Pizarras los Templarios S.A.
Sotillo de Cabrera (León)

This deposit belongs to the "Agüeria" formation (Medium - Upper Ordovician). A slow grade regional metamorphic process related to the first Hercinic phase formed the slate of this quarry.

It is a black slate of fine grain presenting very light lineation. Its main minerals are sericite, chlorite and quartz, with very few metals present. It has a very good cut, solidity and resistance to flexion and to environmental aggressions. It is a superb slate.

The slate is produced in sizes from 22 x 16 cm to 40 x 22 cm, the most common size is 32 x 22 cm, with a thickness of 2,5 mm / 4 mm. The reference name is RF-40.

The physical-chemical characteristics of this slate makes it very good for all building applications being an excellent performer in any climate zone.