The Delaware Piedmont is underlain by metamorphosed sedimentary and igneous rocks of Middle Proterozoic to Paleozoic age. The rocks have been studied for many years, but because of poor exposure, high-grade metamorphism, and intense deformation, it has been difficult to identify units, understand their stratigraphic relationships to one another, and determine their origin and history; however, northern Delaware occupies a critical position in the central Appalachian Piedmont, and understanding its geology is key to understanding the geology of this region.
Please give proper credit to the Delaware Geological Survey.
Schenck, W.S. and Plank, M.O. , 1995, Data Report on Rock Cores from Red Mill Road, Harmony Road, Prices Corner, and Newport, Delaware: Delaware Geological Survey Open File Report R3,
Delaware Geological Survey
University of Delaware
Delaware Geological Survey Building
Newark, DE 19716
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