Ozarks (Rural)
Ozark County sits on karst, so springs, losing streams, and sinkholes shape the ground
Karst terrain controls drainage, well water, and where surface water actually goes, which matters to anyone buying or building rural land here.
Ozark County lies on soluble carbonate bedrock, the classic recipe for karst: caves, sinkholes, losing streams, and big springs where groundwater surfaces. The county’s spring-fed waters, including the cold flows that feed the North Fork River and Bryant Creek, are the visible outlets of that underground plumbing. For a buyer or builder the practical points are concrete. Surface water can vanish into the ground and resurface elsewhere, so a dry-looking draw may still drain a wide area, and a sinkhole can act as a direct pipe to the aquifer, which is why what goes into one can reach a spring or a downgradient well. The Missouri Geological Survey within DNR maps and explains karst features and is the place to start before assuming a parcel drains the way it looks. Treat sinkholes as plumbing connected to groundwater, not as low spots to fill.
References
Where this fits: this note belongs to Ozark County. See every local note for the county on its page.