The Piedmont of South Carolina and Georgia is a complex mosaic of exotic terranes of uncertain provenance. Farther south and east, these terranes form the basement beneath several kilometers of Cretaceous and Cenozoic sedimentary rocks, commonly referred to as the Atlantic Coastal Plain. The distribution and geologic history of this hidden crystalline basement can be inferred only on the basis of limited exposures at the margins of the Coastal Plain onlap, aeromagnetic lineaments that define basement trends in the subsurface, and core data from wells that penetrate basement. During the past 40 years, basement cores aggregating more than 6 miles (10,000 m) have been recovered from 57 deep wells at the Department of Energy's Savannah River Site. These cores provide the only known samples of basement terranes that lie southeast of the Fall Line in central South Carolina. Cores from the 57 deep wells, along with structural trends defined by aeromagnetic lineaments, allow us to define four distinct units within the basement beneath the Coastal Plain: (1) the Crackerneck Metavolcanic Complex (greenstones and felsic