When the Mountain Dwarfs Danced: Aboriginal Traditions of Paleoseismic Events along the Cascadia Subduction Zone of Western North America
Authors:
- Alan D. McMillanAMAlan D. McMillan
- Ian HutchinsonIHIan Hutchinson
- 1 January 2002
- journal article
- Published by Duke University Press in Ethnohistory
- Vol. 49 (1) , 41-68
Abstract
Geological evidence demonstrates that recurrent great earthquakes have been generated at the Cascadia subduction zone, off the west coast of North America, throughout the Holocene. Such major earthquakes and associated tsunamis would have had devastating impacts on Native villages along this coastline. Native oral traditions of such disasters, along with earthquake figures in myth and ceremony, are examined for evidence of the nature of such past geological events and the impact they had on human populations.Keywords
This publication has 34 references indexed in Scilit:
- Evidence for large earthquakes at the Cascadia Subduction ZoneReviews of Geophysics, 1997
- Tree-ring evidence for an A.D. 1700 Cascadia earthquake in Washington and northern OregonGeology, 1997
- Earthquake-Induced Subsidence and Burial of Late Holocene Archaeological Sites, Northern Oregon CoastAmerican Antiquity, 1996
- Time and size of a giant earthquake in Cascadia inferred from Japanese tsunami records of January 1700Nature, 1996
- Giant Earthquakes of the Pacific NorthwestScientific American, 1995
- Holocene debris flows and environmental history, Hazelton area, British ColumbiaCanadian Journal of Earth Sciences, 1991
- The Rubble Creek landslide, southwestern British ColumbiaCanadian Journal of Earth Sciences, 1978
- THE COAST SALISH OF PUGET SOUND1American Anthropologist, 1941
- TOLOWA NOTESAmerican Anthropologist, 1932
- THE CEREMONIAL SOCIETIES OF THE QUILEUTE INDIANS1American Anthropologist, 1921