qfaults web comp As of January 12, 2017, the USGS maintains a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. For the most up-to-date information, please refer to the interactive fault map.

Archived report (descriptions no longer maintained)

Cascadia megathrust (Class A) No. 781

Last Review Date: 2006-04-12

County(s) and State(s) CLATSOP COUNTY, OREGON (offshore)
COOS COUNTY, OREGON (offshore)
CURRY COUNTY, OREGON (offshore)
DOUGLAS COUNTY, OREGON (offshore)
LANE COUNTY, OREGON (offshore)
LINCOLN COUNTY, OREGON (offshore)
TILLAMOOK COUNTY, OREGON (offshore)
PACIFIC COUNTY, WASHINGTON (offshore)
DEL NORTE COUNTY, CALIFORNIA (offshore)
HUMBOLDT COUNTY, CALIFORNIA (offshore)
Physiographic province(s) PACIFIC BORDER (offshore)
Reliability of location Poor
Compiled at 1:500,000 scale.
Length (km) 754 km.
Average strike N4°W
Sense of movement Thrust
Dip 9–11° E
Historic earthquake
Most recent prehistoric deformation latest Quaternary (<15 ka)
Slip-rate category Greater than 5.0 mm/yr
References Adams, J., 1984, Active deformation of the Pacific northwest continental margin: Tectonics, v. 3, no. 4, p. 449-472.

Adams, J., 1990, Paleoseismicity of the Cascadia subduction zone—Evidence from turbidites off the Oregon-Washington margin: Tectonics, v. 9, no. 4, p. 569-583.

Adams, J., 1996, Great earthquakes recorded by turbidites off the Oregon-Washington coast, in Rogers, A.M., Walsh, T.J., Kockelman, W.J., and Priest, G.R., eds., Assessing earthquake hazards and reducing risk in the Pacific Northwest: U.S. Geological Survey Professional Paper 1560, v. 1, p. 147-158.

Ando, M., and Balazs, E.I., 1979, Geodetic evidence for aseismic subduction of the Juan de Fuca Pl.: Journal of Geophysical Research, v. 84, no. B6, p. 3023-3028.

Asquith, A.C., 1996, A biostratigraphic test of the "earthquake deformation cycle" at the Salmon River estuary, Oregon, USA: Southampton, U.K., University of Southampton, B.S. thesis, 86 p.

Atwater, B.E., Haraguchi, T., Takada, K., Satake, K., Shimokawa, K., and Baker, D., 2001, Sand sills in huge cores along the Columbia River, Washington: Seismological Research Letters, v. 72, no. 2.

Atwater, B.F., 1987, Evidence for great Holocene earthquakes along the outer coast of Washington State: Science, v. 236, p. 942-944.

Atwater, B.F., 1992, Geologic evidence for earthquakes during the past 2000 years along the Copalis River, southern coastal Washington: Journal of Geophysical Research, v. 97, no. B2, p. 1901-1919.

Atwater, B.F., 1994, Geology of Holocene liquefaction features along the Lower Columbia River at Marsh, Brush, Price, Hunting, and Wallace Islands, Oregon and Washington: U.S. Geological Survey Open-File Report 94-209, 64 p.

Atwater, B.F., 1996, Coastal evidence for great earthquakes in western Washington, in Rogers, A.M., Walsh, T.J., Kockelman, W.J., and Priest, G.R., eds., Assessing earthquake hazards and reducing risk in the Pacific Northwest: U.S. Geological Survey Professional Paper 1560, p. 77-90.

Atwater, B.F., and Hemphill-Haley, E., 1997, Recurrence intervals for great earthquakes of the past 3,500 years at northeastern Willapa Bay, Washington: U.S. Geological Survey Professional Paper 1576, 108 p.

Atwater, B.F., and Yamaguchi, D.K., 1991, Sudden, probably coseismic submergence of Holocene trees and grass in coastal Washington State: Geology, v. 19, p. 706-709.

