Hopkins Roofing Built for Snow Loads, Hail, and High Winds

Hopkins sits about 900 feet above sea level in Hennepin County, and that elevation means winter storms pile snow onto roofs fast. When that snow melts and refreezes at the eaves, ice dams form, and water seeps under shingles and wicks along the decking. We see the damage every spring: rot in the sheathing, peeling paint on ceilings, and granule loss on worn-out shingles. That's why we use self-adhered ice-and-water shield at the eaves and in all valleys—it stops water before it reaches the wood.

The homes here tell the story. Mid-century ramblers and split-levels from the 1950s and 1960s often have low-slope roofs that need careful flashing at the walls and chimneys. Craftsman and older bungalows from the early 1900s have steep pitches and detailed rooflines where a proper starter course and staggered courses make the difference. Newer townhomes in planned developments may have architectural shingles, but they still need ring-shank nails driven to the right depth—overdriven nails can back out under wind uplift.

We approach every Hopkins roof the same way: assess the actual condition, then recommend the least invasive fix that works. If a roof has years left, we repair it. If it's at end-of-life wear, we tear-off and replace it with materials rated for this climate. We don't overlay a second layer over a sagging deck, and we never skip the ventilation work that prevents ice dams and heat buildup. The goal is a roof that lasts its full service life, with no callbacks.