Otway Silty Clay
This series consists of shallow, somewhat excessively drained, strongly sloping soils.
These soils are not extensive but are widely scattered throughout the eastern third of the
country. They formed in residuum derived from soft, calcareous shale (marl) and from some
thinly interbedded limestone.
Representative profile:
Depth
|
Color
|
Texture
|
Structure
|
0 to 4 inches
|
very dark grayish-brown
|
silty clay
|
slightly sticky
|
4 to 10 inches
|
olive
|
silty clay or clay
|
sticky and plastic; strong, blocky structure
|
17 to 48+ inches
|
dark grayish-brown
|
silt loam
|
many olive and gray mottles; massive
|
[Ashton] [Beasley] [Captina] [Corydon] [Crider] [Dickson] [Elk]
[Fairmount] [Huntington]
[Lowell] [Lawrence] [Lindside] [Newark]
[Otway] [Robertsville]
[Russellville] [Shelbyville] [Taft] [Woolper]
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