Atwater, B.F., Nelson, A.R., Clague, J.J., Carver, G.A., Yamaguchi, D.K., Bobrowsky, P.T., Bourgeois, J., Darienzo, M.E., Grant, W.C., Hemphill-Haley, E., Kelsey, H.M., Jacoby, G.C., Nishenko, S.P., Palmer, S.P., Peterson, C.D., and Reinhart, M.A., 1995, Summary of coastal geologic evidence for past great earthquakes at the Cascadia subduction zone: Earthquake Spectra, v. 11, no. 1, p. 1-18.

Atwater, B.F., Stuiver, M., and Yamaguchi, D.K., 1991, Radiocarbon test of earthquake magnitude at Cascadia subduction zone: Nature, v. 353, p. 156-158.

Atwater, T., 1970, Implications of pl. tectonics for the Cenozoic tectonic evolution of western North America: Geological Society of America Bulletin, v. 81, p. 3513-3536.

Barnett, E.T., 1997, Potential for coastal flooding due to coseismic subsidence in the central Cascadia margin: Portland, Oregon, Portland State University, M.S. Thesis, 157 p.

Benson, B.E., Atwater, B.F., Yamaguchi, D.K., Amidon, L.J., Brown, S.L., and Lewis, R.C., 2001, Renewal of tidal forests in Washington State after a subduction earthquake in A.D. 1700: Quaternary Research, v. 56, p. 139-147.

Briggs, G.G., 1994, Coastal crossing of the elastic strain zero-isobase, Cascadia Margin, south central Oregon Coast: Portland State University, unpublished M.S. thesis, 251 p.

Byrne, J.V., Fowler, G.A., and Maloney, N.J., 1966, Uplift of the continental margin and possible continental accretion off Oregon: Science, v. 154, p. 1654-1655.

Carlson, P.R., and Nelson, C.H., 1987, Chapter 21-Marine geology and resource potential of Cascadia Basin, in Scholl, D.W., Grantz, A., and Vedder, J.G., eds., Geology and resource potential of the continental margin of Western North America and adjacent ocean basins—Beaufort Sea to Baja, California: Circum-Pacific Council for Energy and Mineral Resources Earth Science Series, v. 6, p. 523-535.

Clague, J.J., 1997, Evidence for large earthquakes at the Cascadia subduction zone: Reviews of Geophysics, v. 35, no. 4, p. 439-460.

Clague, J.J., Atwater, B.F., Wang, K., Wang, Y., and Wong, I., 2000, Penrose Conference report—Great Cascadia earthquake tricentennial: GSA Today, v. 10, no. 11, p. 14-15.

Crosson, R.S., and Owens, T.J., 1987, Slab geometry of the Cascadia subduction zone beneath Washington from earthquake hypocenters and teleseismic converted waves: Geophysical Research Letters, v. 14, no. 8, p. 824-827.

Darienzo, M.E., 1991, Late Holocene paleoseismicity along the northern Oregon coast: Portland State University, unpublished Ph.D. dissertation, 167 p.

Darienzo, M.E., and Peterson, C.D., 1990, Episodic tectonic subsidence of late Holocene salt marshes, northern Oregon Central Cascadia Margin: Tectonics, v. 9, no. 1, p. 1-22.

Darienzo, M.E., and Peterson, C.D., 1995, Magnitude and frequency of subduction-zone earthquakes along the northern Oregon coast in the past 3,000 years: Oregon Geology, v. 57, no. 1, p. 3-12.

Darienzo, M.E., Peterson, C.D., and Clough, C., 1994, Stratigraphic evidence for great subduction-zone earthquakes at four estuaries in northern Oregon, U.S.A.: Journal of Coastal Research, v. 10, no. 4, p. 851-876.

DeMets, C., Gordon, R.G., Argus, D.F., and Stein, S., 1990, Current pl. motions: Geophysical Journal International, v. 101, p. 425-478.

DeMets, C., Gordon, R.G., Argus, D.F., and Stein, S., 1994, Effect of recent revisions to the geomagnetic reversal time scale on estimates of current pl. motions: Geophysical Research Letters, v. 21, no. 20, p. 2191-2194.

Dragert, H., and Hyndman, R.D., 1995, Continuous GPS monitoring of elastic strain in the northern Cascadia subduction zone: Geophysical Research Letters, v. 22, no. 7, p. 755-758.

