Serving Spring House
Groundwater & Basement Water Intrusion in Spring House, PA
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
It arrives at the wall long after the sky has cleared.
Late water has traveled along the rock rather than across the surface. It soaks through the soil, meets stone it cannot pass, and runs the top of it until something interrupts, which takes time and can bring it from beyond the property line. Surface flow shows up during the storm. That gap is genuine evidence and it points the remedy below ground rather than at the gutters.
How would we find out how deep the rock is under our lot?
A test pit is the cheap answer and it takes an afternoon. Dig down beside the house during a wet spell and you learn two things at once: how far it is to rock, and whether water is standing in the material around the foundation. That is more useful than any general statement about the area, because depth here changes over a few dozen feet and it is the whole reason neighbors get different results from identical work.
The stream behind us is small and it came over.
Small headwater channels do exactly that. The catchment above has been developing, so it sheds quickly, and there is very little room in the channel to take a rise, which means the level jumps rather than the water spreading. It drops as fast as it came. Watching it once during heavy rain tells you more than any amount of looking at it in August.
These questions come from the Spring House page.