Slate is a metamorphic rock formed from clay and mud deposits, transformed under heat and pressure so that it splits along one plane into thin, flat sheets. That cleavage — not the colour or the hardness — is the property on which every building application rests.

The original sediment was compressed within the earth’s crust, and the platy minerals in it (mainly clay minerals that recrystallised into mica and chlorite) all lined up in the same direction. This produces the slaty cleavage, which need not coincide with the original bedding of the sediment.

Characteristics

Applications

Quality and standard

Slate for roofing is covered by the European standard EN 12326, which sets requirements for bending strength, water absorption and behaviour in thermal-cycle and sulphur dioxide tests, among others. A key selection criterion is the pyrite content: pyrite (iron sulphide) in the slate can oxidise in the presence of moisture and cause rust staining or even pitting. A high carbonate content is likewise unfavourable, because it leaches under acid rain.

Practical tips

Related terms

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