Dragert, H., Hyndman, R.D., Rogers, G.C., and Wang, K., 1994, Current deformation and the width of the seismogenic zone of the northern Cascadia subduction thrust: Journal of Geophysical Research, v. 99, no. B1, p. 653-668.

Duncan, J.R., Jr., 1968, Late Pleistocene and post-glacial sedimentation and stratigraphy of deep-sea environments off Oregon: Corvallis, Oregon, Oregon State University, unpublished Ph.D. dissertation, 222 p.

Duncan, R.A., and Kulm, L.D., 1989, Pl. tectonic evolution of the Cascades arc-subduction complex, in Winterer, E.L., Hussong, D.M., and Decker, R.W., eds., The eastern Pacific Ocean and Hawaii: Boulder, Colorado, Geological Society of America, The Geology of North America, v. N, p. 413-428.

Fluck, P., Hyndman, R.D., and Wang, K., 1997, Three-dimensional dislocation model for great earthquakes of the Cascadia subduction zone: Journal of Geophysical Research, v. 102, no. B9, p. 20,539-20,550.

Goldfinger, C., 1994, Active deformation of the Cascadia Forearc—Implications for great earthquake potential in Oregon and Washington: Oregon State University, unpublished Ph.D. dissertation, 246 p., http://hdl.handle.net/1957/36664.

Goldfinger, C., Kulm, L.D., Yeats, R.S., McNeill, L., and Hummon, C., 1997, Oblique strike-slip faulting of the central Cascadia submarine forearc: Journal of Geophysical Research, v. 102, no. B4, p. 8217-8243.

Goldfinger, C., Kulm, L.D., Yeats, R.S., Mitchell, C., Weldon, R., II, Peterson, C., Darienzo, M., Grant, W., and Priest, G.R., 1992, Neotectonic map of the Oregon continental margin and adjacent abyssal plain: State of Oregon, Department of Geology and Mineral Industries Open-File Report 0-92-4, 17 p., 2 pls.

Goldfinger, C., Nelson, C.H., and Johnson, J.E., 2002, Cascadia great earthquake chronology based on the turbidite event record: Geological Society of America Abstracts with Programs, v. 34, no. 5, p. A-36.

Grant, W.C., 1989, More evidence from tidal-marsh stratigraphy for multiple late Holocene subduction earthquakes along the northern Oregon coast: Geological Society of America Abstracts with Programs, v. 21, no. 5, p. 86.

Grant, W.C., and McLaren, D.D., 1987, Seismic potential of Cascadia subduction zone II: Eos, Transactions of the American Geophysical Union, v. 68, no. 44, p. 1239.

Grant, W.C., and Minor, R., 1991, Paleoseismic evidence and prehistoric occupation associated with Late Holocene sudden submergence, northern Oregon coast: Eos, Transactions of the American Geophysical Union, supplement, v. 72, no. 44, p. 313.

Griggs, G.B., and Kulm, L.D., 1970, Sedimentation in Cascadia deep-sea channel: Geological Society of America Bulletin, v. 81, p. 1361-1384.

Guffanti, M., and Weaver, C.S., 1988, Distribution of Late Cenozoic volcanic vents in the Cascade Range—Volcanic arc segmentation and regional tectonic considerations: Journal of Geophysical Research, v. 93, no. B6, p. 6513-6529.

Heaton, T.H., and Hartzell, S.H., 1986, Source characteristics of hypothetical subduction earthquakes in the Northwestern United States: Bulletin of the Seismological Society of America, v. 76, no. 3, p. 675-708.

Heaton, T.H., and Kanamori, H., 1984, Seismic potential associated with subduction in the northwestern United States: Bulletin of the Seismological Society of America, v. 74, no. 3, p. 933-941.

Hemphill-Haley, E., 1995, Diatom evidence for earthquake-induced subsidence and tsunami 300 yr ago in southern coastal Washington: Geological Society of America Bulletin, v. 107, p. 367-378.

Hemphill-Haley, E., 1996, Diatoms as an aid in identifying late-Holocene tsunami deposits: The Holocene, v. 6, p. 439-448.

Hughes, J.M., and Carr, M.J., 1980, Segmentation of the Cascade volcanic chain: Geology, v. 8, p. 15-17.

