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Saprolite
Fall Zone
The Fall Zone delineates the boundary between the Coastal Plain and the Piedmont. Here rivers draining the Piedmont drop steeply to sea level and in the process form dramatic rapids.

James River profile (red line) from the Piedmont, west of Richmond, through the Fall Zone to the Coastal Plain. Notice the dramatic change in gradient from 1-2’ per mile above the Fall Zone to 14’ per mile in the Fall Zone. The vertical steps in the Piedmont are due to dams along the river, the blue dashed line traces the original pre-dam profile.
The Neoproterozoic Lynchburg Group
The Neoproterozoic Lynchburg Group is a thick sequence of metasedimentary rocks exposed in the eastern Blue Ridge from northern to south-central Virginia. These deposits range from coarse-grained conglomerate to fine-grained mudstone.

Boulder conglomerate in the Rockfish Conglomerate at the base of the Neoproterozoic Lynchburg Group in Nelson County. Click here to learn more about the Rockfish Conglomerate.










