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Great earthquakes of variable magnitude at the Cascadia subduction zone

Published online by Cambridge University Press:  20 January 2017

Alan R. Nelson ,
Harvey M. Kelsey  and
Robert C. Witter
Alan R. Nelson*
Affiliation:
Geologic Hazards Team, U.S. Geological Survey, MS 966, PO Box 25046, Denver, CO 80225, USA
Harvey M. Kelsey
Affiliation:
Department of Geology, Humboldt State University, Arcata, CA 95521, USA
Robert C. Witter
Affiliation:
Oregon Department of Geology and Mineral Industries, Coastal Field Office, 313 SW 2nd St., Suite D, Newport, OR 97365, USA
*
*Corresponding author. E-mail address:[email protected] (A.R. Nelson).
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Abstract

Comparison of histories of great earthquakes and accompanying tsunamis at eight coastal sites suggests plate-boundary ruptures of varying length, implying great earthquakes of variable magnitude at the Cascadia subduction zone. Inference of rupture length relies on degree of overlap on radiocarbon age ranges for earthquakes and tsunamis, and relative amounts of coseismic subsidence and heights of tsunamis. Written records of a tsunami in Japan provide the most conclusive evidence for rupture of much of the plate boundary during the earthquake of 26 January 1700. Cascadia stratigraphic evidence dating from about 1600 cal yr B.P., similar to that for the 1700 earthquake, implies a similarly long rupture with substantial subsidence and a high tsunami. Correlations are consistent with other long ruptures about 1350 cal yr B.P., 2500 cal yr B.P., 3400 cal yr B.P., 3800 cal yr B.P., 4400 cal yr B.P., and 4900 cal yr B.P. A rupture about 700–1100 cal yr B.P. was limited to the northern and central parts of the subduction zone, and a northern rupture about 2900 cal yr B.P. may have been similarly limited. Times of probable short ruptures in southern Cascadia include about 1100 cal yr B.P., 1700 cal yr B.P., 3200 cal yr B.P., 4200 cal yr B.P., 4600 cal yr B.P., and 4700 cal yr B.P. Rupture patterns suggest that the plate boundary in northern Cascadia usually breaks in long ruptures during the greatest earthquakes. Ruptures in southernmost Cascadia vary in length and recurrence intervals more than ruptures in northern Cascadia.

Keywords

PaleoseismologySubduction zoneEarthquake hazardsRadiocarbon correlationCoseismic subsidenceTsunami depositEarthquake recurrencePlate-boundary earthquakes
Type
Research Article
Information
Quaternary Research , Volume 65 , Issue 3 , May 2006 , pp. 354 - 365
Copyright
University of Washington

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References

Abramson, H.F., (1998). Evidence for tsunamis and earthquakes during the last 3500 years from Lagoon Creek, a coastal freshwater marsh, northern California [MS thesis].. Humboldt State University, 76 pp.Google Scholar
Ando, M., (1975). Source mechanisms and tectonic significance of historical earthquakes along the Nankai Trough, Japan. Tectonophysics 27, 119–140.Google Scholar
Atwater, B.F., (1987). Evidence for great Holocene earthquakes along the outer coast of Washington state. Science 236, 942–944.CrossRefGoogle ScholarPubMed
Atwater, B.F., (1992). Geologic evidence for earthquakes during the past 2000 years along the Copalis River, southern coastal Washington. Journal of Geophysical Research 97, B2 1901–1919.Google Scholar
