Shingle Roofing

For most steep-slope homes in Greater Houston, asphalt shingles remain the practical choice: a wide range of colors and profiles, a manageable installed weight for typical residential framing, and a repair process that doesn't require replacing an entire system every time one section gets damaged. That last point matters here in particular, where hail and wind create a steady stream of localized damage that a shingle system can usually address section by section rather than all at once.

The shingles themselves get the attention, but a properly built system also includes underlayment as a secondary moisture barrier, a starter strip along the edges to resist wind uplift from day one, flashing at every valley, wall and penetration, and a ridge cap that finishes the roof's peak. Skipping or under-building any one of those pieces shows up later as a leak that has nothing to do with the shingles being defective. See our glossary if any of those terms need a plain definition.

Architectural, dimensional shingle profiles are the common choice for most Houston homes today, and color selection is mostly a matter of matching the house and, in HOA-governed neighborhoods, getting sign-off before installation. We install Owens Corning Duration shingles, which come in a range of colors suited to different architectural styles across the region.

Long, humid summers put more stress on a shingle roof from underneath than most manufacturers design around for cooler, drier climates. That's why attic ventilation gets treated as part of the shingle system rather than an afterthought — heat and moisture trapped under the deck shortens shingle life regardless of how good the shingles themselves are.

A shingle roof rarely needs the same decision twice. Isolated damage is a job for repair, ongoing maintenance stretches out the years between major decisions, and widespread wear or storm damage eventually points toward replacement. A free inspection tells you honestly which one applies to your roof right now.

Granule loss and shingle curling show up as a roof approaches the end of its service life, usually gradually and evenly rather than in one spot. Cracked or split shingles often trace back to a specific hail or wind event rather than age alone. Lifted or missing tabs concentrate at edges and ridges where wind pressure is highest, and nail pops — where a fastener backs out of the deck over time — show up as small raised bumps under an otherwise intact shingle. Each of these has a different fix, which is why we look closely before quoting anything.