Ice and water shield
Self-adhering membrane at vulnerable points
Drip edge is the L-shaped metal at the eaves and rakes that throws water clear of the fascia and into the gutter. Without it, water tracks back along the underside of the shingle edge and runs down the fascia board, which is the single most common reason fascia rots. It is inexpensive, it is required by most current codes, and it is routinely missing on older roofs — so it is worth checking whenever fascia or gutter work is being done.
Tazewell 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 Tazewell 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.
It is why the fascia rots. Water clings to the underside of the shingle edge and tracks back onto the timber instead of dropping into the gutter. Retrofitting it is cheap compared with replacing fascia repeatedly.
At the eaves it can often be slid under the first shingle course. At the rakes it needs to go under the underlayment, which usually means lifting the edge courses. Both are localised jobs.
Self-adhering membrane at vulnerable points
Missing, cracked or lifted shingles
Crown, cap and masonry
Lifted tabs and broken seals
Remaining-life letter for a sale or insurer
Algae streaking and moss growth
You will get a straight answer on whether Tazewell County needs someone out today or whether it can wait — before anyone quotes you for anything.
Call (706) 696-1888