OBSERVATIONS OF THE SEQUATCHIE FAULT AND GEOLOGIC MAPPING IN NORTHEASTERN ALABAMA
In the Mt. Carmel quadrangle, the trace of the fault extends from the eastern boundary southwestward and cuts down section in both the hanging wall and footwall from Mississippian rocks into the Upper Ordovician south of Roden Ridge. The trace of the fault continues within the Middle Ordovician Nashville and Stones River Groups and becomes a blind thrust further southwest. To the northeast, the Mississippian Monteagle Limestone is in the footwall of the fault. Continuing southwestward, the fault cuts down section in the footwall to the Nashville and Stones River Groups at the terminus of the surface fault trace. In the hanging wall, the Mississippian Tuscumbia Limestone, Fort Payne Chert, and Maury Formation undifferentiated is juxtaposed against the Mississippian Monteagle Limestone from the eastern edge of the quadrangle to a small inlet of Guntersville Lake, beyond which rocks in the hanging wall become progressively older, ending in the Nashville and Stones River Groups at the terminus of the mapped fault in the quadrangle. The exact location at which the Sequatchie fault becomes blind is unknown.