Hyndman, R.D., and Wang, K., 1995, The rupture zone of Cascadia great earthquakes from current deformation and the thermal regime: Journal of Geophysical Research, v. 100, no. B11, p. 22,133-22,154.

Jacoby, G.C., Bunker, D.E., and Benson, B.E., 1997, Tree-ring evidence for an A.D. 1700 Cascadia earthquake in Washington and northern Oregon: Geology, v. 25, no. 11, p. 999-1002.

Karlin, R.E., Holmes, M., Abella, S.E.B., and Sylwester, R., 2004, Holocene landslides and a 3500-year record of Pacific Northwest earthquakes from sediments in Lake Washington: Geological Society of America Bulletin, v. 116, p. 94-108.

Kelsey, H.M., Engebretson, D.C., Mitchell, C.E., and Ticknor, R.L., 1994, Topographic form of the coast ranges of the Cascadia Margin in relation to coastal uplift rates and pl. subduction: Journal of Geophysical Research, v. 99, no. B6, p. 12,245-12,255.

Kelsey, H.M., Nelson, A.R., Hemphill-Haley, E., and Witter, R.C., 1998, Short-term and long-term changes in ocean level recorded by a coastal, freshwater meromictic lake, Cascadia subduction zone, southern Oregon: Geological Society of America Abstracts with Programs, v. 30, no. 7, p. 162.

Kelsey, H.M., Witter, R.C., and Hemphill-Haley, E., 1996, Late Holocene relative sea level history at Cape Blanco, Oregon: Technical report to U.S. Geological Survey, under Contract 1434-93-G-2321, 46 p.

Kelsey, H.M., Witter, R.C., and Hemphill-Haley, E., 1998, Response of a small Oregon estuary to coseismic subsidence and postseismic uplift in the past 300 years: Geology, v. 26, no. 3, p. 231-234.

Kelsey, H.M., Witter, R.C., and Hemphill-Haley, E., 2002, Pl.-boundary earthquakes and tsunamis of the past 5500 yr, Sixes River estuary, southern Oregon: Geological Society of America Bulletin, v. 114, no. 3, p. 298-314.

Kulm, L.D., and Embley, R.W., 1988, Nature of the deformation front along the Oregon-Washington subduction zone, in Shearer, C.F., ed., Minutes of the National Earthquake Prediction Evaluation Council April 2 and 3, 1987: U.S. Geological Survey Open-File Report 88-37, p. 185-195.

Kulm, L.D., Suess, E., Moore, J.C., Carson, B., Lewis, B.T., Ritger, S.D., Kadko, D.C., Thornburg, T.M., Embley, R.W., Rugh, W.D., Massoth, G.J., Langseth, M.G., Cochrane, G.R., and Scamman, R.L., 1986, Oregon subduction zone—Venting, fauna, and carbonates: Science, v. 231, p. 561-566.

Long, A.J., and Shennan, I., 1998, Models of rapid relative sea-level change in Washington and Oregon, USA: The Holocene, v. 8, p. 129-142.

Long, A.J., Innes, J.B., Shennan, I., and Tooley, M.J., 1999, Coastal stratigraphy—A case study from Johns River, Washington, U.S.A., in Jones, A.P., Tucker, M.E., and Hola, J.K., eds., The description and analysis of Quaternary stratigraphic field sections: London, Quaternary Research Association, p. 267-286.

McCaffrey, R., and Goldfinger, C., 1995, Forearc deformation and great subduction earthquakes—Implications for Cascadia offshore earthquake potential: Science, v. 267, p. 856-859.

McKenzie, D.P., and Parker, R.L., 1967, The North Pacific—An example of tectonics on a sphere: Nature, v. 216, p. 1276-1280.

McNeill, L.C., Goldfinger, C., Yeats, R.S., and Kulm, L.D., 1998, The effects of upper pl. deformation on records of prehistoric Cascadia subduction zone earthquakes, in Stewart, I.S., and Vita-Finzi, C., eds., Coastal tectonics: Geological Society Special Publication No. 146, p. 321-342.