Atwater, B.F., Hemphill-Haley, E., (1997). Recurrence intervals for great earthquakes of the past 3500 years at northeastern Willapa Bay, Washington.. U.S. Geological Survey Professional Paper 1576, 108 pp.Google Scholar
Atwater, B.F., Stuiver, M., Yamaguchi, D.K., (1991). A radiocarbon test of earthquake magnitude at the Cascadia subduction zone. Nature 353, 156–158.Google Scholar
Atwater, B.F., Nelson, A.R., Clague, J.J., Carver, G.A., Bobrowsky, 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., Reinhart, M.A., Yamaguchi, D.K., (1995). Summary of coastal geologic evidence for past great earthquakes at the Cascadia subduction zone. Earthquake Spectra 11, 1–18.Google Scholar
Atwater, B.F., Yamaguchi, D.K., Bondevik, S., Barnhardt, W.A., Amidon, L.J., Benson, B.E., Skjerdal, G., Shulene, J.A., Nanayama, F., (2001). Rapid resetting of an estuarine recorder of the 1964 Alaska earthquake. Geological Society of America 113, 1193–1204.2.0.CO;2>CrossRefGoogle Scholar
Atwater, B.F., Tuttle, M., Schweig, E.S., Rubin, C.M., Yamaguchi, D.K., Hemphill-Haley, E., (2004). Earthquake recurrence inferred from paleoseismology. Gillespie, A.R., Porter, S.C., Atwater, B.F., The Quaternary period in the United States, Developments in Quaternary Science Elsevier, New York.331–350.Google Scholar
Atwater, B.F., Musumi-Rokkaku, S., Satake, K. Tsuji, Y., Ueda, K., Yamaguchi, D.K., (2005). The orphan tsunami of 1700–Japanese clues to a parent earthquake in North America, U.S. Geological Survey Professional Paper 1707. 133 p. (published jointly by University of Washington Press, Seattle.).Google Scholar
Bronk Ramsey, C., (2001). Development of the radiocarbon program OxCal. Radiocarbon 43, 355–363.Google Scholar
Charland, J.W., Priest, G.R., (1995). Inventory of critical and essential facilities vulnerable to earthquake or tsunami hazards on the Oregon coast.. Oregon Department of Geology and Mineral Industries Open-File Report O-95-02, 52 p.Google Scholar
Cisternas, M., Atwater, B.F., Torrejón, F., Sawai, Y., Machuca, G., Lagos, M., Eipert, A., Youlton, C., Salgado, I., Kamataki, T., Shishikura, M., Rajendran, C.P., Malik, J.K., Rizal, Y., Husni, M., (2005). Predecessors to the giant 1960 Chile earthquake. Nature 437, 404–407.CrossRefGoogle Scholar
Clague, J.J., (1997). Evidence for large earthquakes at the Cascadia subduction zone. Reviews of Geophysics 35, 439–460.CrossRefGoogle Scholar
Clague, J.J., Atwater, B.F., Wang, K., Wang, Y., Wong, I., compilers, (2000a). Geological Society of America Penrose Conference 2000 (Seaside, Oregon, 2–8 June 2000)–Great Cascadia Earthquake Tricentennial, Program Summary and Abstracts.. Oregon Department of Geology and Mineral Industries, Special Paper 33, 156 p.Google Scholar
Clague, J.J., Bobrowsky, T., Hutchinson, I., (2000b). A review of geological records of large tsunamis at Vancouver Island, British Columbia, and implications for hazard. Quaternary Science Reviews 19, 849–863.Google Scholar
Darienzo, M.E., Peterson, C.D., (1990). Episodic tectonic subsidence of late Holocene salt marshes, northern Oregon central Cascadia margin. Tectonics 9, 1–22.CrossRefGoogle Scholar
Darienzo, M.E., Peterson, C.D., (1995). Magnitude and frequency of subduction-zone earthquakes along the northern Oregon coast in the past 3,000 years. Oregon Geology 57, 3–12.Google Scholar
Edwards, R.J., Horton, B.P., (2006). Developing detailed records of relative sea-level change using a foraminiferal transfer function: An example from North Norfolk, U.K.. Philos. Trans. R. Soc. London A 364, 973–991.Google Scholar
