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Cheaha Mountain

Cheaha Mountain
Cheaha Lake in the Fall.jpg
Lake at base of Cheaha Mountain
Highest point
Elevation 2,413 ft (735 m) 
Prominence 1,445 ft (440 m) 
Listing U.S. state high point 35th
Coordinates 33°29′08″N 85°48′31″W / 33.485511278°N 85.80866305°W / 33.485511278; -85.80866305Coordinates: 33°29′08″N 85°48′31″W / 33.485511278°N 85.80866305°W / 33.485511278; -85.80866305
Geography
Cheaha Mountain is located in Alabama
Cheaha Mountain
Cheaha Mountain
Parent range Talladega Mountains
Topo map USGS Cheaha Mountain
Geology
Age of rock Devonian
Mountain type quartzite rock
Climbing
Easiest route Road

Cheaha Mountain /ˈhɔː/, often called Mount Cheaha, is the highest natural point in the U.S. state of Alabama. It is located a few miles northwest of the town of Delta in scenic Cheaha State Park, which offers a lodge, a restaurant, and other amenities.

The highest point is marked with a USGS benchmark in front of Bunker Tower, a stone Civilian Conservation Corps building with an observation deck on top. The CCC also constructed a road to Cheaha, but the road has been closed for years. The old road is known as CC Road and contains interesting ruins. Near the peak is Bald Rock, which was recently improved with a wheelchair-accessible wooden walkway that provides an impressive overlook of the surrounding region. The entire area gives an impression of being at a much higher elevation than it actually is, in part because of the relatively low elevation of the adjacent area to the west.

Cheaha Mountain is part of the Talladega Mountains, a final southern segment of the Blue Ridge, unlike other elevations of the Appalachians in north Alabama, which are part of the Cumberland Plateau. The mountain also has the unique distinction of being the highest geographical point in the eastern portion of the Sun Belt (south of Interstate 20, and north of the Gulf of Mexico). Geologically it is composed of weakly metamorphosed sandstones and conglomerates of the Cheaha quartzite, of Silurian / Devonian age, and stands high topographically due to the erosional resistance of these rocks.


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