Cumberland Plateau

The Cumberland Plateau is a deeply dissected plateau, with topographic relief commonly of about four hundred feet (120 meters), and frequent sandstone outcroppings and bluffs.

At Kentucky's Pottsville Escarpment, which is the transition from the Cumberland Plateau to the Bluegrass in the north and the Pennyrile in the south, there are many spectacular cliffs, gorges, rockhouses, natural bridges, and waterfalls. In Tennessee, the Cumberland Plateau's western border is the Highland Rim east of the Nashville Basin, and its eastern edge is marked by Walden Ridge, which continues south into Alabama as Sand Mountain. Walden Ridge and Sand Mountain are separated from the main portion of the Cumberland Plateau by the Sequatchie Valley. The Sequatchie River empties into the Tennessee River just below Nickajack Dam and the valley extends into Jackson County, Alabama, as part of the Tennessee Valley.

In Kentucky, the height of the plateau's hills increases from northwest to southeast, with the westernmost areas of the plateau having a relief of around 200 feet and an appearance similar to the knobs region, whereas areas near Black Mountain have a relief exceeding 2,500 feet.

The Cumberland Plateau is a physiographic section of the larger Appalachian Plateau province, which in turn is part of the larger Appalachian Highlands physiographic division.[2] The Plateau rises about 1000 feet above the surrounding areas in the region (Tennessee Vacation, 2018). The rough topography that makes up the Cumberland Plateau has caused a development of isolated settlements and the local economies based on subsistence agriculture (Britannica, 2016).

The sedimentary rocks that compose the Cumberland Plateau and larger Appalachian Plateau are of Mississippian and Pennsylvanian geological age, composed of near-shore sediments washed westward from the Appalachian Mountains. Some rock layers were laid down in shallow coastal waters, some, including bituminous coal seams were laid onshore in swampy environments. These are interlaced with delta formations of cross-bedded sandstones and occasionally conglomerate.

There are numerous discontinuities in the beds, where they were raised high enough to be eroded, then lowered to have more sediments added on top near Cumberland Falls, 400 feet below the top of the formation, going by the age of the bedrock which has moved less than a tenth of an inch for the last 300 million years, caused mainly by lateral erosion of the plateau.

The plateau contains some of the largest stretches of contiguous forest in the eastern United States. Regionally, forests are intermediate between oak (Quercus) and hickory (Carya) forest types with pines (Pinus) occurring on dry, upland sites and mesophytic species occurring in protected coves.

The Oak Ridge National Laboratory is involved with the conservation of the mixed mesophytic forests within the Northern Cumberland Plateau.[3] Conservation organizations active on the Cumberland Plateau include The Nature Conservancy, the Doris Duke Charitable Foundation, and the Natural Resources Defense Council.

• Cumberland Mountains
• Geology of the Appalachians

• Caudill, Harry M., Night Comes to the Cumberlands (1962). ISBN 0-316-13212-8
• Finger, J. R. (2001) Tennessee Frontiers: Three Regions in Transition. Indiana University Press.

Wikimedia Commons has media related to Cumberland Plateau.

• The Kentucky Highlands Project
• Physiographic Regions of Tennessee Broken link as of 2016-12-18
• The Columbia Gazetteer of North America, Cumberland Plateau
• Tennessee landforms

32.4761206°N 85.0525375°W / 32.4761206; -85.0525375