Serving Johns Creek
Groundwater & Basement Water Intrusion in Johns Creek, GA
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 river rose sharply on a clear day.
Releases from the dam upstream change the level here on a schedule that has nothing to do with the weather at the property. It is announced rather than unpredictable, and anyone using the river or with ground close to it is worth signing up for the notifications. The rise is not a flood and is not dangerous to a house set back from the bank, but it catches people out every year.
Water appears partway down the slope with nothing above it.
That is a seep, and it follows a change in the ground rather than the shape of the land. Water works down through the weathered granite until it meets sound rock, then runs sideways along that boundary and emerges where it reaches the surface. Regrading above it achieves nothing because it is not surface water. Intercepting it uphill of the building is what works.
The lower level is finished. What does that change?
Where the damage happens and how long it stays hidden. Water that would have crossed bare concrete now soaks into the base of the walls and the underlay, and the visible surface can be dry within a day while what is behind it is not. On a large finished lower level that difference is expensive. It is the reason a meter reading matters more than a look at the floor after any event down there.
The Johns Creek overview carries this FAQ with the city research.