Frankel, A.D., Petersen, M.D., Mueller, C.S., Haller, K.M., Wheeler, R.L., Leyendecker, E.V., Wesson, R.L., Harmsen, S.C., Cramer, C.H., Perkins, D.M., Rukstales, K.S., (2002). Documentation for the 2002 update of the national seismic hazard maps.. U.S. Geological Survey Open-File Report 02-420, 33 p. (http://geohazards.cr.usgs.gov/eq/of02-420/OFR02-420.pdf).Google Scholar
Garrison-Laney, C.E., (1998). Diatom evidence for tsunami inundation from Lagoon Creek, a coastal freshwater pond, Del Norte County, California [MS thesis].. Humboldt State University, 97 pp.Google Scholar
Geist, E., Yoshioka, S., (1996). Source parameters controlling the generation and propagation of potential local tsunamis along the Cascadia margin. Natural Hazards 13, 2 151–177.Google Scholar
Goldfinger, C., Kulm, L.D., McNeil, L.C., Watts, P., (2000). Super-scale failure of the southern Oregon Cascadia margin. Pure and Applied Geophysics 157, 1189–1226.CrossRefGoogle Scholar
Goldfinger, C., Nelson, C.H., Johnson, J.E., (2003). Holocene earthquake records from the Cascadia subduction zone and northern San Andreas fault based on precise dating of offshore turbidites. Annual Review of Earth and Planetary Sciences 31, 555–577.CrossRefGoogle Scholar
Guilbault, J.-P., Clague, J.J., Lapointe, M., (1995). Foraminiferal evidence for the amount of coseismic subsidence during a late Holocene earthquake on Vancouver Island, west coast of Canada. Quaternary Science Reviews 15, 913–937.Google Scholar
Grant, W.C., (1989). Radiocarbon dating of late Holocene coastal subsidence above the Cascadia subduction zone–Compilation for Washington, Oregon, and northern California. EOS, Transactions of the American Geophysical Union 70, 43 1331.Google Scholar
Heaton, T.H., Hartzell, S.H., (1987). Earthquake hazards on the Cascadia subduction zone. Science 236, 162–168.Google Scholar
Hemphill-Haley, E., (1995). Diatom evidence for earthquake-induced subsidence and tsunami 300 yr ago in southern coastal Washington. Geological Society of America Bulletin 107, 367–378.Google Scholar
Hughes, J.F., Mathewes, R.W., Clague, J.J., (2002). Use of pollen and vascular plants to estimate coseismic subsidence at a tidal marsh near Tofino, British Columbia. Palaeogeography, Palaeoclimatology, Palaeoecology 185, 145–161.Google Scholar
Hyndman, R.D., Wang, K., (1995). The rupture zone of Cascadia great earthquakes from current deformation and the thermal regime. Journal of Geophysical Research 100, 22,133–22,154.CrossRefGoogle Scholar
Jacoby, G.C., Carver, G., Wagner, W., (1995). Trees and herbs killed by an earthquake 300 yr ago at Humboldt Bay, California. Geology 23, 77–80.2.3.CO;2>CrossRefGoogle Scholar
Jacoby, G.C., Bunker, D.E., Benson, B.E., (1997). Tree-ring evidence for an A.D. 1700 Cascadia earthquake in Washington and northern Oregon. Geology 29, 999–1002.2.3.CO;2>CrossRefGoogle Scholar
Kelsey, H.M., Witter, R.C., Hemphill-Haley, E., (1998). Response of a small Oregon estuary to coseismic subsidence and postseismic uplift in the past 300 years. Geology 26, 231–234.Google Scholar
Kelsey, H.M., Witter, R.C., Hemphill-Haley, E., (2002). Plate-boundary earthquakes and tsunamis of the past 5500 years, Sixes River estuary, southern Oregon. Geological Society of America Bulletin 114, 298–314.Google Scholar
Kelsey, H.M., Nelson, A.R., Hemphill-Haley, E., Witter, R., (2005). Tsunami history of an Oregon coastal lake reveals a 4600 yr record of great earthquakes on the Cascadia subduction zone. Geological Society of America Bulletin 117, 1009–1032.Google Scholar
