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Bulletin of the Seismological Society of America; October 1982; v. 72; no. 5; p. 1591-1599
© 1982 Seismological Society of America
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Tectonics and recent seismicity near Flathead Lake, Montana

ANTHONY QAMAR, JERRY KOGAN and MICHAEL C. STICKNEY

DEPARTMENT OF GEOLOGY UNIVERSITY OF MONTANA, MISSOULA, MONTANA 59812
MONTANA BUREAU OF MINES AND GEOLOGY MONTANA COLLEGE OF MINERAL SCIENCE AND TECHNOLOGY, BUTTE, MONTANA 59701

Abstract

Since 1900, more than 290 earthquakes have been reported near Flathead Lake, Montana. Surprisingly, none has exceeded magnitude 5 to Formula. Most recent earthquake swarms appear to result from east-west or northwest-southeast extension along short fault segments west and north of the lake. Major normal faults like the Swan and Mission faults east of the lake may pose higher risk, but they appear dormant today. Deformation of sediments in Flathead Lake may be caused by several large earthquakes more than 10,000 years ago but is more probably due to glacial processes accompanying the last retreat of the Cordilleran ice sheet.




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