Freedonia, Chambers Co., Alabama, USA
Latitude & Longitude (WGS84): | 32° 59' 22'' North , 85° 17' 17'' West |
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Latitude & Longitude (decimal): | 32.98957,-85.28809 |
Köppen climate type: | Cfa : Humid subtropical climate |
3.5 km SE of town
Mineral List
2 valid minerals.
Regional Geology
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
Paleozoic - Precambrian 252.17 - 4000 Ma ID: 3008502 | Dadeville Complex; Rock Mills Granite Gneiss Age: Eoarchean to Permian (252.17 - 4000 Ma) Stratigraphic Name: Rock Mills Granite Gneiss Description: Coarse to medium-grained biotite granite gneiss; locally includes thick bands of epidote and thin, small amphibolite bodies. Boundary between Rock Mills Granite Gneiss and Camp Hill Granite Gneiss arbitrarily defined. Lithology: Major:{biotite gneiss}, Minor:{amphibolite} Reference: Horton, J.D., C.A. San Juan, and D.B. Stoeser. The State Geologic Map Compilation (SGMC) geodatabase of the conterminous United States. doi: 10.3133/ds1052. U.S. Geological Survey Data Series 1052. [133] |
Paleozoic - Neoproterozoic 252.17 - 1000 Ma ID: 3190741 | Precambrian-Phanerozoic crystalline metamorphic rocks Age: Neoproterozoic to Permian (252.17 - 1000 Ma) Comments: Piedmont Lithology: Felsic paragneiss; amphibolite grade paragneiss/metavolcanic gneiss Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154] |
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