Flatwoods series soils are moderately deep and moderately well drained. They formed in weathered acid shale material in the highlands of the Great Valley. The slopes range from 2 to 15 percent.
The Flatwoods physiographic region extends south of Houston, Chickasaw County, along the western edge of the Black Belt into Alabama, and ranges from three to fifteen miles wide (Lowe, 1919).
The gray soil of the Flatwoods is not fertile and it drains poorly; therefore, it is not conducive to cultivation. Although this area can sustain several varieties of upland hardwood, it is considered one of the least productive soil regions in the state.
With this information, we can conclude that the Flatwoods is formed in weathered acid shale material in the highlands of the Great Valley.
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