Lowell Silt Loam
This series consists of deep, well-drained, sloping soils on hillsides. These
soils are widely scattered in the extreme eastern part of the country, but their acreage
is small. They formed in residuum derived from thin-bedded, argillaceous limestone.
Representative profile:
Depth
|
Color
|
Texture
|
Structure
|
0 to 6 inches
|
brown
|
very friable silt loam
|
|
6 to 20 inches
|
yellowish-brown to brown
|
silty clay loam
|
medium, blocky structure; slightly sticky
|
20 to 40+ inches
|
yellowish-brown
|
silty clay
|
sticky and slightly plastic; strong, blocky structure
|
[Ashton] [Beasley] [Captina] [Corydon] [Crider] [Dickson] [Elk]
[Fairmount] [Huntington]
[Lowell] [Lawrence] [Lindside] [Newark]
[Otway] [Robertsville]
[Russellville] [Shelbyville] [Taft] [Woolper]
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