in
Maryland, winds its way among rolling Piedmont hills in central
Virginia, though most hills in the Piedmont region are smaller than these. The surface relief of the Piedmont is characterized by relatively low, rolling hills with heights above
sea level between 200 feet (50 m) and 800 feet to 1,000 feet (250 m to 300 m). Its
geology is complex, with numerous rock formations of different materials and ages intermingled with one another. Essentially, the Piedmont is the remnant of several ancient
mountain chains that have since been eroded. Geologists have identified at least five separate events which have led to
sediment deposition, including the
Grenville orogeny (the collision of continents that created the
supercontinent Rodinia) and the
Appalachian orogeny during the formation of
Pangaea. The last major event in the history of the Piedmont was the break-up of Pangaea, when
North America and
Africa began to separate. Large
basins formed from the
rifting and were filled by the sediments shed from the surrounding higher ground. The series of
Mesozoic basins is almost entirely located inside the Piedmont region. ==Ecology==