Sinkhole risk in Parke County, IN: 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
- under 1%
- Buried under cover
- 9%
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 41 of Parke County's 445 square miles on soluble rock, 1 of them with the rock at or near the surface. With about 16,508 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 338 map points about 1.1 miles apart, so a pocket smaller than that can be missed or overstated.
Two things to read before deciding: why gypsum and salt move faster than limestone, and why the 9% under cover still counts.
Counties around Parke County
The nearest county rated sinkhole country is Monroe County, IN, about 56 miles southeast. 3 of the 6 closest counties land in the same band; the ground changes quickly around here.
- Vermillion County, IN 15 mi west · 0% at surface
- Putnam County, IN 20 mi east · under 1% at surface
- Fountain County, IN 24 mi north · 0% at surface
- Montgomery County, IN 24 mi northeast · 0% at surface
- Vigo County, IN 26 mi southwest · 0% at surface
- Clay County, IN 27 mi south · 0% at surface
What Parke County is built on
The largest mapped soluble unit here is the Sanders Group (limestone), Mississippian in age, covering about 5% of the county. Next is the Blue River Group at 4%.
The county also lies over the Illinois Basin, 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 Indiana
Parke County ranks 31 of 92 in Indiana for soluble rock at the surface, and sits above 51% of US counties on that measure.
- Harrison County 94%
- Orange County 90%
- Crawford County 83%
- Lawrence County 71%
- Washington County 62%