Chapter 1: Why do the valleys on our Wentworth Estate house keep leaking?
What we find
A large house of the 1920s onward is rarely one simple pitch. It is made of several roofs meeting at angles, and wherever two slopes join there is a valley, a channel that carries the water of both slopes down to the gutter. Valleys on these houses are lined with lead or an older metal sheet, and the tile edges are bedded on either side. Lead splits where it has been bent repeatedly by heat and cold, and the tile cuts along the edge can slip or crack.
The giveaway is a stain on a ceiling below a roof junction rather than below a flat expanse of tiling. Pine needles and oak leaves bank up in a valley and hold water against the lead, which speeds up the corrosion. A valley on a shaded slope can also hold moss that dams the flow, so that water backs up under the tile edges instead of running away.
What we fix
We start with a close look at the valley from the roof and from the loft, because the stain inside is often a metre from the actual hole. Debris is cleared, the tile edges are checked, and small splits in sound lead can sometimes be repaired. Where the lead has crept, cracked along a fold or been patched before, a new valley lining is the lasting repair: the tiles each side are lifted, a new lead lining is laid on a fresh underlay with proper laps, and the tiles are cut and bedded back over it.
Lead is a skilled material and it pays to get the thickness and the laps right, so we explain on the survey photographs which option your valley needs. Our lead roofing and leadwork page sets out how that work is done. If the valleys are sound and only blocked, a clear-out and a tree-trimming recommendation may be all the roof needs.