In the Cumberland Plateaus of southeastern Tennessee, northwestern Georgia, and northeast Alabama, Pennsylvanian strata are siliciclastics containing discontinuous coal seams. Above some of these coal seams, the shale deposits contain fossils of marine or brackish fauna. The entire sequence was deposited in an asymmetric foreland basin and is thickest in the southeast. Within this general trend there are locally thick deposits of lowermost Pennsylvanian Gizzard Group sequences that mark subbasins. Conglomeratic sandstone members of the Gizzard Group are discontinuous and tend to be thicker in the subbasins. In contrast, conglomeratic to sandy units are more laterally continuous in the overlying Crab Orchard Mountains Group. The Pennsylvanian sequence overlies paleosols with subjacent freshwater-neomorphosed shallow marine carbonates, or siliciclastics of the uppermost Mississippian Pennington Formation. A provenance discrimination diagram indicates that Pennsylvanian siliciclastics were derived from an orogenic source. Profile analysis of thick quartzose sandstone sequences indicates facies, architectural elements, and bounding surfaces characteristic of braided stream deposits. A dominant southwest paleoflow direction is inferred from paleocurrent indicators in sandy braided and meandering stream deposits.