Serving Amarillo
Groundwater & Basement Water Intrusion in Amarillo, TX
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 basin at the edge of the property held water for a month.
Those basins have no connection to any stream, so what arrives leaves by soaking down or evaporating and both are slow. A month is ordinary. For a property beside one the number that matters is how high the water stands and for how long, rather than any rate of flow, and that is a different sum from a creek.
The aquifer under this country has been dropping for decades.
It has, and it is measured and published rather than disputed. For a house it matters mainly through wells: a supply that was reliable at one depth may not be at the same depth in twenty years. It also means the ground here is drying out in the long term rather than getting wetter.
There are canyons cut into the plain not far from the city.
There are, at the edge of the caprock, and they produce catchments that are short, steep and quick in a landscape that is otherwise flat and slow. A property near one of those rims is dealing with a completely different hazard from a property out on the plain, and the two are only a few miles apart.
The Amarillo overview carries this FAQ with the city research.