Serving Stow
Groundwater & Basement Water Intrusion in Stow, OH
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 neighbor's drainage work made no difference to us.
Depth to rock changes over a few dozen feet here, so identical work gives different answers. A drain that intercepts a water table on deeper soil does nothing on a lot where the water is running along the rock from somewhere else entirely. Nothing above ground distinguishes the two. Digging a small pit on your own lot during a wet spell settles which situation you are in, and it costs almost nothing.
Water arrives some hours after the rain has stopped.
That delay points at flow along the rock rather than across the surface. Rain soaks through the soil, reaches sandstone, and travels along the bedding, which takes time and can bring water from a distance. Surface runoff arrives during the storm; rock flow arrives afterward. The timing is genuinely useful diagnostic information and it puts the remedy below grade.
Can a footing drain be installed where rock is close?
Usually, and the discharge point is the difficulty rather than the drain. On sloping ground a gravity line to daylight is ideal since it has no pump to fail. Where the rock leaves nowhere lower to go, an interior perimeter drain to a sump is the practical alternative. What does not work is relying on backfill in a rock excavation to drain by itself, because there is nowhere for it to drain to.
Read it with the local conditions on the Stow page.