Article · Wikipedia archive · Last revised Jun 1, 2026

Choptank Formation

The Choptank Formation is a geologic formation in Virginia and Maryland. It preserves fossils dating from the mid-late Miocene of the Neogene period, from the latest Langhian to the early Tortonian.

Last revised
Jun 1, 2026
Read time
≈ 2 min
Length
361 w
Citations
5
Source
Choptank Formation
Stratigraphic range:
Chesapecten nefrens, Choptank Formation
TypeFormation
Unit ofChesapeake Group
UnderliesSt. Marys Formation
OverliesCalvert Formation
Location
RegionVirginia, Maryland
CountryUnited States
Type section
Named forChoptank River

The Choptank Formation is a geologic formation in Virginia and Maryland. It preserves fossils dating from the mid-late Miocene of the Neogene period, from the latest Langhian to the early Tortonian (13.9 to 11 million years ago).1

Fossils

The Choptank Formation is extremely fossiliferous. Some of the fossil species represented include the following:23

Sharks

Rays and Other Cartilaginous Fish

Fish

Cetaceans

Pinnipeds

Crocodilians

Invertebrates

4

Terrestrial Mammals

See also

See also

References

References

  1. Carnevale, Giorgio; Godfrey, Stephen James (2018). "Miocene bony fishes from the Calvert, Choptank, St. Marys and Eastover Formations, Chesapeake Group, Maryland and Virginia". Smithsonian Contributions to Paleobiology (100).
  2. Godfrey, Stephen J., ed. (2018-09-25). "The Geology and Vertebrate Paleontology of Calvert Cliffs, Maryland, USA". Smithsonian Contributions to Paleobiology (100): 2–274. doi:10.5479/si.1943-6688.100. ISSN 1943-6688.
  3. "Paleobiology Collections Search". collections.nmnh.si.edu. Retrieved 2020-08-14.
  4. "Collections". The Fossil Forum. Retrieved 2020-08-14.
  5. Eshelman, R. E.; Lambert, W. D.; Morgan, G. S.; Godfrey, S. J.; Bohaska, D. J. (2026). "Review of the Miocene Gomphotheriidae (Mammalia: Proboscidea) from the Chesapeake Group, Middle Atlantic Coastal Plain of North America". Smithsonian Contributions to Paleobiology. 109: 5–72. doi:10.5479/si.32085168.