Rock Identifier
Slate (Slate (Foliated Metamorphic Rock)) — metamorphic
metamorphic

Slate

Slate (Foliated Metamorphic Rock)

Hardness: 2.5-4 Mohs; Color: Gray, black, or earthy tones; Luster: Dull to satiny; Structure: Foliated (slaty cleavage); Cleavage: Perfect planar cleavage.

Hardness
2
Color
Gray, black, or earthy tones
Luster
Dull to satiny
Identified More metamorphic
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Physical properties

Hardness: 2.5-4 Mohs; Color: Gray, black, or earthy tones; Luster: Dull to satiny; Structure: Foliated (slaty cleavage); Cleavage: Perfect planar cleavage.

Formation & geological history

Formed through low-grade metamorphism of shale or mudstone under relatively low pressure and temperature conditions. It is typically associated with regional metamorphism during mountain-building events.

Uses & applications

Used for roofing shingles, flooring tiles, billiard table tops, blackboards, and garden landscaping.

Geological facts

Slate is unique because it can be split into very thin, flat sheets. Some of the world's most famous slate comes from Wales, UK, and the Slate Valley of Vermont/New York.

Field identification & locations

Identified in the field by its ability to split into thin sheets and its distinct 'clink' sound when struck. Found in mountainous or formerly mountainous regions globally.