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| System | Age | Formation | Average Thickness (ft) | Elevation near Huntsville (ft) | Geologic Description | Exposure Siting in Huntsville - Madison County Area |
| Quaternary | Recent | Alluvium Deposits | 0-30 | 1560-1580 | Unconsolidated sand, clay, and gravel | Some evidence found in northeast Madison County atop Bingham Mountain |
| Pennsylvanian | Pottsville Formation | 85-90 | 1480 | Sandstone, brown and gray-brown, medium to coarse grained, massive and thin bedded, contains some shale and a thin seam of coal near base. Well rounded grains. Iron containing. | Top of Cumberland Plateau including Monte Sano, Green, Keel, and Wallace Mountain | |
| Mississippian | Chester | Pennington Formation | 80-100 | 1400 | Shale, red, gray, and green with sand and some shaly limeston beds | Thin seam found near base of sandstone caprock along Monte Sano bike trails running below the bluffs |
| Bangor Limestone | 350-400 | 1000 | Limestone, blue-gray, dark gray, crystalline, oolitic and partly fossiliferous, dolomitic | Numerous outcroppings found at surface. Exposed in upper rock cuts along Governors Drive/Highway 431 across Monte Sano heading into Big Cove | ||
| Hartselle Sandstone | 0-90 | 910 | Sandstone, tan to brownish gray, medium to coarse grained, hard, sharp edged grains | Found all across the upper crest of Chapman Mountain, Weatherly Mountain, King Mountain, and Garth Mountain | ||
| Gasper Formation | 40-90 | 820 | Limestone, light-gray to gray, argillaceous, crystalline, abundantly fossiliferous, partly oolitic, some shale layers. | Large exposure all across mountainous slopes | ||
| Meremac | St. Genevieve Limestone | 180+/- | 640 | Limestone, light gray, oolitic, thick-bedded, fossiliferous | Exposure along lower base of mountains | |
| Tuscumbian Limestone | 150-200 | below median ground level | Limestone, dark to light gray, crystalline, massive bedded, fossiliferous, some chert near base of layer | Outcroppigs all across Huntsville including Big Springs Park below banks and the courthouse. Thick layers below surface all across metro area. Red Clay Forming. | ||
| Osage | Fort Payne Chert | 95-160 | below median ground level | Limestone, gray and yellow, abundant chert, highly porous | Heavily Saturated Ground water bearing formation. Tapped into at Dallas Wells. | |
| Devonian | Chattanooga Shale | 0.5-10 | below median ground level | Shale, black, hard, fissile, contains bitumen and pyrite, some sand, partly radioactive | Thin seams found along Flint River Basin in Northeast and North Central Madison County near Riverton Area. | |
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