Pinole Tuff Formation Explained

Pinole Tuff Formation
Type:Geologic formation
Age:Neogene
Period:Neogene
Prilithology:Tuff, breccia
Namedfor:Pinole, California
Region:Contra Costa County
California
Country:United States
Underlies:Orinda Formation,
Monterey Formation Group units
Overlies:Neroly Formation
San Pablo Formation
Thickness:270m (890feet)

The Pinole Tuff Formation is a geologic formation of the East Bay region of the San Francisco Bay Area in California.

It is found near Pinole and Rodeo area at San Pablo Bay and the Briones Hills of western Contra Costa County.

FossilsIt preserves fossils, including Oncorhynchus rastrosus[1] and fragments of a proto-hipparion prehistoric horse, dating back to the Neogene period.

See also

References

Notes and References

  1. Cavender. Ted M.. Miller. Robert Rush. Smilodonichthys Rastrosus: A New Pliocene Salmonid Fish from Western United States. Bulletin of the Museum of Natural History. 18. 1972. University of Oregon.