

Districts
The Cumberland Plateau is divided into eight districts: Sand Mountain, Lookout Mountain, Blount Mountain, Warrior Basin, Jackson County Mountains, Murphrees Valley, Wills Valley, and Sequatchie Valley [see Figures 2 and 3].
The Sand Mountain district separates the valleys of the Tennessee River and Big Wills Creek, stretching for about 90 miles from the Alabama-Tennessee-Georgia border to near Cleveland, in Blount County. It is about 15 miles wide at its widest point and slopes gently to the southwest, with elevations decreasing from 1,960 feet at Fox Mountain (DeKalb County) to about 500 feet in Blount County. Its southwestern boundary is the Warrior Basin, and its surface is flat and unremarkable, cut by very few streams.
Lookout Mountain lies to the east of Wills Valley and stretches from the Georgia state border in DeKalb County to Gadsden, in Etowah County. It continues through northwest Georgia to Chattanooga, Tennessee. At less than 10 miles wide and under 50 miles long, Lookout Mountain is narrower and shorter than Sand Mountain. The plateau tilts toward both the southwest and the southeast. Elevations along its northwestern edge overlooking Wills Valley decrease from about 1,800 feet above sea level at the Alabama-Georgia line to about 900 feet at Gadsden. The southeastern edge of the plateau is between 100 and 300 feet lower than the northwest edge. Along most of its length, the interior of the plateau sags between 100 to 200 feet below the southeastern edge.

The Warrior Basin district occupies most of the Cumberland Plateau in central and western Alabama. It stretches from just south of the Tennessee River in Morgan County to Tuscaloosa. Its northern boundary with the Jackson County Mountains is the first cliff face, or scarp, south of the Tennessee River. Farther to the west, it is bounded by a scarp that forms the southern edge of Moulton Valley. Its eastern boundary is a low ridge, called Rock Mountain and Sand Mountain in Blount and Jefferson counties, respectively. (Sand Mountain forms the northwestern horizon when looking in that direction from downtown Birmingham.) The southwestern boundary with the East Gulf Coastal Plain occurs from about Vance, in Tuscaloosa County, to Hamilton, in Marion County.

The Murphrees, Wills, and Sequatchie Valley districts are three roughly parallel valleys that run northeast-southwest. Each formed on an anticline, an arch-shaped fold in a rock layer, capped in the Pottsville Sandstone that was eroded away over time. As a result, water action cut deep, narrow valleys into the uplands areas. These valleys are narrow (generally less than eight miles wide) and deep, with nearly vertical sides that commonly descend between 500 and 600 feet below the uplands.
The Murphrees Valley district is the smallest, being only about 30 miles long and about three miles wide. It is bounded by the Straight and Red Mountains. The valley begins near Mountainburg, in Etowah County, and joins Big Canoe Valley just north of Pinson, in Jefferson County.

Sequatchie Valley widens to the northeast, narrows near Blountsville, in Blount County, and then reaches a width of eight miles north of Lake Guntersville. The valley extends 90 miles northeast to Bridgeport, in Jackson County and continues into Tennessee.
River Systems
The Warrior and Tennessee River systems drain most of the Cumberland Plateau [See Figure 4]. Each has a distinctive drainage pattern.
The Tennessee River flows southwest in Sequatchie Valley from the Alabama-Tennessee border to Guntersville, in Marshall County, where it abruptly changes direction and flows northwest through the Jackson County Mountains and into the Highland Rim physiographic section. The change in direction has been attributed to a large northwest-southeast-trending structure called the Anniston Cross-Strike Structural Discontinuity, a northwest-trending zone of highly crushed rocks. This geologic feature caused a zone of weakness into which the river eroded.
The Black Warrior system has two different flow patterns. Its eastern tributaries, the Mulberry Fork and Locust Fork, rise between Cullman and Guntersville and flow southwest in a trellis pattern consisting of long, relatively straight stream segments with smaller short tributaries joining at right angles. The northern tributary, the Sipsey Fork, flows in a very distinctive rectangular pattern. Several individual straight stream segments flow either southwesterly or southeasterly and make approximately right-angle bends at various points.

Natural Resources
The Cumberland Plateau contains economic deposits of Pennsylvanian-aged bituminous coal [See Figure 5]. The deposits are divided geographically into four regions, or fields: the Warrior Basin, Plateau, Cahaba, and Coosa. During the nineteenth century, the Coosa and Cahaba fields were the source of coal for Alabama's fledgling iron industry and for the Confederacy. Much of the coal mining in the twentieth century was surface mining, and the scars can be seen throughout the area. Recent reclamation efforts in many places have begun to restore the landscape. Methane is also an important economic resource in the Cumberland Plateau. A by-product of coal formation, methane gas accumulates in and around the coal beds and is thus called coalbed methane. The gas is extracted from several areas in the Warrior Basin, mainly in Tuscaloosa, Walker and Jefferson counties.
Additional Resources
Adams, G.I., et al. Geology of Alabama. Geological Survey of Alabama Special Report 14. Tuscaloosa, Ala.: Geological Survey of Alabama, 1926.
Additional Resources
Adams, G.I., et al. Geology of Alabama. Geological Survey of Alabama Special Report 14. Tuscaloosa, Ala.: Geological Survey of Alabama, 1926.
Coleman, J. L., et al. "Structure of the Wills Valley Anticline-Lookout Mountain Syncline between the Rising Fawn and Anniston CSDs, Northeast Alabama." Geological Society of Alabama Guidebook 25. Tuscaloosa: Geological Society of Alabama, 1988.
Jones D. E. Geology of the Coastal Plain of Alabama. Guidebook of the 80th Meeting of the Geological Society of America, New Orleans, 1967.
Lacefield, J. Lost Worlds in Alabama Rocks. Tuscaloosa: Alabama Museum of Natural History, 2013.