Roofing Services in Broomfield
Broomfield’s older sections, with their 1960s and 1970s ranch and split-level homes, are a big part of what makes this neighborhood feel established. But those same roofs are now pushing fifty years old. Original asphalt shingles are curling, losing tabs, and showing end-of-life wear. That’s not a cosmetic issue—it’s a signal that the roof deck underneath may already be seeing water intrusion.
We’ve worked on plenty of these mid-century homes. The low-pitch rooflines and wide eaves that give them their character also mean water moves slower across the surface. When shingles start to fail, water can seep into the decking and wick along the rafters. That’s how rot and decay get a foothold before you ever notice a leak inside. If your roof is from the original build era, it’s worth having a crew check the condition of the substrate, not just the shingles you can see from the street.
Newer Broomfield builds—those 1990s and 2000s two-story tract homes—have their own issues. The steeper pitches shed water better, but they catch more hail impact. Summer storms roll in off the Front Range and drop marble-sized hail that dents and cracks asphalt shingles. Granule loss accelerates, and within a few seasons you’re looking at a roof that’s lost most of its protective coating. We see it all the time in the sections near Big Dry Creek Trail, where the open space gives storms a clear run at the rooftops.
Here’s how we handle roofing in Broomfield. We start with a full inspection—not just a glance from the driveway. We check for soft spots, exposed fasteners, and any places where the starter course or field course has lifted. If the roof is beyond repair, we do a complete tear-off down to the deck. We replace any rotted or sagging plywood, then install a self-adhered ice and water shield along the eaves and valleys. That’s critical for the snow loads Broomfield gets. We use ring-shank nails for the shingles, and we hand-seal the edges where wind could lift them. Staggered courses keep the roof looking clean and performing the way it should.
If your roof still has life in it, we can recover or overlay in some cases, but we’re honest about when that makes sense. An overlay only works if the deck is sound and the existing layer is flat. On a 1960s roof that’s already curled and brittle, a recover is just a band-aid. We’d rather tell you the truth and do it right the first time.
Our crews know Broomfield. We’ve done jobs on streets off Main Street, near the Mamie Doud Eisenhower Public Library, and along the open space by Broomfield County Commons Park. We understand the HOA expectations in the newer developments and the practical realities of working on older homes. When we’re up on a roof, we’re not just looking at shingles—we’re looking at the whole picture: the cottonwood branches that overhang your gutters, the way the afternoon sun hits the south slope, the roof’s history in this specific Colorado climate.
Common Roof Problems in Broomfield
Walk through Broomfield’s older sections and you’ll see the same pattern: 1960s asphalt shingle roofs that have simply reached the end of their service life. The shingles curl at the edges, some tabs are missing entirely, and the surface is rough with granule loss. These roofs are past the point of patching. The asphalt has oxidized and become brittle. When hail hits them, they crack instead of flexing.
Homes along Big Dry Creek Trail take a beating from summer hailstorms. The open space gives the wind a clear fetch, and the hail that comes through can dent shingles and knock off granules. That erosion exposes the fiberglass mat underneath, and once that happens, the shingle’s ability to shed water drops fast. You might not see a leak right away, but the roof is degrading from the top down.
Then there are the cottonwoods. Mature trees along the creek and in older yards drop heavy branches in wind events. A branch can scrape across the roof, tearing the shingle surface, or land on the edge and crack the fascia. Even without direct hits, the constant shade from those trees keeps the roof damp longer, which encourages moss and algae to grow and hold moisture against the shingles. That’s a recipe for rot and decay in the decking below.
Snow loads are the other factor. Broomfield gets real winters. When snow sits on a roof that’s already lost its seal, water can work its way under the shingles and freeze. Ice dams form at the eaves, and the water backs up under the field course. That’s how you get interior ceiling stains that look nothing like the roof problem they came from.