
Vermont, Buckingham, Peach Bottom and Pennsylvania. Knowing which quarry the original roof came from is half of getting the match right.
Vermont and New York produced the unfading and semi-weathering greens, purples, reds and mottled ranges. Buckingham County, Virginia produced the dense blue-black that never fades. Peach Bottom, on the Pennsylvania–Maryland line, produced a hard blue-black now long out of production. The Pennsylvania soft-vein belt produced the grey-black slate found on a great many ordinary period houses.
Unfading slate holds its quarry colour for the life of the roof. Semi-weathering slate is meant to change—greens drift to buff and tan over decades, which is exactly why a fresh semi-weathering green will not match an eighty-year-old semi-weathering green field until it has had a decade of its own.
Construction date, region, the colour of a freshly broken edge versus the weathered face, and thickness. Send us a piece and we will tell you what we think it is.
Call 225-954-8393 and describe the roof. We will tell you what is realistic.