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Pomerado Conglomerate

Geologic formation From Wikipedia, the free encyclopedia

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

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

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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]

Fossil content

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Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

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

Mammals

Ferae

More information Ferae reported from the Pomerado Conglomerate, Genus ...

Rodents

More information Rodents reported from the Pomerado Conglomerate, Genus ...


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See also

References

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Further reading

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