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Groundwater & Basement Water Intrusion in Sandy, UT

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

What is a fan and why does it matter for this house?

It is the spread of gravel and sand a canyon has laid down where it leaves the mountains, and the developed ground here sits on one. What matters is that the canyon built it by moving across it. The channel is where it is today because that is where it happens to be, and a large enough event can put water on ground dry for a century.

The stream out of the canyon runs high for most of May.

That is the melt rather than any storm, and it means weeks of sustained flow instead of a peak that passes. Equipment and defenses chosen against a storm are the wrong shape for it, because nothing about the situation resolves in a day. What matters is whether something can run continuously for a month without attention.

Debris came down the canyon with the water once before.

Fans are built by exactly that, which is why the ground the city stands on is there at all. A canyon that has delivered rock and mud onto its fan has a fair chance of doing it again, particularly after fire on the slopes above. Where the channel across the fan currently runs is not where it has always run.

Open the Sandy FAQ beside the housing and climate notes.

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