Mitchell Caverns

Detailed Description
The road to Mitchell Caverns is on the eastern flank of the Providence Mountains. The Providence Mountains consist mostly of partially metamorphosed strata of late Paleozoic age - Devonian, Mississippian, and Permian limestone (and marble) (Stone and others, 1983; Norris and Webb, 1990).
Details
Image Dimensions: 800 x 600
Date Taken:
Location Taken: US