Tulare Formation

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Short description: Geologic formation in central California, US
Tulare Formation
Stratigraphic range: Neogene & Quaternary
TypeFormation
Underlies(is topmost formation)
OverliesSan Joaquin Formation
Thicknessup to 4,000 feet (1,200 m)
Location
RegionSan Joaquin Valley, California
CountryUnited States

The Tulare Formation (/tʊˈlɛəri/ (About this soundlisten)) is a Pliocene to Holocene epoch geologic formation in the central and southern San Joaquin Valley of central California .[1][2]

Geology

It overlies the San Joaquin Formation, and can be up to 4,000 feet (1,200 m) thick.[1][2]

Its sediments consist mainly of unconsolidated deposits of clay, silt, sand, and gravel.[1]

Fossils

Many freshwater fossils are preserved in the formation, dating back to the Neogene and Quaternary Periods of the Cenozoic Era.[3] They include the largest fossil assemblage of clams and snails known on the Pacific Coast.[1]

See also

  • Neogene California
  • List of fossiliferous stratigraphic units in California
  • Paleontology in California

References

  1. 1.0 1.1 1.2 1.3 USGS.gov: "Geology of the Tulare Formation and other continental deposits, Kettleman City area, San Joaquin Valley, California, with a section on ground-water management considerations and use of texture maps"; Water-Resources Investigations Report 83-4000; by R.W. Page; 1983.
  2. 2.0 2.1 USGS.gov: "Neogene Gas Total Petroleum System—Neogene Nonassociated Gas Assessment Unit of the San Joaquin Basin Province"; Chapter 22 of the Petroleum Systems and Geologic Assessment of Oil and Gas in the San Joaquin Basin Province, California; by Allegra Hosford Scheirer and Leslie B. Magoon.
  3. ((Various Contributors to the Paleobiology Database)). "Fossilworks: Gateway to the Paleobiology Database". http://www.fossilworks.org/cgi-bin/bridge.pl?action=home. 





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