Hayward fault deformation: Migration of Hamilton Creek
The figure above illustrates the
Hamilton Creek. Creep along the
Hayward fault resulted in the
"migration" of the stream. In the
Figure you can see the almost 90
degrees change in the course of
the stream.

Photos and information
presented in this page was
collected during a field trip with
Professor Douglas Dreger, of the
Berkeley Seismological
Laboratory, University of
California at Berkeley.
                               Related links:

Hayward fault deformation: Berkeley Memorial Stadium damage

Hayward fault deformation: Migration of Hamilton Creek

Structures on top of the Hayward fault trace

Road deformation due to Hayward fault creep
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