Roof leak detection
Finding where the water actually gets in
A new roof is more than the covering: decking, underlayment, ice and water membrane at vulnerable points, drip edge, flashing at every junction, and a ventilation system that balances intake against exhaust. Most premature failures trace back to one of those details being skipped rather than to the shingles themselves — which is why two roofs with identical materials can differ by a decade in service life.
Livingston County gets the full range — freeze-thaw cycling through winter, severe convective storms with hail and straight-line wind in spring and summer, and enough temperature swing between them to work every joint on the roof loose. Freeze-thaw is the quiet one: water finds a hairline gap in flashing, freezes overnight, expands, and opens it slightly wider, repeating through a Livingston County winter until a joint that was watertight in October is leaking by March. Spring brings the loud damage, and derechos have put straight-line wind through this region at speeds that take ridge caps and whole shingle courses. Housing stock here is older than average, which means a lot of roofs where the flashing has already been through several decades of that cycle.
Detailing, not materials. Flashing reused instead of replaced, ventilation left unbalanced, drip edge omitted, or nails driven high or overdriven — each shortens the life of an otherwise identical roof. These are the things worth asking about.
No. It is the cheapest component and the most common failure point. Reusing it on a new roof means the first thing to fail will be the old part you kept.
Finding where the water actually gets in
Airflow that stops condensation and ice dams
Cedar shake roofs
Lifted tabs and broken seals
What repairs actually cost here
Scheduled checks instead of emergencies
You will get a straight answer on whether Livingston County needs someone out today or whether it can wait — before anyone quotes you for anything.
Call (706) 696-1888