Author Archives: cmbail
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.
Siluro-Devonian cross bedded carbonate strata
Twenty years of change at Cedar Island
Cedar Island is one of Virginia’s barrier islands that separates the Eastern Shore from the Atlantic Ocean. Barrier islands are dynamic environments that respond quickly to environmental changes. Over time barrier islands move, and their shorelines migrate. During the past two decades shoreline change at the south end of Cedar Island has been dramatic. Compare the 1994 aerial imagery to the 2014 aerial imagery (below). Cedar Island’s southern tip has eroded northward by more than a kilometer, and the shoreline has retreated ~400 meters to the west. Wachapreague Inlet has gotten larger, and Parramore Island’s northern edge has been relatively stable.
Geoscientists have long known that Cedar Island is a particularly mobile barrier island. Yet, Cedar Island is privately owned, and in 1990 dozens of houses were permitted (by the Virginia Marine Resource Commission) to be built on the barrier island. Another example of scientific evidence being tossed aside by policy makers. By 1997 27 homes had been constructed facing the Atlantic Ocean. In 2014 the last houses on Cedar Island had succumb to the shifting sand and moving island. A legal quagmire continues as property owners are still taxed (albeit at a low rate) over lots that are now fully submerged beneath the Atlantic waves.

Coastal erosion at Cedar Island, Virginia. U.S. Geological Survey photo













