The Madison County Trap: Modest Snow, Constant Cycling
Three inches of snow and a week of days above freezing and nights below it will build ice on a Madison County eave just as reliably as a foot of snow further north.

And the cycling is relentless rather than dramatic. Fifteen or twenty crossings of freezing in a season each add a layer, and the houses with the thinnest attic insulation in Madison County all find out in the same week.
Ice-barrier practice in Madison County
The residential code Kentucky follows requires eave ice barrier on new work, and Madison County enforces it. The variable on any given house is simply when it was last roofed.
What a Crew Does on a Richmond Roof
Nothing gets touched until the roof has been walked and photographed. The crew finds every dam, locates where water is getting in, shows you, and gives you the crew-hour rate and a time estimate before the equipment comes off the truck.
Removal then works from the worst point outward, so water starts draining early rather than at the end. Gutters and downspouts frozen solid get steamed through in the same visit — leaving them means the eave dams again within days.
What the dam has already done to the gutter and fascia
Ice expands as it forms, and a trough packed solid pushes the gutter away from the fascia a little more every cycle. By the time the dam is thick enough to leak, the hangers are often pulled, the back of the trough has lifted, and the fascia board behind it has been wet for weeks.
None of that is visible until the ice is off. It gets photographed when it appears, because a bent gutter found in February is a great deal easier to argue about with a carrier than one discovered in May.
Why the dam formed in the first place
Ice dams are a heat problem wearing a weather costume. Warm air escaping into the attic melts snow on the upper roof; that meltwater runs to the eave, which hangs past the heated envelope and stays below freezing; it refreezes there, and the ridge of ice grows a layer every cycle. Removal is the emergency fix. Before the crew leaves you will know which part of your attic is feeding it.
Dormers, valleys and dead spots
Ice does not distribute evenly. It concentrates where two roof planes meet, behind dormers, in dead valleys that drain nowhere, and along the north face that never sees sun. Those pockets hold water deepest and leak first.
A crew working a roof in Richmond clears the full eave line and then goes back through the valleys and dormer pockets specifically, because clearing the easy straight run and calling it done is how a roof leaks again a week later.
| Pricing model | Billed by the crew hour, rate quoted before dispatch |
|---|---|
| Dispatch window | Same day to 24 hours |
| Typical scope | Steam, 4-8 crew hours typical |
| Primary climate stressor | Repeated thaw-freeze cycling |
| Coverage area | Richmond and Madison County |
| Documentation | Dated before and after photos, written scope in Xactimate line items |
| Local ice-barrier practice | Eave membrane on new work, often absent |
Madison County Coverage From Richmond
Crews working Richmond cover the adjoining communities on the same route — Waco, Berea, Winston and Paint Lick — so a storm week usually means one truck handling several addresses in Madison County rather than separate trips.
Nearest hub towns with their own crew pages: Nicholasville, Lexington, Georgetown, Elizabethtown, Louisville, Florence.
During a cold snap Richmond gets worked alongside the neighboring Madison County towns on the same route, with active interior leaks moved to the front of the list.
If water is already inside a property in Richmond, call (888) 561-9664 rather than filling in a form — the phone is faster and leaks jump the line.















