ASSESSING TECTONIC STRAIN AT COYOTE DAM DUE TO ACTIVE CREEP ALONG THE CALAVERAS FAULT, SANTA CLARA COUNTY, CALIFORNIA
In the vicinity of Coyote Dam the predominantly right-lateral Calaveras fault system is marked by a 6-km long elongate structural basin probably formed by down-dropping of a block along a releasing bend, or pull-apart structure. The dam straddles the northernmost end of the pull-apart basin. Here, the active Calaveras fault trace marks the northwestern boundary of the pull-apart basin and a fault known as the Right Abutment fault marks the northeastern boundary.
We evaluated crest monument survey data for the period 1936 to 2004 to determine a timeline for the propagation of fault creep displacement from the embankment foundation to the dam crest. Deformation of the embankment due to right-lateral creep on the Calaveras fault falls into three general periods. From 1936 to ~1954 there is general absence of right lateral deformation between crest monuments. From ~1954 to ~1980 there is a relatively low rate (~4 mm/yr) of right-lateral separation of monuments, indicating that fault displacement had begun propagation upward through the embankment. Since ~1980, the creep rate of lateral separation of the monuments has increased to ~14-16 mm/yr, which is similar to the range at other locations along this segment of the fault. We conclude that fault-induced deformation of the dam core has fully developed and took ~44 years to propagate through ~18 vertical meters of embankment.