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
- ^ a b 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". Archived from the original on 2014-07-31. Retrieved 22 June 2014.
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