Punchbowl Formation

Punchbowl Formation
Stratigraphic range: Neogene
Type Formation
Location
Region San Gabriel Mountains,
Los Angeles County, California
Country United States

The Punchbowl Formation is a sedimentary sandstone geologic formation in the northern San Gabriel Mountains, above the Antelope Valley in Los Angeles County, southern California.[1][2]

Geology

The Devil's Punchbowl, in the San Gabriel Mountains.

The formations sandstone strata are seen in the walls of the Devil's Punchbowl, a scenic gorge within the Devil's Punchbowl Natural Area, an L.A. County park within the Angeles National Forest. has folded and uplifted the formation in view.[1] The Devil's Punchbowl is a large plunging sandstone syncline, where the edges of the formation have been folded upward, and the center has dipped. It was formed by the Punchbowl Fault, which is near the San Andreas Fault to the north.

The uplifted formation preserves fossils dating back to the Neogene period of the Cenozoic geologic era, formed during the lower Pliocene to upper Miocene Ages (~5-10 million years ago).[1][3]

The Devil's Punchbowl drainage flows into Sandrock Creek, a tributary of Big Rock Creek, which disappears into the Mojave Desert.[1]

See also

References

  1. 1 2 3 4 UCB−Seismo.berkeley.edu: Field Guide to the Punchbowl Fault Zone at the Devil's Punchbowl Natural Area . accessed 7.7.2015
  2. ↑ Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 8 July 2014.
  3. ↑ L.A. County: "Geological History", with images.
Wikimedia Commons has media related to Devil's Punchbowl (California).
Quaternary
Pleistocene Holocene
Early | Middle | Late Preboreal | Boreal |
Atlantic | Subboreal | Subatlantic


This article is issued from Wikipedia - version of the 3/24/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.