That beautiful icicle fringe is a plumbing system you didn’t order, meltwater backing up under shingles and into ceilings two rooms from the eave. From Old Town Park City to Snyderville, Heber, Midway, and Kamas, it is the signature winter water loss of the Wasatch Back.
Heat escaping through the roof melts the snowpack from below; the water runs down to the cold overhang and refreezes into a ridge, the dam. New melt pools behind it, and pooled water on a roof does what water does: finds the nail holes and laps under shingles, which shed running water but don’t seal against standing water. The stain shows up on a ceiling or wall top plate, often far from the actual entry.
The dam itself is ice; the damage is a slow interior water loss that runs every warm afternoon and refreezes every night, often for weeks before anyone notices.
Ceiling stain mid-winter? That’s a now call, not a spring call
No pressure, no truck rolled, just an honest read on your situation.
Catch drips, move contents, and resist the urge to chip the dam, hatchets kill shingles and occasionally people. We trace the entry path with thermal imaging, dry the cavity before mold’s 48-hour clock runs, and document the cause: ice-dam interior damage is generally covered on Utah policies, and the file we build is what keeps it uncontested. The full response runs like any water intrusion; historic Old Town plaster gets the preservation-first treatment.
Talk to a real person, free
No pressure, no truck rolled, just an honest read on your situation.
Five-minute callback, honest advice, zero obligation. That’s the whole pitch.
Keep your phone nearby. If water is still spreading, shut off the main valve now, it’s usually in the basement or crawl space, on the street-facing wall.