Earth:Stadium Conglomerate
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Short description: Geologic formation in California, US
Stadium Conglomerate Stratigraphic range: Eocene | |
---|---|
Type | Geologic formation |
Underlies | Mission Valley Formation |
Overlies | Friars Formation |
Lithology | |
Primary | Conglomerate |
Location | |
Region | San Diego County, California |
Country | United States |
Type section | |
Named for | San Diego Stadium |
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.
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]
See also
- Geology of San Diego County, California
- Paleogene Period in California
- List of fossiliferous stratigraphic units in California
- Paleontology in California
References
- ↑ 1.0 1.1 1.2 1.3 1.4 Kennedy, Michael P. (1975). Geology of the San Diego metropolitan area, California. California Division of Mines and Geology. https://archive.org/details/geologyofsandieg00kennrich.
- ↑ Geiconsultants.com: Geologic Formations of Western San Diego County[yes|permanent dead link|dead link}}], by Jeffrey D. Brown, R.G., C.E.G. − circa 1996.
- ↑ ((Various Contributors to the Paleobiology Database)). "Fossilworks: Gateway to the Paleobiology Database". http://www.fossilworks.org/cgi-bin/bridge.pl?action=home.
Further reading
- "General Plan Final Program EIR: 3.11 Paleontological Resources". http://www.sandiego.gov/planning/genplan/pdf/peir/paleontological.pdf.
Original source: https://en.wikipedia.org/wiki/Stadium Conglomerate.
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