Serving Manhattan
Groundwater & Basement Water Intrusion in Manhattan, KS
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
Does the levee line run in front of this address or behind it?
Nothing on the ground announces it, so it is the first thing to establish rather than assume. A defended area has an edge and simply stops there, which means two houses within sight of each other can fall either side with unrelated exposures and unrelated premiums. The city and the current mapping both mark where it runs.
The hills here are limestone with very little soil on them.
They are, which means the slopes shed nearly everything that lands on them and deliver it to the valley floor quickly. It also means a drainage scheme that needs depth is breaking rock rather than digging soil. Surface work and interception above a building achieve more here than anything that relies on the ground accepting water.
The households here turn over every year. Where does the history live?
Annual turnover means the record of what a property has done lives in the files rather than in anybody's head. City records show past repairs, the mapping shows the ground, and the households on a street that have stayed put hold everything else. Ask inside the first month; nobody offers it unprompted during a storm.
The same questions, in context, on the Manhattan mold removal page.