Pinnacles National Park occupies the southern reaches of this landscape, where the distinct volcanic spires of the Pinnacles rise above the high desert floor. The area is defined by the massive tectonic forces of the San Andreas Fault, which cuts through the central valley and separates the Gabilan Range from the Diablo Range. This geological rift dictates the drainage patterns of the San Benito River and its various tributaries, including Willow Creek and North Fork Chalone Creek.
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1915 · Soledad
USGS Topo · 1:62,500
1919 · San Benito
USGS Topo · 1:62,500
1921 · Gonzales
USGS Topo · 1:62,500
1921 · Metz
USGS Topo · 1:62,500
1931 · San Benito
USGS Topo · 1:62,500
1940 · Metz
USGS Topo · 1:62,500
1940 · Soledad
USGS Topo · 1:62,500
1940 · San Benito
USGS Topo · 1:62,500
1940 · Gonzales
USGS Topo · 1:62,500
1941 · Gonzales
USGS Topo · 1:62,500