Stadium Conglomerate

The Stadium Conglomerate is a geologic formation in San Diego County, California.[1][2] It is found at the northern end of Mission Valley near San Diego Stadium.

Stadium Conglomerate
Stratigraphic range: Eocene
TypeGeologic formation
UnderliesMission Valley Formation
OverliesFriars Formation
Lithology
PrimaryConglomerate
Location
RegionSan Diego County, California
Country United States
Type section
Named forSan Diego Stadium

Geology

The formation consists of a massive cobble conglomerate with a dark yellowish-brown coarse-grained sandstone matrix.[1] The conglomerate has dispersed lenses of fossiliferous crossbedded sandstone.[1]

It overlies the Friars Formation, and underlies the sandstone Mission Valley Formation.[1]

Fossil content

It preserves fossils dating back to the Eocene epoch of the Paleogene period, during the Cenozoic Era.[3] The fossils include calcareous nanoplankton.[1]

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gollark: Why ever not?
gollark: Labels work out as about 30 bytes per tick with efficient base 187 encoding.
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gollark: <@509348730156220427> I have some useless ideas I can't be bothered to make:- mesh networking- communication between adjacent computers by changing and reading labels very fast

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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