Hydrologic changes associated with the October 28, 1983, Idaho earthquake
Significant hydrologic changes were observed after the magnitude 7.3 earthquake that occurred on October 28, 1983, in central Idaho. Groundwater levels rose by as much as 3 meters near the epicenter. Discharge in many streams and springs increased, in some instances by more than 100%. One warm spring ceased flowing for several days; the flow then resumed and peaked at about nine times its original rate. Available data show no significant changes in water quality following the earthquake. ?? 1985 Birkha??user Verlag.
Citation Information
Publication Year | 1985 |
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Title | Hydrologic changes associated with the October 28, 1983, Idaho earthquake |
DOI | 10.1007/BF00874599 |
Authors | R.L. Whitehead, R.W. Harper, H.G. Sisco |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Pure and Applied Geophysics PAGEOPH |
Index ID | 70013359 |
Record Source | USGS Publications Warehouse |