Testing & Assessment
Mold Inspection & Testing in Missoula, MT
An assessment establishes whether mold is present, where it is growing, and how far it extends — before anyone quotes removal. A mold inspection locates moisture and growth that a room-level look would miss, reading wall cavities, subfloor, and the areas behind finished surfaces. The result is a scope: what is affected, what has to come out, and what is driving the moisture.
Most people reach this page after noticing something rather than after something broke: a smell that returns, a stain that spreads, a room that feels damp. An inspection answers what is actually there and where the moisture comes from, which is the information every later decision depends on. Several states, Texas among them, keep assessment and remediation as separate licensed roles specifically so the party identifying the problem is not the party selling the fix. Nothing here is medical advice — if you have health questions, those are for a clinician.
Every pro in our network is licensed and insured in Montana.
Frequently asked questions
Seventeen inches of precipitation. Where does basement water come from?
Mostly from the mountains rather than the sky above the house. Snowpack at elevation releases over several weeks and raises the valley water table, so a basement can take water in a month with almost no local rainfall. Reading a rain gauge will not explain the timing.
What is an inversion and does it matter indoors?
Cold air settling into the valley and staying there under a warmer layer above. It matters because it removes the drying capacity a normal winter day would provide: air movement is minimal and humidity in the valley stays elevated, so anything damp stays damp for much longer than the temperature alone suggests.
Does lake-bed soil behave differently from ordinary valley fill?
Yes, because it is exceptionally fine. Silts and clays deposited in still water drain slowly and hold moisture well, so water reaching a foundation through them lingers. It also means test results from one part of the valley transfer poorly to another, since the deposits vary in thickness.