
Hail damage to a shingle is a fracture in the mat. Everything else — lost granules, dark round marks, raised bubbles — is a different problem wearing the same clothes. That one distinction decides claims, and it is why two people can stand on the same roof and honestly disagree.
Both directions of that disagreement cost money. Real damage gets waved off as cosmetic. Cosmetic conditions get sold as damage by crews who arrived the same week as the storm and leave the same month.
What hail damage on a roof actually looks like
Haag Engineering, whose assessment protocol most adjusters were trained against, defines functional hail damage to asphalt shingles narrowly: punctures, tears, or fractures in the shingle mat. Not marks. Not color. A fracture.
On the surface that reads as an indentation with granules knocked out of it, exposing the asphalt beneath. Some are unmistakable. Many are not, and those get found by hand: press a thumb on the mark and a bruised shingle gives, softly and only there. Haag's papers describe the feel as a bruise in an apple — exactly accurate, and useless until the first time you feel one.
Why it feels soft is the part worth carrying. The fracture begins on the underside, where the impact puts the mat in maximum tension, and propagates upward toward the granules. The definitive evidence therefore sits on the side facing the deck — which is why no hail argument is ever settled by a photograph of the top of a shingle, and lifting one is the only honest way to end it.
One more tell: recently exposed asphalt is black, while asphalt exposed for months oxidizes gray. That difference is how the same protocol separates this storm from one three years ago.
Hail damage shingles: what breaks, and what only looks broken
Granule loss is the most misunderstood item here, and the correction comes from a study rather than a louder opinion.
Haag brushed measured amounts of granules off new three-tab shingles — 6, 15, 45 and 70 percent, plus one laid bare — nailed them to a south-facing 4:12 deck in Dallas and left them out for ten years. The shingle stripped of 70 percent was still shedding water at the end. Only the fully bare one eroded noticeably.
Two numbers from the same work reframe the argument. About a third of a shingle's weight is granules, and 12 to 15 percent of them had to come off before the mat was exposed at all, because manufacturers apply more than are needed to cover it. Granules are a wearing surface with slack built in.
The consequence is sharper than it sounds. If a stone stripped granules to bare asphalt but the mat underneath is intact, that shingle was already defective or already at the end of its life — a sound one struck that hard would have fractured. Hail did not take that roof's life. It found a roof that had already spent it.
Shingles are weakest where the deck does not support them — ridges, rakes, eaves, valleys — so a roof with no bruises in the field can still have broken edges along a rake.
Roof blistering vs hail damage
Start off the roof. This is the part a homeowner can settle without a ladder.
Hail comes from a direction. It dents everything soft on that side of the house at once — gutters and gutter aprons, downspouts, vent caps, fascia wrap, mailbox, the aluminum fins on the condenser. Haag's protocol treats exactly that material as evidence: spatter marks on faded metal such as condenser housings, electrical boxes and window frames, scuffs on wood fences, dents in condenser fins. Those items record the size and direction of the hailfall, and the roof's story is expected to agree with them. Concentrated, direct impacts land on the windward slope; leeward slopes get fewer, glancing ones.
Blistering dents nothing, because it never came from outside. It is gas and moisture in the asphalt expanding under heat, pushing the granule crust outward from within.
So the first question is not what the mark looks like. It is whether anything else on the property was hit, and whether the marked slopes face the storm. Clean soft metal plus marks spread evenly across every slope is a thin case for hail.
On the roof itself, the two separate cleanly.
| Hail bruise | Blister | |
|---|---|---|
| Profile | Indented into the shingle | Raised, until the crust breaks open |
| Feel | Soft spot underfoot or under a thumb | Firm; a steep-sided void once open |
| Size | Varies with stone size | Typically a quarter inch across or less |
| Mat underneath | Fractured, visible from the underside | Intact |
| Distribution | Directional, concentrated on storm-facing slopes | Wherever the shingle ran hot, any slope |
| Cause | A specific dated storm | Poor-quality asphalt and heat, often within the first year |
Blistering is a manufacturing condition or a heat condition, and the two are hard to separate from the roof. Haag attributes blisters to poor-quality asphalt combined with heat. The trade explanation for the heat half — widely taught, not a code position — is a poorly vented deck cooking the shingles from below, which is why blistering and inadequate roof ventilation turn up on the same houses.
Neither route is sudden and neither is accidental, which is the language a hail claim turns on. And there is a nastier interaction hiding in it: an open blister is a crust of granules over a void, so even small hail can break the crust away and expose bitumen without ever fracturing the mat. That leaves a roof covered in fresh-looking round marks after a storm that did not, in the technical sense, damage it.
