@mastersthesis {82466,
	title = {Processes of Sea-Cliff Erosion on the Oregon Coast : from Neotectonics to Wave Run-Up},
	year = {1992},
	note = {The rate of sea-cliff erosion in Oregon is determined by the interplay between tectonic uplift and sea level rise.  The Lincoln City area on the central Oregon coast is undergoing relatively little uplift, and therefore experiences a higher rate of erosion than areas to the north and south. This doctoral dissertation examines the rate of erosion and examines the transport and distribution of eroded sand. Although most of the work is concerned with ocean erosion, the author does examine the Siletz Spit and the dunes at the entrance of the Salmon River.},
	pages = {135 p.},
	school = {Oregon State University},
	type = {Doctoral dissertation},
	edition = {Ph. D.},
	chapter = {College of Oceanography},
	address = {Corvallis, Or.},
	keywords = {Cascade Head, Salmon River, Lincoln City (Or.), Siletz Spit, Siletz Bay, Siletz River, Fogarty Creek, Government Point, beach processes, coastal hazards, erosion, geography, geology, human impacts, sea levels, sediment data, wave height, theses},
	url = {https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/r781wh97w },
	author = {Shih, Shyuer-Ming}
}
