Coffee Mill Hammock Formation

The Coffee Mill Hammock Formation is a geologic formation in Florida. The formation is about two-feet thick and is composed of shell marl. It sits on top of the Fort Thompson Formation and preserves fossils from the Late Pleistocene,[1] predominantly Chione cancellata. It can be seen at Goodno's Landing, Fort Thompson, and at Coffee Mill Hammock, 12 north of LaBelle, Florida, in Glades County.[2]

Coffee Mill Hammock Formation
TypeFormation
Location
RegionFlorida
CountryUnited States

See also

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References

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  1. ^ "Neogene Geology of the Southeastern United States".
  2. ^ "Geologic Unit: Coffee Mill Hammock". National Geologic Map Database. United States Geological Survey. Retrieved 2 March 2017.