Signs of hail damage on a roof, checked from the ground
None of this requires a ladder, and all of it is worth doing before you call anyone.
Look at the soft metal first. Gutters, downspouts, the gutter apron under the first course, vent caps, chimney caps, window wraps, garage doors, the condenser. Dented aluminum is the cheapest hail record you own.
Check for a direction. Walk all four sides. Hail that dented the north and west and left the south and east alone is behaving normally. Damage on every elevation equally is behaving suspiciously. Wood fences and deck rails hold hail scuffs too.
Scan the ridge and rake lines with binoculars. Unsupported edges break first, and a broken edge is visible from the ground when a field bruise is not.
Ignore the ceiling. Hail bruises rarely leak straight away. A fractured mat is a shortened life, not an open hole, and a roof can be genuinely hail-damaged over a bone-dry attic. Waiting for a stain finds storm damage two policies too late.
The four things most often mistaken for hail
Haag's inspectors, having looked at thousands of these roofs, list the same misidentifications repeatedly.
Foot traffic. Walking a hot roof pushes softened asphalt aside with the granules, leaving a raised ridge along the outer edge of the mark. Hail does not build a rim.
Adhesive spots. Sealant that dripped or bonded where it should not, then tore a round patch of granules off when the shingles separated. Dark, round, entirely innocent.
Manufacturing deficiencies. Bands or spots of missing granules or asphalt off the production line. They run in lines, which hail never does.
Age. Cupping, clawing, crazing and flaking all come from asphalt shrinking. They are frequently discovered after a hailstorm, which is not the same as being caused by one — worth remembering when someone finds them the week the storm passed.
A fifth category exists: marks made deliberately, with a hammer, screwdriver or coin. It is caught by pattern — grouped or lined up, centered on the shingle, one per shingle, high on the slope away from the edges, struck perpendicular to whatever plane the person stood on. Hail is random and does not aim.
How big the hail has to be
Small stones do less than the internet implies. In Haag's ice-impact testing, aged organic-mat shingles were damaged about half the time by one-inch stones; aged glass-fiber mat shingles took about 1.25 inches; thicker aged laminates took about 1.5 inches.
Set that against the National Weather Service threshold: a thunderstorm is severe at one inch of hail, a bar lowered from three-quarters of an inch in 2010. A severe thunderstorm warning is not a damaged-roof warning, and the two are read as one sentence in every storm-market sales pitch.
Stone density, impact angle, deck support and how brittle the shingles already were all move those numbers. Hail size sets the probability; the roof it lands on sets the outcome.
What Georgia does and does not let you undo
Hail work moves faster than any other kind of roofing, by design. Contracts get signed in driveways within days of a storm, often before anyone has established that a single mat is fractured. What you can get out of afterward is state law, not paperwork.
Georgia keeps this in the Fair Business Practices Act at 10-1-393.12: you may cancel up to midnight on the fifth business day after your insurer tells you in writing that all or part of the claim is not covered. Mailing the notice is enough, and it takes effect when you drop it in the box. No payment can be demanded before then, and your roofer cannot negotiate the claim unless separately licensed as a public adjuster.
The free-roof offer, read against Georgia law
The pitch is always a version of the same thing: sign now, insurance covers it, your deductible is handled. Notice the assumption — that the claim will pay, before anyone has lifted a shingle to look at the underside of the mat.
Georgia makes it illegal to advertise or promise to rebate any part of your deductible, and the drafting is clever: the ban sits inside the public adjuster statute, but a further subsection sweeps in anyone who commits the act, so a roofer is caught without ever holding an adjuster license. It is a misdemeanor and grounds to revoke any license held. The section 33-24-9.1 cited all over the web does not exist.
Bottom line
Fractured mat, or not. Everything else — granule loss, dark round spots, blisters, ridged scuffs — belongs to a different cause with a different owner. Check the soft metal for direction and stone size before you look at a shingle, expect blisters raised and bruises indented, and treat any diagnosis made from the driveway with the seriousness it earned. What insurance then does with the answer is covered in whether insurance covers a roof replacement; what a documented inspection should contain is in roof inspection cost.
Fractured mat is something you can be shown, and a slope-by-slope report that shows it settles the argument before an adjuster ever arrives. Dalton Roof Pros produces one in Dalton and northwest Georgia, alongside storm damage restoration, roof inspections and roof replacement. Call (877) 611-5034 — and we will also tell you when it is blistering and there is no claim to make.
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Related services in Dalton
Dalton Roof Pros money pages — go straight to the service you need.
- Roof Replacement →
Most roofs we replace in Whitfield County measure between eleven and sixteen squares. That figure governs more of your project than the brand printed on the shingle wrapper does, and almost nobody quotes it to you first.
