Talbot Formation

From Wikipedia, the free encyclopedia
Talbot Formation
Stratigraphic range: Neogene
Minor faulting of interbedded clay and sand of Talbot Formation on Morgan Creek
TypeFormation
Location
Region Maryland
Country United States
Type section
Named forTalbot County, Maryland
Named byG. B. Shattuck (1901)[1]

The Talbot Formation is a geologic formation in Maryland. It preserves fossils dating back to the Neogene period.

The term is no longer formally recognized but occurs in geologic literature.[2] The term is retained as a geomorphic feature, the Talbot terrace.

See also[edit]

References[edit]

  1. ^ Shattuck, G.B., 1901, The Pleistocene problem of the north Atlantic Coastal Plain: Johns Hopkins University Circular, v. 20, no. 152, p. 69-75.
  2. ^ National Geologic Map Database, Geolex — Unit Summary, Talbot
  • Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.