@article {82987,
	title = {Comparison of Oregon tsunami hazard scenarios to a probabilistic tsunami hazard analysis (PTHA)},
	volume = {no.O-19-04},
	year = {2019},
	note = {In this paper, two different scenarios for tsunamis generated after earthquakes are contrasted. Five different sizes of earthquakes are compared.  {\textquotedblleft}The immediate objective of this project is to determine how closely tsunami forces at typical coastal bridges compare between the DOGAMI  and AECOM  (Thio, 2019) tsunami simulations.  The long-term objective is to determine the best and most cost-effective approach for estimating the current forces of a 1,000-yr exceedance tsunami for bridge design.{\textquotedblright} Estimated tsunamis and their effects on coastal bridges are explored, in order to help future bridges be designed to withstand these forces.},
	pages = {94 p.},
	institution = {Oregon Department of Geology and Mineral Industries  },
	address = {Portland, Or.},
	keywords = {Astoria (Or.), Seaside (Or.), Cannon Beach (Or.), Bandon (Or.), Gold Beach (Or.), Coastal hazards, earthquakes, tsunamis, mathematical modeling, bridges, Columbia River, Necanicum River, Ecola Creek, Coquille River estuary, Rogue River, Lincoln City (Or.), Newport (Or.), Waldport (Or.), Yachats (Or.), Siletz Bay, Yaquina Bay, Alsea Bay, Yachats River estuary},
	url = {https://www.oregongeology.org/pubs/ofr/O-19-04_report.pdf },
	author = {Priest, George R. and Allan, Jonathan C.}
}
@article {54886,
	title = {Tsunami impact to Washington and northern Oregon from segment ruptures on the southern Cascadia subduction zone},
	journal = {Natural Hazards},
	volume = {72},
	year = {2014},
	note = {All who live on the West Coast of the United States should be aware of the possibility of a major  earthquake occurring.  But what if only a part of the subduction zone ruptures?  This article examines a possible rupture in the southern half of the Cascadia Subduction Zone (south of Alsea Bay, Oregon).  The authors ask important questions. How quickly does tsunami wave height decline north of the southern rupture areas?  How much time do communities north of the southern rupture areas have to evacuate before the first inundation and the largest inundation occur? How far north of the southern rupture areas will felt shaking likely trigger evacuation of a populace trained to evacuate for a local earthquake? (p.851) The authors address these questions using a 10,000-year record of offshore turbedite deposits and  a ~4,600-year record of tsunami deposits at Bradley Lake.},
	month = {2014, Jun.},
	pages = {p.849-870},
	keywords = {Bandon (Or.), Brookings (Or.), Cannon Beach (Or.), Cape Blanco, coastal hazards, Columbia River, Coos Bay, Crescent City (Cal.), Depoe Bay (Or.), earthquakes, Florence (Or.), geology, Gold Beach (Or.), Grays Harbor (Wa.), Lincoln City (Or.), Long Beach (Wa.), Manzanita (Or.), Netarts Bay, Newport (Or.), Pacific City (Or.), paleosciences, Port Orford (Or.), Rockaway (Or.), Seaside (Or.), Tillamook Bay, tsunamis, Waldport (Or.), Winchester Bay},
	doi = {10.1007/s11069-014-1041-7},
	author = {Priest, George R. and Zhang, Yinglong and Witter, Robert C. and Wang, Kelin and Goldfinger, Chris and Stimely, Laura L.}
}
@article {54631,
	title = {Tsunami inundation scenarios for Oregon},
	volume = {no. O-13-19},
	year = {2013},
	note = {This technical document accompanies the 2013 tsunami inundation map series for coastal Oregon.  It describes the methodology used to produce the maps.  In addition to the report, the CD includes GIS shapefiles with embedded metadata.},
	pages = {17 p.},
	institution = {Oregon Department of Geology and Mineral Industries},
	address = {Portland, Or.},
	keywords = {coastal hazards, earthquakes, general, maps, mathematical modeling, Oregon, tsunamis},
	url = {https://www.oregongeology.org/pubs/ofr/O-13-19.pdf},
	author = {Priest, George R. and Witter, Robert C. and Zhang, Y. Joseph and Wang, Kelin and Goldfinger, Chris and Stimely, Laura L. and English, John T. and Pickner, Sean G. and Hughes, Kaleena L. B. and Wille, Taylore E. and Smith, Rachel L. and Oregon. Department of Geology and Mineral Industries,}
}
