Sinkhole risk in Morgan 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
- 5%
- At or near the surface
- 2%
- Buried under cover
- 2%
The next step for one property
Sinkholes are uncommon here; watch for new depressions after heavy rain or leaking pipes.
That works out to roughly 18 of Morgan County's 404 square miles on soluble rock, 10 of them with the rock at or near the surface. With about 73,825 residents (183 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 337 map points about 1.1 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 Morgan County
The nearest county rated sinkhole country is Monroe County, IN, about 23 miles south, close enough that the same rock may run under the county line. 2 of the 6 closest counties land in the same band; the ground changes quickly around here.
- Johnson County, IN 19 mi east · 0% at surface
- Hendricks County, IN 20 mi north · 0% at surface
- Monroe County, IN 23 mi south · 54% at surface
- Brown County, IN 23 mi southeast · 0% at surface
- Owen County, IN 24 mi southwest · 16% at surface
- Putnam County, IN 25 mi northwest · under 1% at surface
What Morgan County is built on
The largest mapped soluble unit here is the Sanders Group (limestone), Mississippian in age, covering about 5% of the county.
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
Morgan County ranks 21 of 92 in Indiana for soluble rock at the surface, and sits above 59% of US counties on that measure.
- Harrison County 94%
- Orange County 90%
- Crawford County 83%
- Lawrence County 71%
- Washington County 62%