Serving Tipton
Groundwater & Basement Water Intrusion in Tipton, IN
Basement seepage, failed sumps, and hydrostatic pressure against the foundation are extracted and dried, and the path from the ground is identified so the loss does not repeat. Groundwater and basement seepage are extracted and dried only after the path from the soil is identified — a wall, a slab, a drain, or a failed sump. Drying the interior without stopping that path returns the same water to the same floor.
Frequently asked questions
The creeks here look like ditches.
Many of them were straightened and deepened to drain the farmland, which is why they run so directly. A straightened channel moves water faster than a meandering one and has lost the floodplain it used to spread into. That is efficient for the fields and it concentrates the flow arriving downstream.
The basement is wet in spring with no heavy rain.
That is the water table rather than any storm. Across this flat ground it rises seasonally to sit close under basement floors and pushes up through the slab and the joint at the wall. It affects properties nowhere near a channel, and it follows the season rather than the weather.
The fields empty faster than the ground ever would.
Because it was made to. This was wet prairie and it only became farmland once tile was laid to carry the water away. That tile still works, moving rain to the creeks within hours instead of the days the original ground took, which is why levels come up quickly after a storm.
These questions come from the Tipton page.