Fast access to the families of these products: Limestone | Marble | Sandstone | Granite | Silica
The limestone rocks are not all as strong. According to their compositions, they are more or less permeable. Limestone is the largest sedimentary rock and is composed of at least 50% of calcite. The limestone is formed by the accumulation of fragments of skeletons or calcareous shells.
Champlain
Champlain meulé Listing details |
Champlain bouchardé Listing details |
Champlain éclaté Listing details |
Indiana Grey
Indiana Gris meulé Listing details |
Indiana Gris bouchardé Listing details |
Indiana Gris éclaté Listing details |
Golden Sand
Golden Sand meulé Listing details |
Golden Sand bouchardé Listing details |
Indiana Beige
Indiana Beige meulé Listing details |
Indiana Beige bouchardé Listing details |
Indiana Beige éclaté Listing details |
St-Marc
St-Marc meulé Listing details |
St-Marc bouchardé Listing details |
St-Marc éclaté Listing details |
According to geologists, the marble is a rock containing at least 50% of calcite or dolomite, which has undergone a transformation in the solid state as a result of an increase in temperature or increase pressure. An impurity during training gives it its color. This results in a material premium quality to the ornamentation.
White Marble
Marbre blanc meulé Listing details |
Marbre blanc bouchardé Listing details |
Marbre blanc éclaté Listing details |
Brown Marble (Eramosa)
Marbre brun (Éramosa) meulé Listing details |
Marbre brun (Éramosa) bouchardé Listing details |
Marbre brun (Éramosa) éclaté Listing details |
Cuban Marble
Marbre de Cuba meulé Listing details |
Marbre de Cuba bouchardé Listing details |
Marbre de Cuba éclaté Listing details |
Ontario Marble
Marbre d'Ontario meulé Listing details |
Marbre d'Ontario bouchardé Listing details |
Marbre d'Ontario éclaté Listing details |
Sandstone is a fragmental rock, porous, often linked, consisting of sand bound by a cement limestone.
Yellow Sandstone
Grès jaune meulé Listing details |
Grès jaune bouchardé Listing details |
Grès jaune éclaté Listing details |
Red Sandstone
Grès rouge meulé Listing details |
Grès rouge bouchardé Listing details |
Grès rouge éclaté Listing details |
Green Sandstone
Grès vert meulé Listing details |
Grès vert bouchardé Listing details |
Grès vert éclaté Listing details |
Granite is an igneous rock composed of very common crystals of varying size (feldspar is the most abundant up to 70%, quartz and black mica) that can distinguish to the naked eye. Granite is formed deep in the crust on Land from a bubble of magma subjected to temperature variations.
Winneway Granite Winneway Listing details |
Green Prairie Granite Vert Prairie Listing details |
Laurentian Green Granite Vert Laurentien Listing details |
Frost Green Granite Vert Givre Listing details |
Boreal Green Granite Vert Boreal Listing details |
Vermilion Granite Vermillion Listing details |
Tadoussac Granite Tadoussac Listing details |
Silver Cloud Granite Sylver Could Listing details |
Stanstead Granite Steanstead Listing details |
Santa Cecilia Granite Santa Cecillia Listing details |
Saint Sebastian Granite Saint Sébastien Listing details |
African Red Granite Rouge Africain Listing details |
Picasso Granite Picaso Listing details |
Peribonka Granite Péribonka Listing details |
Missouri Red Granite Misouri Red Listing details |
Milford Rose Granite Milford Rose Listing details |
Canadian Mahogany Granite Mahogany Canadien Listing details |
Kodiak Granite Kodiak Listing details |
Granville Granite Granville Listing details |
Birch Bark Granite Écorche de bouleau Listing details |
Dakota Mahogany Granite Dakota Mahogany Listing details |
Cambrian Granite Cambriand Listing details |
Caledonia Granite Calédonia Listing details |
Blue Pearl Granite Blue Pearl Listing details |
Autumn Brown Granite Automne Brun Listing details |
American Mist Granite American Mist Listing details |
It is a siliceous rock compact, smooth or finely conchoidal fracture splintery. The stone is made of silica quartz crystals welded together, often toothed and meshed.
