Belgrade Formation

Belgrade Formation
Stratigraphic range: Miocene
Type Formation
Sub-units Pollocksville Member, Haywood Landing Member
Lithology
Primary limestone sand
Other clay
Location
Region  North Carolina
Country  United States
Type section
Named for Belgrade, North Carolina

The Belgrade Formation is a limestone geologic formation in North Carolina characterized by limestone coquina mixed with sand, and thinly laminated clays[1]. It preserves fossils dating back to the Paleogene period.

Description

The Belgrade Formation is composed of two subunits: the Pollocksville Member and the Haywood Landing member. The Pollocksville member is composed of unconsolidated oyster shells and sand. It was deposited in the early Miocene. The Haywood Landing member is composed of shelly sands and thinly laminated clays. The Belgrade Formation was originally considered part of an Eocene formation called the Trent Marl before it was identified as being deposited in the Miocene and split off. [1]

See also

References

  1. 1 2 Ward, Lauck W.; Lawrence, David R.; Blackwelder, Blake W. (1979). "Stratigraphic revision of the middle Eocene, Oligocene, and lower Miocene; Atlantic Coastal Plain of North Carolina" (PDF). U.S. Geological Survey Bulletion. 1457-F: 3–10. Retrieved 26 June 2018.
  • Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 22 June 2014.


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