The Senoia Formation of the Atlanta Group, here named in the Newnan-Tucker synform near Atlanta, GA, consists of garnet-biotite-muscovite schist interlayered with fine-grained hornblende-plagioclase amphibolite. Its lower contact has not been mapped. It sharply and conformably underlies the Wahoo Creek Formation. It is correlative with most of the Clairmont Formation. Age is Late Proterozoic and (or) early Paleozoic.
Source: GNU records (USGS DDS-6; Reston GNULEX).
The Senoia Formation of the Atlanta Group, here abandoned, is revised as the Senoia Member of the Zebulon Formation. It is a thin, <1 m thick interval of gondite (Spessartine quartzite) and magnetite-bearing gondite beds in the upper part of the Zebulon Formation, and it has been mapped with the Zebulon in many areas of the Zebulon thrust sheet in Georgia and Alabama. Age is Late Proterozoic to Early Ordovician(?).
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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