|
| | Carbonton Soil
To obtain official soil series description,
click
here.
 The Carbonton series consists of moderately deep, somewhat poorly drained soils with slow permeability. They formed in residuum from Triassic siltstone,
mudstone, conglomerate, and shale. These soils are on uplands of the Triassic Basin in the Southern Piedmont. Slope ranges from 2 to 40 percent. Mean
annual precipitation is about 47 inches and mean annual air temperature is about 60 degrees F. near the type location.
TAXONOMIC CLASS: Fine, mixed, semiactive, thermic Oxyaquic Hapludalfs
< Back to Soils Gallery
| |
|
About Us
Back to Top