| 词条 | Coffee Mill Hammock Formation |
| 释义 |
| name = Coffee Mill Hammock Formation | image = | caption = | type = Formation | age = | prilithology = | otherlithology = | namedfor = | namedby = | region = {{Flag|Florida}} | country = {{Flag|United States}} | coordinates = | unitof = | subunits = | underlies = | overlies = | thickness = | extent = | area = | map = | map_caption = }} The Coffee Mill Hammock Formation is a geologic formation in Florida. About two-feet thick of shell marl, it sits on top of the Fort Thompson Formation, and it preserves fossils, 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.[1] See also{{Portal|Earth sciences|Florida|Paleontology|}}
References1. ^{{cite web|title=Geologic Unit: Coffee Mill Hammock|url=https://ngmdb.usgs.gov/Geolex/UnitRefs/CoffeeMillHammockRefs_1144.html|website=National Geologic Map Database|publisher=United States Geological Survey|accessdate=2 March 2017}}
1 : Geologic formations of Florida |
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