Sinkhole risk in Madison County, MS: No soluble rock mapped
No soluble rock mapped
No soluble bedrock mapped.
- On soluble rock
- under 1%
- At or near the surface
- under 1%
- Buried under cover
- 0%
What this means before you buy
No soluble bedrock is mapped here, so natural sinkholes are unlikely. Collapses from broken pipes or old mines are a separate risk.
That works out to roughly 1 of Madison County's 714 square miles on soluble rock, 1 of them with the rock at or near the surface. With about 114,247 residents (160 per square mile), homes are spread across towns and farmland, and a mapped unit may or may not reach the developed parts. The figures come from 539 map points about 1.2 miles apart, so a pocket smaller than that can be missed or overstated.
Read next: why gypsum and salt move faster than limestone, and how these percentages are measured.
Counties around Madison County
The nearest county rated sinkhole country is Oktibbeha County, MS, about 86 miles northeast. 1 of the 6 closest counties land in the same band; the ground changes quickly around here.
- Yazoo County, MS 22 mi northwest · 3% at surface
- Rankin County, MS 26 mi south · 13% at surface
- Leake County, MS 31 mi east · 9% at surface
- Scott County, MS 33 mi southeast · 7% at surface
- Holmes County, MS 34 mi north · 0% at surface
- Hinds County, MS 36 mi southwest · 24% at surface
What Madison County is built on
The largest mapped soluble unit here is the Vicksburg group and Chickasawhay limestone (limestone), Oligocene in age, covering about under 1% of the county.
The county also lies over the Gulf Coast salt domes, a deep salt or gypsum basin. Deep beds rarely cause surface collapse on their own, but wells and mining into them have.
Against the rest of Mississippi
Madison County ranks 34 of 82 in Mississippi for soluble rock at the surface, and sits above 50% of US counties on that measure.
- Clay County 94%
- Oktibbeha County 94%
- Chickasaw County 93%
- Noxubee County 88%
- Pontotoc County 82%