Serving Vicksburg
Groundwater & Basement Water Intrusion in Vicksburg, MS
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
Should we be worried about the bank behind the house after a wet spring?
It deserves a look rather than an assumption. Loess holds a vertical face when it is dry and loses strength as it saturates, so the risk here builds through a wet season rather than arriving with a single storm. Early signs are small: cracks running parallel to the top of a slope, soil pulling away from a structure, a step forming where the ground was smooth. Those are worth photographing and monitoring rather than filling in.
Water runs down the bluff face and into the lower property.
That is the standard geometry here and the remedy is upslope rather than at the building. Water concentrated on a loess face erodes it as well as delivering water below, so a diversion at the top that keeps runoff from ever reaching the face addresses both problems at once. Work done only at the bottom of the slope treats the water and leaves the erosion, which usually means returning to the same job in a few years.
Is the flooding here from the river or from the rain?
Both occur and they affect different properties. River flooding is a low-ground and backwater problem with days of warning from upstream gauges. Rainfall here produces bluff runoff and saturation, which affects the high ground and gives no warning at all. Because the city spans both settings, general local flood advice is close to useless without knowing which of the two situations a specific property is in.
Read it with the local conditions on the Vicksburg page.