@article {15386,
	title = {Coastal subsidence in Oregon, USA, during the giant Cascadia earthquake of A.D. 1700},
	journal = {Quaternary Science Reviews},
	volume = {30},
	year = {2011},
	note = {This article represents an attempt to estimate how much subsidence occurred after the great Cascadia earthquake of 1700.  Stratigraphy is given for 5 rivers in Oregon, with subsidence estimates for each.  The estimate for the Salmon River is 0.6 m plus or minus .29 m},
	pages = {p.364-376},
	keywords = {Alsea Bay, coastal hazards, Coos Bay, earthquakes, geology, Nehalem River estuary, Nestucca River estuary, paleosciences, Salmon River Estuary, Siuslaw River estuary, South Slough},
	doi = {10.1016/j.quascirev.2010.11.017},
	url = {https://nora.nerc.ac.uk/id/eprint/13572/1/Hawkes_QSR_2011.pdf},
	author = {Hawkes, A.D. and Horton, B.P. and Nelson, Alan R. and Vane, C.H. and Sawai, Y.}
}
