Dating the 1700 Cascadia Earthquake: Great Coastal Earthquakes in Native Stories

Although scientific recognition of the earthquake hazard presented by the Cascadia subduction zone (CSZ) is relatively recent, native peoples have lived on the Cascadia coast for thousands of years, transferring knowledge from generation to generation through storytelling. This paper considers the ways in which information on coastal earthquakes is presented in native traditions and estimates the date of the most recent event from them. The primary plate-boundary fault of the CSZ separates the oceanic Juan de Fuca Plate from the continental North America Plate (Figure 1). It lies about 80 km offshore and extends roughly parallel to the coast from the middle of Vancouver Island to northern California. Although recognized as early as the mid-1960's, the CSZ was initially assumed to be incapable of producing great megathrust earthquakes. It is seismically quiet, and no sizable earthquake has occurred on it since European settlement began. As the theory of plate tectonics matured, studies of subduction zones worldwide identified characteristics associated with megathrust earthquakes. These earthquakes are most common in areas where hot, young, buoyant crust is rapidly subducted (Heaton and Kanamori, 1984). Although the rate of subduction in Cascadia is relatively slow, the subducted crust is among the youngest and hottest anywhere. Field investigations soon located geological evidence of abrupt land-level changes characteristic of megathrust earthquakes in “ghost forests” of dead cedar trees in coastal estuaries in Washington and Oregon (Nelson et al. , 1995). The cedars, originally above the limit of the tides, were killed when their roots were suddenly plunged into salt water. Beneath the surface of these same estuaries, soil cores revealed layered deposits showing a repeated cycle of slow uplift and rapid submergence. Preliminary age estimates based on radiocarbon dating (Nelson et al. , 1995) and tree-ring studies (Yamaguchi et al. , 1989) suggested that the …

[1]  Kenji Satake,et al.  Fault slip and seismic moment of the 1700 Cascadia earthquake inferred from Japanese tsunami descriptions , 2003 .

[2]  R. B. Inverarity,et al.  Indian Legends of the Pacific Northwest , 1953 .

[3]  Daniel E. Bunker,et al.  Tree-ring dating the 1700 Cascadia earthquake , 1997, Nature.

[4]  J. Stein,et al.  Earthquake-induced burial of archaeological sites along the southern Washington coast about A.D. 1700 , 1996 .

[5]  Brian F. Atwater,et al.  Recurrence Intervals for Great Earthquakes of the Past 3,500 Years at Northeastern Willapa Bay, Washington , 1997 .

[6]  Ian Hutchinson,et al.  When the Mountain Dwarfs Danced: Aboriginal Traditions of Paleoseismic Events along the Cascadia Subduction Zone of Western North America , 2002 .

[7]  E. Arima Between Ports Alberni and Renfrew: Notes on West Coast Peoples , 1991 .

[8]  Claude Lévi-Strauss,et al.  The Way of the Masks , 1984 .

[9]  Thomas H. Heaton,et al.  Seismic potential associated with subduction in the northwestern United States , 1984 .

[10]  J. Clague,et al.  Radiocarbon evidence for extensive plate-boundary rupture about 300 years ago at the Cascadia subduction zone , 1995, Nature.

[11]  T. Heaton,et al.  Possible tsunami along the northwestern coast of the United States inferred from Indian traditions , 1985 .

[12]  C. Pearson,et al.  Nehalem Tillamook Tales , 1960 .

[13]  Wilson Duff The Upper Stalo Indians of the Fraser Valley, British Columbia , 1952 .

[14]  G. R. Newell,et al.  Indian days at Neah Bay , 1961 .

[15]  R. Bucknam,et al.  Abrupt Uplift Within the Past 1700 Years at Southern Puget Sound, Washington , 1992, Science.

[16]  Indians of the Northwest Coast , 1956 .

[17]  Kenji Satake,et al.  Time and size of a giant earthquake in Cascadia inferred from Japanese tsunami records of January 1700 , 1996, Nature.

[18]  I. Hutchinson,et al.  Archaeological Evidence for Village Abandonment Associated with Late Holocene Earthquakes at the Northern Cascadia Subduction Zone , 1997, Quaternary Research.

[19]  Melville Jacobs Coos narrative and ethnologic texts , 1939 .

[20]  J. Lander,et al.  Tsunamis Affecting the West Coast of the United States: 1806-1992 , 1993 .

[21]  P. Heeb,et al.  Mixed blessings for middle-aged mothers , 1997, Nature.

[22]  Takeshi Sagiya,et al.  A revised dislocation model of interseismic deformation of the Cascadia subduction zone , 2003 .

[23]  L. Frachtenberg Alsea texts and myths , 1920 .

[24]  J. Clague Early historical and ethnographical accounts of large earthquakes and tsunamis on western Vancouver Island, British Columbia , 1995 .

[25]  J. Clague,et al.  A review of geological records of large tsunamis at Vancouver Island, British Columbia, and implications for hazard , 2000 .

[26]  R. Minor,et al.  Earthquake-Induced Subsidence and Burial of Late Holocene Archaeological Sites, Northern Oregon Coast , 1996, American Antiquity.