Temblor Formation

Geologic formation in California From Wikipedia, the free encyclopedia

The Temblor Formation is a geologic formation in California. It preserves fossils dating back from the Late Oligocene to the Middle Miocene of the Neogene period. It is notable for the famous Sharktooth Hill deposit (otherwise known as Ernst Quarry).[1][2][3]

Sub-unitsAgua Sandstone Member, Buttonbed Sandstone Member, Carneros Sandstone Member, Cymric Shale Member, Devilwater Siltstone, Gould Shale, Media Shale Member, Round Mountain Silt, Santos Shale Member, Wygal Sandstone Member
Quick facts Type, Sub-units ...
Temblor Formation
Stratigraphic range: Late Oligocene-Mid Miocene
~28–11.6 Ma
TypeGeologic formation
Sub-unitsAgua Sandstone Member, Buttonbed Sandstone Member, Carneros Sandstone Member, Cymric Shale Member, Devilwater Siltstone, Gould Shale, Media Shale Member, Round Mountain Silt, Santos Shale Member, Wygal Sandstone Member
UnderliesMonterey Formation
Lithology
PrimaryShale, sandstone
Location
RegionWestern San Joaquin Valley,
Kern County, California
CountryUnited States
Type section
Named forTemblor Ranch, McKittrick district, Kern County
Named byAnderson
Year defined1905
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Fossils

Vertebrates

Cartilagenous fishes

Sharks
Isurus planus upper teeth from the Sharktooth Hill bonebed
Rays and skates

Reptiles

Birds

Artist's rendering of Hypohippus in its natural habitat
Restoration of Paleoparodoxia

Mammals

See also

References

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