Pomerado Conglomerate

The Pomerado Conglomerate Formation is a geologic formation in southwestern San Diego County, California.[1][2]

Pomerado Conglomerate Formation
Stratigraphic range: Late Eocene
Typegeologic formation
OverliesMission Valley Formation
Thickness0–55 metres (0–180 ft)
Lithology
Primaryconglomerate
Location
RegionSan Diego County, California
CountryUnited States
Type section
Named forPomerado Road

It was named for exposures located along Pomerado Road, at the divide between Carroll Canyon and Poway Valley.[1]

Geology

The Pomerado Conglomerate is of the Late Eocene Epoch, and is a massive cobble conglomerate. It is lithologically identical to the local Stadium Conglomerate.[1]

It overlies the sandstone Mission Valley Formation.[1] It is the uppermost formation of the Poway Group, and has a maximum thickness of 55 metres (180 ft).[1]

Fossils

It preserves fossils dating back to the Late Eocene Epoch of the Paleogene period, during the Cenozoic Era.[3]

See also

References

  1. Kennedy, Michael P. (1975). Geology of the San Diego metropolitan area, California. California Division of Mines and Geology.
  2. Geiconsultants.com: Geologic Formations of Western San Diego County, by Jeffrey D. Brown, R.G., C.E.G. − circa 1996.
  3. Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Archived from the original on 31 July 2014. Retrieved 8 July 2014.

Further reading


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