@article {37711,
	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://www.oregongeology.org/pubs/ofr/O-97-11.pdf},
	author = {Priest, George R.}
}
@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}
}
@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}
}
@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}
}