Leonard, L.J., Hyndman, R.D., Mazzotti, S., (2004). Coseismic subsidence in the 1700 great Cascadia earthquake: coastal estimates versus elastic dislocation models. Geological Society of America Bulletin 116, 655–670.CrossRefGoogle Scholar
McAdoo, B.G., Watts, P., (2004). Tsunami hazard from submarine landslides on the Oregon continental slope. Marine Geology 203, 235–245.Google Scholar
McCaffrey, R., Goldfinger, C., (1995). Forearc deformation and great subduction earthquakes: implications for Cascadia offshore earthquake potential. Science 267, 856–859.Google Scholar
McCalpin, J.P., Nelson, A.R., (1996). Introduction to paleoseismology. McCalpin, J.P., Paleoseismology Academic Press, Orlando, FL.1–32.Google Scholar
Myers, E., Baptista, A.M., Priest, G.R., (1999). Finite element modeling of potential Cascadia subduction zone tsunamis. Science of Tsunami Hazards 17, 3–18.Google Scholar
Nanayama, F., Satake, K., Furukawa, R., Shimokawa, K., Atwater, B.F., Shigeno, K., Yamaki, S., (2003). Unusually large earthquakes inferred from tsunami deposits along the Kuril trench. Nature 424, 660–663.Google Scholar
Nelson, A.R., (1992a). Discordant 14C ages from buried tidal-marsh soils in the Cascadia subduction zone, southern Oregon coast. Quaternary Research 38, 74–90.Google Scholar
Nelson, A.R., (1992b). Holocene tidal-marsh stratigraphy in south-central Oregon–Evidence for localized sudden submergence in the Cascadia subduction zone. Fletcher, C.P., Wehmiller, J.F., Quaternary Coasts of the United States-Marine and Lacustrine Systems. Tulsa, Oklahoma Society for Sedimentary Geology Special Publication no. 48, 287–301.Google Scholar
Nelson, A.R., Personius, S.F., (1996). The potential for great earthquakes 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., Priest, G.R. (Eds.), Earthquake hazards in the Pacific Northwest of the United States. U.S. Geological Survey Professional Paper 1560, 91–114.Google Scholar
Nelson, A.R., Atwater, B.F., Bradley, L.-A., Stafford, T.W., (1994). AMS 14C correlation of subsided wetland soils using rooted-herb and detrital samples in the Cascadia subduction zone. Geological Society of America Abstracts with Programs 26, 7 A-522.Google Scholar
Nelson, A.R., Atwater, B.F., Bobrowsky, T., Bradley, L.-A., Clague, J.J., Carver, G.A., Darienzo, M.E., Grant, W.C., Krueger, H.W., Sparks, R., Stafford, T.W. Jr., Stuiver, M., (1995). Radiocarbon evidence for extensive plate-boundary rupture about 300 years ago at the Cascadia subduction zone. Nature 378, 371–374.CrossRefGoogle Scholar
Nelson, A.R., Shennan, I., Long, A.J., (1996a). Identifying coseismic subsidence in tidal-wetland stratigraphic sequences at the Cascadia subduction zone of western North America. Journal of Geophysical Research 101, B3 6115–6135.Google Scholar
Nelson, A.R., Jennings, A.E., Kashima, K., (1996b). 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 108, 141–154.Google Scholar
Nelson, A.R., Ota, Y., Umitsu, M., Kashima, K., Matshushima, Y., (1998). Seismic or hydrodynamic control of rapid late-Holocene sea-level rise in southern coastal Oregon, USA?. The Holocene 8, 287–299.Google Scholar
Nelson, A.R., Jennings, A.E., Gerson, L.D., Sherrod, B.L., (2000). Differences in great earthquake rupture extent inferred from tsunami-laid sand and foraminiferal assemblages beneath intertidal marshes at Alsea Bay, central Oregon coast. Geological Society of America Abstracts with Programs 32, 7 A-443.Google Scholar
