Lindside Silt Loam

The Linside series consists of deep, moderately well drained soils of the first bottoms. These soils are of moderate extent in the county; they are widely scattered along rivers and small creeks. Those soils along the creeks formed in sediment that washed mostly from soils of limestone origin, and those along the Ohio River formed in mixed sediment that washed from the upper part of the Ohio River basin.

Representative profile:

Depth	Color	Texture	Structure
0 to 10 inches	brown	friable silt loam
10 to 23 inches	brown	friable silt loam	few grayish-brown mottles in lower part; massive
23 to 42+ inches	grayish-brown	friable silt loam	yellowish-brown and some light-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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