@article {11871,
	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.}
}
@article {11886,
	title = {The application of intertidal foraminifera to reconstruct coastal subsidence during the giant Cascadia earthquake of AD 1700 in Oregon, USA},
	journal = {Quaternary International},
	volume = {221},
	number = {1-2},
	year = {2010},
	note = {"Changes in species assemblages of intertidal foraminifera can be used to estimate the amount of earthquake-related subsidence during plate-boundary earthquakes at the Cascadia subduction zone." (from the Abstract)},
	pages = {116-140},
	keywords = {Alsea Bay, coastal hazards, Coos Bay, Coquille River, earthquakes, Nehalem River, Salmon River, Siuslaw River, tsunamis},
	doi = {10.1016/j.quaint.2009.09.019},
	author = {Hawkes, A.D. and Horton, B.P. and Nelson, A.R. and Hill, D.F.}
}