Petersen, M.D., Cramer, C.H., Frankel, A.D., (2002). Simulations of seismic hazard for the Pacific Northwest of the United States from earthquakes associated with the Cascadia subduction zone. Pure and Applied Geophysics 159, 2147–2168.Google Scholar
Peterson, C.D., 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., Priest, G.R. (Eds.), Assessing earthquake hazards and reducing risk in the Pacific Northwest. U.S. Geological Survey Professional Paper 1560, 115–146.Google Scholar
Peterson, C.D., Doyle, D.L., Barnett, E.T., (2000). Coastal flooding and beach retreat from coseismic subsidence in the central Cascadia margin, USA. Environmental and Engineering Geoscience 6, 255–269.Google Scholar
Ruff, L.J., (1996). Large earthquakes in subduction zones: segment interaction and recurrence times. Bebout, G.E., Scholl, D.W., Kirby, S.H., Platt, J.P., Subduction Top to Bottom Geophysical Monographs vol. 96, 91–104.Google Scholar
Satake, K., Wang, K., Atwater, B.F., (2003). Fault slip and seismic moment of the 1700 Cascadia earthquake inferred from Japanese tsunami descriptions. Journal of Geophysical Research 108, B11 2535(10.1029/2003JB002521).CrossRefGoogle Scholar
Sawai, Y., Satake, K., Takanobu, K., Nasu, H., Shishikura, M., Atwater, B.F., Horton, B.P., Kelsey, H.M., Nagumo, T., Yamaguchi, M., (2004). Transient uplift after a 17th-century earthquake along the Kuril subduction zone. Science 306, 1918–1920.Google Scholar
Shennan, I., Hamilton, S.L., (2006). Coseismic and pre-seismic subsidence associated with great earthquakes in Alaska. Quaternary Science Reviews 25, 1–8.CrossRefGoogle Scholar
Shennan, I., Long, A.J., Rutherford, M.M., Green, F.M., Innes, J.B., Lloyd, J.M., Zong, Y., Walker, K.J., (1996). Tidal marsh stratigraphy, sea-level change and large earthquakes: I. A 5000 Science year record in Washington, USA. Quaternary Reviews 15, 1023–1059.Google Scholar
Thatcher, W., (1990). Order and diversity in the modes of circum-Pacific earthquake recurrence. Journal of Geophysical Research 95, B3 2609–2624.Google Scholar
Wang, Y., Clark, J.L., (1999). Earthquake damage in Oregon, preliminary estimates of future earthquake losses.. Oregon Department of Geology and Mineral Industries, Special Paper 29, 59 pp.Google Scholar
Wang, Y., He, J., Dragert, H., James, T.S., (2001). Three-dimensional viscoelastic interseismic deformation model for the Cascadia subduction zone. Earth, Planets and Space 53, 295–306.Google Scholar
Weldon, R., Fumal, T., Biasi, G., (2004). Wrightwood and the earthquake cycle: what a long recurrence record tells us about how faults work. GSA Today 14, 4–10.Google Scholar
Witter, R.C., Kelsey, H.M., Hemphill-Haley, E., (2001). Pacific storms, El Nino and tsunamis: competing mechanisms for sand deposition in a coastal marsh, Euchre Creek, Oregon. Journal of Coastal Research 17, 563–583.Google Scholar
Witter, R.C., Kelsey, H.M., Hemphill-Haley, E., (2003). Great Cascadia earthquakes and tsunamis of the past 6700 years, Coquille River estuary, southern coastal Oregon. Geological Society of America Bulletin 115, 1289–1306.CrossRefGoogle Scholar
Yamaguchi, D.K., Atwater, B.F., Bunker, D.E., Benson, B.E., Reid, M., (1997). Tree-ring dating the 1700 Cascadia earthquake. Nature 389, 922–923.CrossRefGoogle Scholar
Yeats, R.S., (1998). Living with Earthquakes in the Pacific Northwest. Oregon State Univ. Press, Corvallis,OR.309 pp.Google Scholar