Tick Canyon Formation


The Tick Canyon Formation is a Miocene epoch geologic formation in the Sierra Pelona Mountains of Los Angeles County, California.
The Tick Canyon Basin drains into the Santa Clara River.

Geology

The formation was deposited on land mostly by streams and consists of green sandstone, coarse-grained conglomerates, and red claystone. It has an average thickness of.
The formation overlies the Oligocene Period Vasquez Formation, and underlies the Upper Miocene Mint Canyon Formation.
North of the Tick Canyon fault, the beds are almost vertical.

Fossils

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