Ross-on-Wye roofs, specifically
Why Ross-on-Wye roofs green up faster than the higher, drier ground around them.
Ross-on-Wye sits on a red-sandstone promontory, the town's name itself coming from a Celtic word for a spur of high ground, with St Mary's spire crowning the bluff and the streets falling away on every side toward the River Wye. It is a beautiful position — The Prospect, John Kyrle's public garden of 1696, looks out over the famous horseshoe bend in the river — but it is also a position that wrecks roofs. The bluff drops steeply to the river and the wide Wye floodplain below it, so the pitches on the lower, steeper streets sit in each other's shade for much of the day, and the river throws up mist and damp air that settles over the town. Moss, lichen and gloeocapsa algae live on exactly that combination of shade and moisture, so a roof here carries noticeably more growth than an identical house up on the drier, more open farmland inland.
You see it most starkly down in the old town. The tight pattern of the High Street, Broad Street, Church Street and Wye Street is packed with tall period properties standing shoulder to shoulder, many of them red-sandstone or brick under natural slate. They shade each other for most of the day, the streets are narrow enough that very little direct sun reaches the lower slopes, and the low ground beside the river floods — the December 2000 floods put the low-lying land along Wilton Road under water, and the town has since had a flood-alleviation scheme on the brooks that run through it. Left for a few winters, a north-facing slate pitch in one of those streets turns into a thick mat of moss sitting in the laps, with rust weeping off old valley metal and gutters packed with washed-down growth.
The river itself is the constant. The Wye loops right around the foot of the town, and even in a dry summer that body of water keeps the air around Ross heavy with moisture. Damp air is what the growth feeds on, and the shaded lower slopes mean the roofs never properly dry out between wet spells. It is a genuinely different microclimate to the open countryside a few miles away — the same house, the same slate, greens up faster here because of where it sits.
Out on the edges of town the roof changes but the problem doesn't. Tudorville, Overross and the Ashburton side, and the newer infill toward Wilton, are mostly post-war and modern concrete interlocking tile. Its rough, sandy face holds on to spores, and in damp valley air it mats up thickly, so the bulk comes off first, with a low-pressure clean or by hand from a tower or roof ladder, before the biocide goes on. A listed sandstone house below the spire and a 1990s semi on the Overross edge are green for the same reason: the damp of the Wye valley.
The one thing that genuinely changes the job in Ross is how much of the town is heritage. The conservation area, first designated in 1970 and extended in 1976, covers most of the old town, and it holds around 154 listed buildings — three of them Grade I. That means an unusually high share of the roofs we quote on are natural slate or old hand-made clay on fragile red-sandstone structures, and those simply cannot be pressure-washed. Blasting splits the slate, strips the surface and drives water under the laps into a building that has stayed watertight for centuries by being left alone. So on Ross's heritage roofs we clean at low pressure and remove the moss by hand, working off a roof ladder that spreads the load, and then treat with biocide. It is slower than blasting a modern tile, but on a slate roof that costs a fortune to re-cover, careful is the whole point.