Serving Monroe
Groundwater & Basement Water Intrusion in Monroe, MI
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 lake came up several feet and there was no storm surge.
A shallow lake responds to sustained wind by piling up at the downwind end, and the difference between one end and the other can be substantial. It has nothing to do with rain and it can happen under a clear sky. When the wind drops the water sloshes back, sometimes more than once. Following the wind direction and duration is what predicts this, not the rainfall forecast.
Nothing came over the bank and the water still rose upstream.
Where a river meets a lake whose level has been pushed up, the river cannot discharge and it holds whatever is in it. So the flooding happens upstream of the mouth, and it happens without any unusual flow in the river at all. It is why properties well back from the lake can be affected by something that is entirely a lake event.
Ice piles up along the shore in the same places.
The same wind that raises the water moves the ice, and it comes ashore where the shape of the shoreline collects it. That is a different hazard from flooding: it is a physical push against whatever is in the way, and it repeats in the same spots year after year. Knowing whether a property sits in one of those places is worth establishing from the neighbors rather than the mapping.
Open the Monroe FAQ beside the housing and climate notes.