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Groundwater & Basement Water Intrusion in Lynchburg, VA

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.

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Frequently asked questions

A creek runs through a wooded corridor in the middle of the city.

It does, in a confined corridor with steep sides and very little room to spread. A channel like that rises fast because its catchment is short and steep, and it carries a great deal of debris that lodges at crossings. The corridor is an amenity at street level and a constriction in hydraulic terms.

Half the yards in this neighborhood are held up by stone walls.

Terracing is how building on ground this steep was made possible, and those retaining walls are often as old as the houses. A wall holds back saturated soil after rain, and if the drainage behind it has silted up the pressure has nowhere to go. Wall condition and cellar dampness on these lots are frequently the same problem.

Does the river matter at this address?

For most properties in this city, no. The ground rises steeply enough from the water that the great majority of addresses sit well above any stage the river reaches, and what causes damage is water moving down the hillsides. Establishing which of the two applies is the first useful step, and for most of the city it is the slope.

This FAQ belongs to the Lynchburg page; it is repeated here.

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