McNeill, L.C., Goldfinger, G., Kulm, L.D., and Yeats, R.S., 2000, Tectonics of the Neogene Cascadia forearc basin: Investigations of a deformed late Miocene unconformity: Geological Society of America Bulletin, v. 112, no. 8, p. 1209-1224.

Meyers, R.A., Smith, D.G., Jol, H.M., and Peterson, C.D., 1996, Evidence for eight great earthquake-subsidence events detected with ground-penetrating radar, Willapa barrier, Washington: Geology, v. 24, no. 2, p. 99-102.

Michaelson, C.A., and Weaver, C.S., 1986, Upper mantle structure from teleseismic P wave arrivals in Washington and northern Oregon: Journal of Geophysical Research, v. 91, no. B2, p. 2077-2094.

Mitchell, C.E., Vincent, P., Weldon, R.J., III, and Richards, M.A., 1994, Present-day vertical deformation of the Cascadia margin, Pacific Northwest, United States: Journal of Geophysical Research, v. 99, no. B6, p. 12,257-12,277.

Morgan, W.J., 1968, Rises, trenches, great faults, and crustal blocks: Journal of Geophysical Research, v. 73, no. 6, p. 1959-1983.

Nelson, A.R., 1992, Discordant 14C from buried tidal-march soils in the Cascadia subduction zone, southern Oregon Coast: Quaternary Research, v. 38, p. 74-90.

Nelson, A.R., 1992, Holocene tidal-marsh stratigraphy in south-central Oregon—Evidence for localized sudden submergence in the Cascadia subduction zone, in Fletcher, C.H., III, and Wehmiller, J.F., eds., Quaternary coasts of the United States—Marine and lacustrine systems: SEPM Special Publication No. 48, p. 287-301.

Nelson, A.R., and Personius, S.F., 1996, Great-earthquake potential in Oregon and Washington—An overview of recent coastal geologic studies and their bearing on segmentation of Holocene ruptures, central Cascadia subduction zone, in Rogers, A.M., Walsh, T.J., Kockelman, W.J., and Priest, G.R., eds., Assessing earthquake hazards and reducing risk in the Pacific Northwest: U.S. Geological Survey Professional Paper 1560, v. 1, p. 91-114.

Nelson, A.R., Atwater, B.F., Bobrowsky, P.T., Bradley, L.-A., Clague, J.J., Carver, G.A., Darienzo, M.E., Grant, W.C., Krueger, H.W., Sparks, R., Stafford, T.W., and Stuiver, J.M., 1995, Radiocarbon evidence for extensive pl.-boundary rupture about 300 years ago at the Cascadia subduction zone: Nature, v. 378, p. 371-374.

Nelson, A.R., Jennings, A.E., and Kashima, K., 1996, An earthquake history derived from stratigraphic and microfossil evidence of relative sea-level change at Coos Bay, southern coastal Oregon: Geological Society of America Bulletin, v. 108, no. 2, p. 141-154.

Nelson, A.R., Kelsey, H.M., and Hemphill-Haley, E., 1996, A 7500 year lake record of Cascadia tsunamis in southern coastal Oregon: Geological Society of America Abstracts with Programs, v. 28, no. 5, p. 95.

Nelson, A.R., Kelsey, H.M., Hemphill-Haley, E., and Witter, R.C., 1998, AMS 14C dating of a 7300-year earthquake history from an Oregon coastal lake: Geological Society of America Abstracts with Programs, v. 30, no. 7, p. 162.

Nelson, A.R., Ota, Y., Umitsu, M., Kashima, K., and Matsushima, Y., 1998, Seismic or hydrodynamic control of rapid late-Holocene sea-level rises in southern coastal Oregon, USA?: The Holocene, v. 8, no. 3, p. 287-299.

Nelson, A.R., Shennan, I., and Long, A.J., 1996, Identifying coseismic subsidence in tidal-wetland stratigraphic sequences at the Cascadia subduction zone of western North America: Journal of Geophysical Research, v. 101, no. B3, p. 6115-6135.

Nelson, C.H., 1984, The Astoria Fan—An elongate type fan: Geo-Marine Letters, v. 3, p. 65-70.

Nelson, C.H., Carlson, P.R., Byrne, J.V., and Alpha, T.R., 1970, Development of the Astoria Canyon—Fan physiography and comparison with similar systems: Marine Geology, v. 8, p. 259-291.

