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Seismic events have long been known to cause changes in the level of oceans, streams, lakes, and the water table. The great San Francisco earthquake of 1906 induced significant hydrologic changes that were qualitatively similar to those changes observed for the Loma Prieta earthquake. What is different is that the hydrologic data sets collected from the Loma Prieta event have enough detail to enable hypotheses on the causes for these changes to be tested. The papers in this chapter document changes in ocean level, stream morphology and flow, water table height, and ground-water flow rates in response to the earthquake. Although hydrologic disturbances may have occurred about 1 hour before the main shock, the papers in this chapter deal strictly with postevent hydrologic changes. The hydrologic responses reported here reflect changes that are not the result of surface rupture. They appear to be the result of landslides, the static displacements induced by the earthquake, and changes in the permeability of the near surface. |
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This publication is part of the set of four multi-chapter USGS Professional Papers on the Loma Prieta, California, Earthquake of October 17, 1989: Professional Paper 1550, Earthquake Occurrence , Coordinators: William H. Bakun and William H. Prescott Professional Paper 1551, Strong Ground Motion and Ground Failure, Coordinator: Thomas L. Holzer Professional Paper 1552, Performance of the Built Environment, Coordinator, Thomas L. Holzer Professional Paper 1553, Societal Response, Coordinator: Dennis S. Mileti |
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URL of this page: https://pubs.usgs.gov/pp/pp1551/pp1551e/
Maintained by: Michael Diggles
Created: July 13, 2006
Last modified: July 20, 2006 (mfd)