Living at 260 metres: what the exposure does
Height above the surrounding country puts more load on every fixing than the same house would carry in a sheltered street.
A roof in a lowland street is shielded on most sides. A roof near the summit of the Mendips is not. The wind meets the slope square on, rain is driven up the covering rather than falling straight down it, and a wet, cold winter at that height is hard on any covering. None of that is dramatic in a single season. It shows up over time, as small movements that eventually let water through.
The first place to look is the fixing. Slates and tiles are held by nails or clips, and a corroded nail gives way long before the slate beneath it has worn out. On an exposed slope, a slate that has lost its nail will slide and then lift, and the courses around it take extra wind as a result. Our approach is to find out whether the failure is local or general. A few slipped slates on an otherwise sound roof can be refixed with a tingle, a thin lead or copper tab bent up under the tail of the slate. A roof showing the same loose pattern on every slope has reached the end of its fixings.
The next layer matters just as much. Underlay is a sheet draped over the rafters and held down by the battens, the cross-timbers that the slates or tiles hang from. It catches wind-blown rain and leads it to the gutter. On a high roof, rain is pushed past the joints more often, so a torn or brittle underlay shows itself through stained rafters and a damp loft long before any tile looks wrong from the ground.
Ridge and verge details deserve the same scrutiny. The 2014 edition of BS 5534 rules out mortar as the sole fixing for ridge and hip tiles, so repairs and new coverings add a clip or screw. A dry-fix ridge or verge, clipped and capped instead of bedded, is tested to BS 8612:2018, and it suits a gale-prone position well. The pitched roofing service covers the roof as a whole, from the timbers to the ridge line.