- Storm Damage Restoration →
On 27 April 2011 an EF4 tornado crossed Ringgold, ran on through Cohutta and went into Tennessee, damaging or destroying hundreds of buildings in Catoosa County on its way. That night reset what people around here expect from a storm response.
- Roof Inspections →
About a third of the occupied housing in Whitfield County is rented. So most of the inspections we write here are not for a nervous buyer with an emotional stake.
- Roof Leak Repair →
A repair costs roughly the same whether your roof is twelve squares or forty-five. A replacement does not.
- Hail Damage Roofing →
Whitfield County gets hail. It does not get Texas hail.
Frequently asked questions
What does hail damage on a roof look like?
A dent with granules knocked out of it, exposing the dark asphalt underneath, and — the part that decides it — a mat underneath that has actually fractured. Haag Engineering, whose protocol most adjusters were trained on, defines functional hail damage to asphalt shingles as punctures, tears or fractures in the shingle mat.
Many bruises are not obvious to the eye at all and are found by pressing a thumb on the mark: a fractured shingle gives softly and locally, like a bruise in an apple.
How do you tell roof blistering from hail damage?
Start off the roof. Hail arrives from one direction and dents everything soft on that side of the house — gutters, gutter apron, vent caps, fascia wrap, the aluminum fins on the air conditioner. Blistering dents nothing, because it comes from inside the shingle.
On the roof itself, blisters are raised before they open, are usually a quarter inch across or smaller, sit on the hot slopes rather than the storm-facing ones, and leave a steep-sided void with no soft spot under it. Hail leaves an indentation, not a bubble.
Is granule loss on its own hail damage?
Generally not, and there is a ten-year study behind that answer rather than an opinion. Haag Engineering brushed measured percentages of granules off new shingles and weathered them in Dallas for a decade. Shingles with 70 percent of their granules removed were still shedding water at the end.
They also found 12 to 15 percent of surface granules had to come off before the mat was even exposed, because more granules are applied than are needed to cover it. Granules are a wearing surface. Losing some in a storm is the surface doing its job.
How big does hail have to be to damage a roof?
Bigger than most people assume, and it depends on what is on your roof. In Haag's ice-impact testing, aged organic-mat shingles were damaged about half the time by one-inch stones, aged glass-fiber mat shingles needed about 1.25 inches, and thicker aged laminated shingles needed about 1.5 inches. The National Weather Service calls a storm severe at one inch of hail. A severe thunderstorm warning is therefore not a damaged-roof warning, and the two get conflated constantly.
Can you see hail damage from the ground?
You can usually see the evidence, even when you cannot see the damage. Hail leaves spatter marks on faded metal — air conditioner housings, electrical boxes, window frames — scuffs on wood fences, and dents in condenser fins. All of that is at eye level, and all of it records the size and direction of the hailfall, and should line up with whatever is being claimed about the roof. The shingle bruises themselves are frequently invisible from the driveway.
How long does hail damage stay visible on a roof?
Years, but it changes appearance, and that is useful. Asphalt exposed by a recent impact is black. Asphalt exposed for a few months oxidizes to a gray film. Inspectors use that color difference to separate this storm from an older one, which matters because a claim rests on a specific storm date. Do not assume old damage has healed over, and do not assume a gray mark is new.
Local context
How this applies in Dalton, GA
Every article here is written from roofing work done in Dalton and northwest Georgia, so the numbers reflect local labour, permit and material costs rather than a national average. Your own job can land either side of them depending on access, the condition of what is already there, and the materials you pick — eave intake vent set behind the drip edge, boxed-cornice fascia spliced and milled to profile, twenty-nine-gauge exposed-fastener panel on purlin roof-overs.
The way to turn any of this into a real answer is to have someone look at your actual situation. The free estimate is free, itemized and written down, with no deposit and no obligation. Call (877) 611-5034 or start on the Dalton Roof Pros homepage.
Areas Dalton Roof Pros covers
Dalton first, then the surrounding communities of northwest Georgia. Each has its own page with local detail rather than a copy of this one:
- Varnell, GA — Whitfield County, population 2179
- Tunnel Hill, GA — Whitfield County, population 963
- Cohutta, GA — Whitfield County, population 764
- Chatsworth, GA — Murray County, population 4874
- Eton, GA — Murray County, population 824
- Ringgold, GA — Catoosa County, population 3414
Or jump to the full list of Dalton services.
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The Dalton Roof Pros Team
roofing specialists serving Dalton, GA
Written by the Dalton Roof Pros team — insured roofing pros serving Dalton, GA and the surrounding area.