Nelson, C.H., Goldfinger, C., and Johnson, J.E., 2000, Turbidite event stratigraphy and implications for Cascadia basin paleoseismicity, in Clague, J.J., Atwater, B.F., Wang, K., Wang, Y., and Wong, I., eds., Penrose Conference 2000 Great Cascadia earthquake tricentennial: State of Oregon, Department of Geology and Mineral Industries Special Paper 33, p. 156.

Nelson, C.H., Goldfinger, C., Vallier, T.L., McGann, M.L., and Kashgarian, M., 1996, North to south variation in Cascadia Basin turbidite event history—Implications for paleoseismicity: Geological Society of America Abstracts with Programs, v. 28, no. 5, p. 96.

Nelson, C.H., Goldfinger, C., Wolf, S.C., and Dunhill, G., 1999, Cascadia Basin channel pathways and late Holocene turbidite event history: American Association of Petroleum Geologists, v. 1999, p. A100.

Obermeier, S.F., and Dickenson, S.E., 1997, Liquefaction evidence for the strength of ground motions from a Cascadia subduction earthquake about 300 years ago, in Wang, Y., and Neuendorf, K.K.E., eds., Earthquakes—Converging at Cascadia: State of Oregon, Department of Geology and Mineral Industries Special Paper 28, p. 53-77.

Ota, Y., and Unitsu, M., 1995, Stratigraphic, radiocarbon, and diatom indicators of sudden submergence along the Naselle River mouth, Washington, USA [in Japanese with English abstract]: Journal of Geography [Japan], v. 104, p. 107-112.

Ota, Y., Nelson, A.R., Umitsu, M., Kashima, K., and Matsushima, Y., 1995, Interpreting an earthquake history from the stratigraphy of late Holocene intertidal deposits in South Slough, Coos Bay, Oregon, USA: Journal of Geography, v. 104, no. 1, p. 94-106.

Parsons, T., Trehu, A.M., Luetgert, J.H., Miller, K., Kilbride, F., Wells, R.E., Fisher, M.A., Flueh, E., ten Brink, U.S., and Christensen, N.I., 1998, A new view into the Cascadia subduction zone and volcanic arc—Implications for earthquake hazards along the Washington margin: Geology, v. 26, no. 3, p. 199-202.

Personius, S.F., 1995, Late Quaternary stream incision and uplift in the forearc of the Cascadia subduction zone, western Oregon: Journal of Geophysical Research, v. 100, no. B10, p. 20,193-20,210.

Peterson, C.D., and Darienzo, M.E., 1996, Discrimination of climatic, oceanic, and tectonic mechanisms of cyclic marsh burial, Alsea Bay, Oregon, in Rogers, A.M., Walsh, T.J., Kockelman, W.J., and Priest, G.R., eds., Assessing earthquake hazards and reducing risk in the Pacific Northwest: U.S. Geological Survey Professional Paper 1560, v. 1, p. 115-146.

Peterson, C.D., and Madin, I.P., 1997, Coseismic paleoliquefaction evidence in the central Cascadia margin, USA: Oregon Geology, v. 59, no. 3, p. 51-74.

Peterson, C.P., Kulm, L.D., and Gray, J.J., 1986, Geologic map of the ocean floor off Oregon and the adjacent continental margin: State of Oregon Geological Map Series GMS-42, 1 sheet, scale 1:500,000.

Rasmussen, J., and Humphreys, E., 1988, Tomographic image of the Juan De Fuca Pl. beneath Washington and western Oregon using teleseismic P-wave travel times: Geophysical Research Letters, v. 15, no. 12, p. 1417-1420.

Reinhart, M.A., and Bourgeois, J., 1989, Tsunami favored over storm or seiche for sand deposit overlying buried Holocene peat, Willapa Bay, WA: Eos, Transactions of the American Geophysical Union, v. 70, no. 43, p. 1331.

Riddihough, R., 1984, Recent movements of the Juan de Fuca Pl. System: Journal of Geophysical Research, v. 89, no. B8, p. 6980-6994.

