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Hydrologic changes associated with the October 28, 1983, Idaho earthquake

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Abstract

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.

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References

  • Crosthwaite, E. G., Thomas, C. A., andDyer, K. L. (1970),Water Resources of the Big Lost River Basin, South-Central Idaho, U.S. Geol. Survey Open-File Report, 109 pp.

  • Moreland, J. A. (1984), U.S. Geol. Survey, written communication.

  • Rovetto, R. (1984), Clayton Silver Mine, oral communication.

  • Swensen, F. A. (1964),Ground-Water Phenomena Associated With the Hebgen Lake Earthquake. InThe Hegben Lake, Montana, Earthquake of August 17, 1959, U.S. Geol. Survey Profess. Paper 435, 159–165.

  • Wood, S. H. (1984), Boise State Univ., written communication.

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Whitehead, R.L., Harper, R.W. & Sisco, H.G. Hydrologic changes associated with the October 28, 1983, Idaho earthquake. PAGEOPH 122, 280–293 (1984). https://doi.org/10.1007/BF00874599

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  • DOI: https://doi.org/10.1007/BF00874599

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