
@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.}
}
@article {51621,
	title = {Yachats Basalt; an upper Eocene differentiated volcanic sequence in the Oregon Coast Range},
	journal = {Journal of Research of the U. S. Geological Survey},
	volume = {2},
	year = {1974},
	note = {This article names and describes the Yachats Basalt formation.  Includes a geologic map and photograph. The authors addressed the geologic setting, distribution, physical qualities, petrography, chemistry, geologic history, tectonic setting, and speculated about its origin. },
	month = {1974, Jul-Aug},
	pages = {p.395-403},
	keywords = {Alsea Bay, basalt, Big Creek, bob Creek, Cape Perpetua, Eckman Creek, geochemistry, geology, Heceta Head, Klickitat Mountain, paleosciences, Tenmile Creek, volcanism, Yachats (Or.), Yachats Basalt, Yachats River},
	author = {Snavely Jr., Parke D. and Macleod, Norman S.}
}