Rieken, E., and Thiessen, R.L., 1992, Three-dimensional model of the Cascadia subduction zone using earthquake hypocenters, western Washington: Bulletin of the Seismological Society of America, v. 82, no. 6, p. 2533-2548.

Rogers, G.C., 1988, An assessment of the megathrust earthquake potential of the Cascadia subduction zone: Canadian Journal of Earth Sciences, v. 25, p. 844-852.

Satake, K., Shimazaki, K., Tsuji, Y., and Ueda, K., 1996, Time and size of a giant earthquake in Cascadia inferred from Japanese tsunami records in January 1700: Nature, v. 379, p. 246-249.

Satake, K., Wang, K., and Atwater, B.F., 2003, Fault slip and seismic moment of the 1700 Cascadia earthquake inferred from Japanese tsunami descriptions: Journal of Geophysical Research, v. 108, no. 11, 17 p.

Savage, J.C., and Lisowski, M., 1991, Strain measurements and the potential for a great subduction earthquake off the coast of Washington: Science, v. 252, p. 101-103.

Savage, J.C., Lisowski, M., and Prescott, W.H., 1991, Strain accumulation in western Washington: Journal of Geophysical Research, v. 96, no. B9, p. 14,493-14,507.

Savage, J.C., Svarc, J.L., Prescott, W.H., and Murray, M.H., 2000, Deformation across the forearc of the Cascadia subduction zone at Cape Blanco, Oregon: Journal of Geophysical Research, v. 105, no. B2, p. 3095-3102.

Schuster, R.L., Logan, R.L., and Pringle, P.T., 1992, Prehistoric rock avalanches in the Olympic Mountains, Washington: Science, v. 258, p. 1620-1621.

Shennan, I., and Long, A.J., 1994, Sea-level changes in Washington and Oregon and the "earthquake deformation cycle": Journal of Coastal Research, v. 10, p. 825-838.

Shennan, I., Long, A.J., Rutherford, M.M., Innes, J.B., Green, F.M., and Walker, K.J., 1996, Tidal marsh stratigraphy, sea-level change and large earthquakes-I—A 5000 year record in Washington, USA: Quaternary Science Reviews, v. 15, p. 1023-1059.

Shennan, I., Long, A.J., Rutherford, M.M., Innes, J.B., Green, F.M., and Walker, K.J., 1998, Tidal marsh stratigraphy, sea-level change and large earthquakes-II—Submergence events during the last 3500 years at Netarts Bay, Oregon, USA: Quaternary Science Reviews, v. 17, p. 365-393.

Silver, E.A., 1969, Late Cenozoic underthrusting of the continental margin off northernmost California: Science, v. 166, p. 1265-1266.

Silver, E.A., 1971, Transitional tectonics and Late Cenozoic structure of the continental margin off northernmost California: Geological Society of America Bulletin, v. 82, p. 1-22.

Siskowic, J., Anderson, D., Peterson, B., Peterson, C., Soar, M., Travis, P., and Volker, K., 1994, Possible coseismic liquefaction evidence at the Sandy River delta, Portland, Oregon—Tentative correlation with the last Great Cascadia rupture: Geological Society of America Abstracts with Programs, v. 26, no. 2, p. 92.

Taber, J.J., and Lewis, B.T.R., 1986, Crustal structure of the Washington continental margin from refraction data: Bulletin of the Seismological Society of America, v. 76, no. 4, p. 1011-1024.

Taber, J.J., and Smith, S.W., 1985, Seismicity and focal mechanisms associated with the subduction of the Juan de Fuca Pl. beneath the Olympic Peninsula, Washington: Bulletin of the Seismological Society of America, v. 75, no. 1, p. 237-249.

Takada, K., Satake, K., and Shimokawa, K., 2002, Geoslicing and liquefaction along the Columbia river at Hunting Island, Washington: Seismological Research Letters, v. 73, no. 2.

Takada, K., Satake, K., Shimokawa, K., Nakata, T., and Haraguchi, T., 2001, Geosliced roots of liquefaction features from great Cascadia earthquakes: Eos, Transactions of the American Geophysical Union, Abstract S52C-0644, v. 82, no. 47, supplement.

