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Tick Canyon Formation
Geologic formation in California, United States From Wikipedia, the free encyclopedia
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The Tick Canyon Formation (Tt) or Tick Canyon strata, is an Early Miocene geologic formation in the Sierra Pelona Ridge of the San Gabriel Mountains in Los Angeles County, California.[2]
The Tick Canyon Basin drains into the Santa Clara River.[3]
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Geology
The formation overlies the Oligocene to Lower Miocene Vasquez Formation, and underlies the Upper Miocene Mint Canyon Formation.[2][4]
The Tick Canyon strata was deposited on land mostly by streams and consists of green sandstones, coarse-grained conglomerates, and red claystones.[2][4][5] The Tick Canyon strata also contain abundant volcanic clasts, most of which resemble volcanic rocks of the Vasquez Formation.[6] It has an average thickness of 600 feet (180 m).[4]
North of the Tick Canyon Fault, the beds are almost vertical.[2]
Fossil content
It preserves vertebrate fossils of the Lower Miocene subperiod of the Miocene epoch, in the Neogene Period of the Cenozoic Era.[2][7]
Mammals
- Artiodactyls
- Miolabis californicus[8][9]
- Merychyus calaminthus[10]
- M. minimus[11]
- Perissodactyls
- Rodents
Birds
- Falconiformes
- Miohierax stocki[14]
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See also
References
Further reading
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