Tick Canyon Formation

Tick Canyon Formation
Stratigraphic range: Lower Miocene
Type Geologic formation
Underlies Mint Canyon Formation
Overlies Vasquez Formation
Thickness 0–1,000 feet (0–305 m) (average)
Location
Region Sierra Pelona Mountains, Los Angeles County, California
Country United States
Type section
Named for Tick Canyon

The Tick Canyon Formation is a Miocene epoch geologic formation in the Sierra Pelona Mountains of Los Angeles County, California. [1]

The Tick Canyon Basin drains into the Santa Clara River.[2]

Geology

The formation was deposited on land mostly by streams and consists of green sandstone, coarse-grained conglomerates, and red claystone.[1][3][4] It has an average thickness of 600 feet (180 m).[3]

The formation overlies the Oligocene Period Vasquez Formation, and underlies the Upper Miocene Mint Canyon Formation.[1][3]

North of the Tick Canyon fault, the beds are almost vertical.[1]

Fossils

It preserves vertebrate fossils of the Lower Miocene subperiod of the Miocene epoch, in the Neogene Period of the Cenozoic Era.[1][5]

See also

References

  1. 1 2 3 4 5 Elsmerecanyon.com: "Tick Canyon Geology"
  2. "Geologic Map of the Mint Canyon Quadrangle" (DF-57) by Thomas W. Dibblee, Jr., 1996.
  3. 1 2 3 Caltech.edu: THESIS - "Geology of the Upper Tick Canyon area, California"; Birman, Joseph Harold; 1950.
  4. Caltech.edu: THESIS - "Geology of the Mint Canyon area, Los Angeles County, California"; Holser, William T.; 1946.
  5. Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 8 July 2014.
Neogene Period
Miocene Pliocene
Aquitanian | Burdigalian
Langhian | Serravallian
Tortonian | Messinian
Zanclean | Piacenzian


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