Black diamond slate provides high quality slate roofing siding products at the best prices with a high level of customer service.
Black roof slates.
Keep the rain out and decorate your roof with style choosing from our wide collection of roof tiles and slate tiles.
Click and collect is available or enjoy free uk delivery on selected orders over pound 150 excl.
Weathering slates weathering slates will change color as they age with most weathering occurring in the first 1 to 3 years but can continue to change infinitely.
The manufacturers listed above are not available at all locations.
North country unfading black is a premium quality roofing slate offering an elegant and lasting roof for both new construction and restoration projects.
Slate is a fine grained foliated homogeneous metamorphic rock derived from an original shale type sedimentary rock composed of clay or volcanic ash through low grade regional metamorphism it is the finest grained foliated metamorphic rock.
Favorably compared to the famous slate of the monson region of maine this smooth rich black slate with a slight luster has earned the admiration of architects contractors and building owners.
Uk slate specialises in the supply of natural slate and stone products.
The light grey and black colors of the roof slates are equally as elegant depending solely on one s personal preference.
Natural slate roofing is one of the most stylish and stunning roofing materials available giving your home a unique and attractive finish whether it is a contemporary or modern style which is one of the main reasons it is so popular.
Slate is a timeless roof material allowing it to be used for both contemporary and more traditional period properties.
Our experienced staff can help you find the slate roofing product that fits your needs and budget.
Slate roof tiles manufacturers we carry.
Weathering slate provides the natural earth tones of bronze browns buffs cream colors which eventually become a blend on the roof.
Shop our roof slate other ranges today.
Foliation may not correspond to the original sedimentary layering but instead is in planes perpendicular to the direction of metamorphic compression.