Serving Cranston
Groundwater & Basement Water Intrusion in Cranston, RI
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
Which end of the city is this address at?
It decides nearly everything, because the bay end and the hillside end are unrelated problems. Down by the water it arrives with the tide behind a coastal system and the work is elevation and defending openings. Up the hill it arrives as runoff within minutes of a cell and the work is drainage capacity. Neither remedy transfers.
A late-winter system did more than any summer one.
Winter systems here move slowly and hold an onshore wind for a day or more, which means they stack water through several successive high tides rather than one. They also deliver long soaking rains onto ground that is frozen or already full. Both effects run together, which is why late winter rather than August is the season here.
The river here goes up and comes back down the same day.
It gathers from a catchment that is largely roof and pavement, so rain reaches the channel within minutes rather than working through soil over hours, and there is very little room in the section to take a rise. The level leaps and drops back. Near a channel like that, any plan has to be in place beforehand.
The Cranston overview carries this FAQ with the city research.