The rocks at Salt Point represent 40-60 million year old submarine landslide deposits (turbidites) that are exceptionally well exposed and very accessible.
The San Andreas fault also crosses through the park juxtaposing rock units with very different origins.
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The tours identify the rocks, environments they represent, and how geologists interpret the geologic history.
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Many of the photographs document creep features and changes over 30 years.
GEOLOGY OF SALT POINT STATE PARK Salt Point, located on the north coast of California, has a spectacular rugged shoreline, sea cliffs, and uplifted marine terraces.
It is visible at the surface and is easily identified due to the fault slowly creeping and deforming structures built over it.
This tour follows the Hayward fault from Fremont to San Pablo Bay and shows you what to look for to identify the fault.