Slates are the foliated fine granular natural stones which low-grade metamorphism of shale or clay stones. Metamorphism realized as the result of high pressure occured from the collosion of tectonic plates. Foliation of slate stones are not happen from the stratification or the foliation of shale or clay stones; foliation event on slate stones happen perpendicular to high pressures which are forming metamorphism process.
Slate stones are formed with the exposure degree of metamorphism of clay or mica minerals which they consist. As the result of increase in the pressure and heat the minerals in the shale transform into mica minerals. Slate stones also consist high amount of quartz minerals and small amount of feldspar, calcite, pyrite and hematite minerals in their structure.
Slate stones are-nonporous and resistant to negative weather conditions and abrasion. They have durable structure for shrinking and bending. Un-slippery characteristic of slate stones make them ideal for slippery grounds. They are also irresponsive to temperature differences and frost. Today slate stones mostly prefered as cut-to-size or natural state in outdoor applications like aesthetic coating materials, window edges, thresholds and floorings.
Slates have various colours depending on structures of minerals that they contain. In nature slates can be find yellow, brown, grey, light green, off-white, claret red, red or multicolor.
Slate stones are marketed as natural state; no surface treatment are made.