The short answer
At fifty years, the weak points tend to be the details and not the broad field of tiles: ridge bedding that has cracked, gable-edge mortar that has crumbled, and bitumen felt that has perished beneath. Those faults let water in long before the tiles themselves give up.
The houses that went up from 1976 were built quickly and well enough to still be standing, but their roofs were detailed in ways that have since changed. Fifty years on, the pattern of faults is consistent from street to street.
Q1.1Why does ridge and verge mortar fail?
The ridge is the line of capping tiles along the top, and the verge is where tiling finishes against the side of a gable wall. On a Toothill house of this era both were normally bedded in sand and cement. Mortar shrinks, cracks and lets go, so you see tiles loose at the ridge or a gable edge that has opened up. Since BS 5534:2014, mortar alone is not relied on for fixing these tiles, and a repair now adds mechanical fixings, or a dry-fix ridge kit that has passed the tests in BS 8612. Our ridge and verge dry-fix page explains the difference.
Q1.2What happens to the felt and battens?
Beneath the tiles sits the underlay, a membrane that catches wind-blown rain and condensation, fixed over battens, the timber laths that carry the tiles. Old bitumen felt goes brittle, tears at the laps and sags between rafters. From the loft you can sometimes see daylight, stained timber or a dark patch on the felt, and each is a clue.
Q1.3Why do valleys and abutments leak?
A valley is the internal angle where two slopes meet, and it carries a great deal of water. Lead or mortar-bedded valley tiles fail quietly, and a stain on a bedroom ceiling is often the first sign. Flashings, the metal strips that seal a slope where it meets a wall or a chimney stack, loosen at the same time.
We list what we find against each part of the roof, so a repair covers the real fault and not just the nearest stain. Our page on roof repairs sets out how we decide.