Rainwater becomes mildly acidic as it moves through air and soil. Over long periods it dissolves limestone along joints and bedding planes. The result can be enlarged fractures, caves, springs, sinking streams, closed depressions, and soil-filled openings. The ground surface may look ordinary above a complex drainage route.
The Tennessee Geological Survey's Maury County atlas maps sinkholes, unstable materials, flood-prone areas, and rock units. Those county maps are screening tools. They cannot confirm the depth, stability, or wastewater path on one homesite, so field soil and geologic work still controls a real decision.
Karst flow can respond quickly to storms. EPA describes water and contaminants moving through discrete conduits, sometimes reaching springs or downgradient water supplies with far less filtering than a uniform soil profile provides. That is why a sinkhole is not a convenient storm drain and why surfacing septic effluent near one carries wider stakes than a wet lawn patch.