Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; October 1994; v. 84; no. 5; p. 1523-1532
© 1994 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Weichert, D.
Right arrow Articles by Evans, S. G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Seismic signatures of landslides: The 1990 Brenda Mine collapse and the 1965 hope rockslides

Dieter Weichert, Robert B. Horner and Stephen G. Evans

Geological Survey of Canada Pacific Geoscience Centre Sidney, British Columbia, V8L 4B2 Canada
Geological Survey of Canada Terrain Sciences Division, Ottawa, K1A 0E8 Canada

Abstract

We present the well-documented case of a 2 · 106 m3 rockslide that was recorded by seismographs to distances of several hundred kilometers and might have entered the Canadian catalog as a bona fide earthquake except for independent knowledge to the contrary. Motivated by the observation of this event, we reexamined the seismograms associated with the 1965 Hope slide in British Columbia, the largest known historical landslide in the Canadian Cordillera, and conclude that these seismograms were the signatures of two rockslides, and not of hypothetical tectonic earthquake triggers as previously suggested (Mathews and McTaggart, 1969; Wetmiller and Evans, 1989). These events raise the general question of differentiation between seismic signals from landslides and true earthquakes. We suggest an LP/SP discriminant as the most obvious, although a resolvable mechanism solution may be even more convincing. Efficiency of energy conversion from potential to seismic is also a diagnostic aid and correlates well with the slope of the slide detachment surface.




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
J. Deparis, D. Jongmans, F. Cotton, L. Baillet, F. Thouvenot, and D. Hantz
Analysis of Rock-Fall and Rock-Fall Avalanche Seismograms in the French Alps
Bulletin of the Seismological Society of America, August 1, 2008; 98(4): 1781 - 1796.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1994 by the Seismological Society of America.