Why Foundation Problems Are Common in Southern Indiana
This region's clay-heavy soils are the primary driver. Clay expands dramatically when wet and contracts when dry β creating constant lateral pressure against foundation walls as the seasons cycle. The Ohio River valley creates a high water table in low-lying areas, and Southern Indiana's meaningful spring and fall rainfall keeps soil saturation high for extended periods.
Indiana's freeze-thaw cycles make everything worse. Water in soil and cracks freezes, expands by roughly 9%, and creates hydraulic pressure no foundation resists indefinitely. A crack that's 1/8 inch in November may be 3/8 inch by April without any other movement occurring.
Block foundations age differently than poured concrete. The mortar joints β not the blocks themselves β are usually the failure point. After 40β50 years, mortar in a block foundation loses enough strength that the same pressures it resisted easily for decades start winning. This is why we see so many bowing wall situations in Jeffersonville and New Albany's older neighborhoods.