Tobin, D.G., and Sykes, L.R., 1968, Seismicity and tectonics of the Northeast Pacific Ocean: Journal of Geophysical Research, v. 73, no. 12, p. 3821-3845.

Trehu, A.M., Asudeh, I., Brocher, T.M., Luetgert, J.H., Mooney, W.D., Nabelek, J.L., and Nakamura, Y., 1994, Crustal architecture of the Cascadia forearc: Science, v. 265, p. 237-243.

Trehu, A.M., Lin, G., Maxwell, E., and Goldfinger, C., 1995, A seismic reflection profile across the Cascadia subduction zone offshore central Oregon-New constraints on methane distribution and crustal structure: Journal of Geophysical Research, v. 100, no. B8, p. 15,101-15,116.

Volker, K., Anderson, D., Peterson, B., Peterson, C., Siskowic, J., Soar, M., and Travis, P., 1994, Discrimination of liquefaction-inducing events (lahar, flood and seismic) at the Sandy River delta, Troutdale, Oregon: Geological Society of America Abstracts with Programs, v. 26, no. 2, p. 101.

Wang, Y., He, J., Dragert, H., and James, T.S., 2001, Three-dimensional viscoelastic interseismic deformation model for the Cascadia subduction zone: Earth, Planets and Space, v. 53, p. 295-306.

Weaver, C.S., and Baker, G.E., 1988, Geometry of the Juan de Fuca Pl. beneath Washington and northern Oregon from seismicity: Bulletin of the Seismological Society of America, v. 78, no. 1, p. 264-275.

Weaver, C.S., and Michaelson, C.A., 1985, Seismicity and volcanism in the Pacific Northwest—Evidence for the segmentation of the Juan de Fuca Pl.: Geophysical Research Letters, v. 12, no. 4, p. 215-218.

Weaver, C.S., and Shedlock, K.M., 1996, Estimates of seismic source regions from the earthquake distribution and regional tectonics in the Pacific Northwest, in Rogers, A.M., Walsh, T.J., Kockelman, W.J., and Priest, G.R., eds., Assessing earthquake hazards and reducing risk in the Pacific Northwest: U.S. Geological Survey Professional Paper 1560, v. 1, p. 285-306.

Williams, H., and Hutchinson, I., 2000, Stratigraphic and microfossil evidence for late Holocene tsunamis at Swantown marsh, Whidbey Island, Washington: Quaternary Research, v. 54, p. 218-227.

Williams, H., Hutchinson, I., and Nelson, A.R., 2004, Multiple sources for late Holocene tsunamis at Discovery Bay, Washington State, USA: The Holocene, (in press).

Witter, R.C., 1999, Late Holocene paleoseismicity, tsunamis and relative sea-level changes along the south-central Cascadia subduction zone, southern Oregon: University of Oregon, unpublished Ph.D. dissertation, 178 p.

Witter, R.C., Kelsey, H.M., and Hemphill-Haley, E., 1997, A paleoseismic history of the south-central Cascadia subduction zone—Assessing earthquake recurrence intervals and upper-pl. deformation over the past 6600 years at the Coquille River Estuary, southern Oregon: Technical report to U.S. Geological Survey, under Contract 1434-HQ-97-GR-03036, 54 p.

Witter, R.C., Kelsey, H.M., and Hemphill-Haley, E., 2003, Great Cascadia earthquakes and tsunamis of the past 6,700 years, Coquille River estuary, southern coastal Oregon: Geological Society of America Bulletin, v. 115, p. 1289-1306.

Yamaguchi, D.K., Atwater, B.F., Bunker, D.E., Benson, B.E., and Reid, M.S., 1997, Tree-ring dating the 1700 Cascadia earthquake: Nature, v. 389, p. 922-923.

Yeats, R.S., Kulm, L.D., Goldfinger, C., and McNeill, L.C., 1998, Stonewall anticline—An active fold on the Oregon continental shelf: Geological Society of America Bulletin, v. 110, no. 5, p. 572-587.

Yeats, R.S., McNeill, L.C., and Goldfinger, C., 2001, Coastal and offshore crustal faulting in Cascadia—Is it real and what are the implications for society?: Seismological Research Letters, v. 72, no. 2, p. 253-254.