Series: Physiographic Provinces

Appalachian Plateaus Province

Upper Delaware Scenic and Recreational River
Upper Delaware Scenic and Recreational River

NPS photo

The Appalachian Plateaus form the northwestern-most province of the Appalachian Mountains, stretching from New York southwest to Alabama. They are composed of sedimentary rocks including sandstones, conglomerates, and shales deposited during the late Paleozoic. These rocks exist largely as horizontal beds that have been cut by streams to form the mountainous terrain that is distinctive today. Mountain ranges existing in the Appalachian Plateaus include the Catskill, Pocono, Allegheny, and Cumberland Mountains.

In addition to these sedimentary rocks, beds of coal are locally significant throughout the Appalachian Plateaus, making this area the heart of the American coal industry. Much of this mining has been done underground in the past, but new technology allows entire areas of surface to be removed, exposing the coal beneath. The first oil well in America was drilled in Bradford, Pennsylvania and extraction of high-quality oil and natural gas continues in the Appalachian Plateaus, although the quantity is dwarfed by the amounts produced in Texas and Louisiana (in the coastal plains province).

The Appalachian Mountains as a whole have a long geologic history. In the early Paleozoic, the North American craton (what would eventually become North America) was located near the equator, and the eastern margin was often submerged beneath a shallow sea depositing carbonate and other sedimentary rocks. In the mid-Paleozoic, the supercontinent Pangea began to assemble as the oceanic Iapetus plate slid underneath the eastern edge of the thick North American craton pulling with it islands, and eventually the continent Gondwana (Africa), to collide with North America. This folded and lifted the sedimentary rocks, creating the beginning of the Appalachian Mountains. As the mountains rose, streams cut through them eroding and carrying sediments to be deposited in the neighboring lowlands. These sediments became the rocks that make up the Appalachian Plateaus. Throughout the Mesozoic, as the supercontinent Pangea broke up and drifted apart, the Appalachian Mountains (then at a height similar to today’s Himalayas) slowly eroded. 

The final step in building the Appalachian Plateaus as we know them occurred with uplift in the Cenozoic. This reinvigorated the streams which cut through the sedimentary rocks to create the mountainous topography we see today. Some of these incisions are truly dramatic, including the New River Gorge slicing up to 335 m (1,100 ft) through the Pottsville sandstone in West Virginia.

In the recent geologic past, the northern portion of the Appalachian Plateaus has been subject to the effects of glaciation, resulting in some distinctive landforms. Most notable of these is the Finger Lakes in New York. Their long, slender shape is the result of pre-glacial valleys that were blocked by glacial debris and filled in with water. The largest of these are Lakes Seneca and Cayuga. 

Map of Appalachian Plateaus

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Educational Resources

Cliffs in Big South Fork National River and Recreation Area
Cliffs in Big South Fork National River and Recreation Area

NPS photo

Water Cycle Unit

Adventure Guide for Teens

  • This Adventure Guide can be used on the Delaware Water Gap section of the Appalachian Trail. Simply open and print the guide to take with you when you visit this area to become a Jr. Ranger of the Appalachian Trail! 

Appalachian Plateaus Parks

Last updated: August 30, 2018