Valley and Ridge.

The gently rolling countryside of the Valley and Ridge Province

Geology of the Valley and Ridge

True to its name, the Valley and Ridge physiographic province consists of a series of parallel ridges and valleys.

The ridges are made of rocks that are more resistant to erosion than those of the valleys. Therefore, the ridges remained as high points on the landscape, while the valleys were eroded into gently sloping lows.

The origin of the rocks in the Valley and Ridge province is traced back to the Paleozoic Era (~540-250 million years ago) and is tied to the continental collisions that took place during the buildup of the Appalachian Mountains a short distance east.

Valley and Ridge rocks record marine and near shore environments when ocean level was higher and a warm shallow sea covered the area. These environments teemed with life, now registered as fossils throughout the province. Carbonates, composed mostly of the shells of microscopic photosynthetic organisms, were deposited during these intervals of high biologic productivity.

During the Taconic and Acadian Orogenies, sediments were shed over the Valley and Ridge from the highlands rising to the east. These are the land–derived sedimentary rocks.

Each type of sediment, whether it was land–derived or carbonate, forms a layer in the Valley and Ridge. These layers are stacked on top of one another, and were later folded and faulted into their characteristic valleys and ridges when Africa crashed into North America between 325 and 265 million years ago during the final period of Appalachian mountain-building.

The modern landscape is a result of erosion of the province’s folded and faulted sedimentary rocks, leaving behind the resistant rocks (sandstones) as ridges and the more easily eroded rocks (carbonates) as valleys. Crumpled rocks of the Valley and Ridge are exposed along the western reaches of Chesapeake and Ohio National Historical Park.

Antietam National Battlefield

The rolling valleys of the Valley and Ridge province can be seen in this view from the observation tower at Antietam National Battlefield.




Springs and Sinkholes

Springs and sinkholes are common features in the carbonate rocks of the Valley and Ridge. Rainwater dissolves the rock, and small fractures can eventually become enlarged voids. The Mumma Farm Springhouse (Antietam National Battlefield) supports a spring that emerges through carbonate bedrock.


RELATED STORIES
Karst Resource Management at Antietam National Battlefield (pdf)
Geology Fieldnotes for Antietam National Battlefield (NPS)

LEARN MORE
Geologic Time Scale (USGS)
Geologic Glossary (USGS/NPS)
Geologic Map of the National Parks in the National Capital Region
Geologic Map of C & O Canal National Historical Park
NPS Resource Reports for Parks

 

 
   

Contact:


National Park Service
Center for Urban Ecology
4598 MacArthur Blvd NW
Washington, DC 20007

(202) 342-1443