Sinkhole risk in Leake County, MS: Mostly deep or small
Mostly deep or small
Some soluble rock, mostly deeply buried or in a small share of the county.
- On soluble rock
- 9%
- At or near the surface
- 9%
- Buried under cover
- 0%
What this means before you buy
Sinkholes are uncommon here; watch for new depressions after heavy rain or leaking pipes.
That works out to roughly 55 of Leake County's 583 square miles on soluble rock, 55 of them with the rock at or near the surface. With about 21,462 residents (37 per square mile), much of the land is open, and the mapped rock may sit far from where people actually live. The figures come from 404 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 Leake County
The nearest county rated sinkhole country is Oktibbeha County, MS, about 59 miles northeast. 1 of the 6 closest counties land in the same band; the ground changes quickly around here.
- Attala County, MS 23 mi north · 0% at surface
- Neshoba County, MS 23 mi east · 0% at surface
- Scott County, MS 24 mi south · 7% at surface
- Madison County, MS 31 mi west · under 1% at surface
- Newton County, MS 34 mi southeast · 21% at surface
- Winston County, MS 36 mi northeast · 18% at surface
Which formation it is
The largest mapped soluble unit here is the Cook Mountain formation (sand), Eocene in age, covering about 9% 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
Leake County ranks 24 of 82 in Mississippi for soluble rock at the surface, and sits above 67% of US counties on that measure.
- Clay County 94%
- Oktibbeha County 94%
- Chickasaw County 93%
- Noxubee County 88%
- Pontotoc County 82%