Rock Identifier
Mica Schist (Metamorphic rock dominated by mica minerals) — metamorphic
metamorphic

Mica Schist

Metamorphic rock dominated by mica minerals

Hardness of 3-4 on the Mohs scale, silvery-gray to brown color, pearly or metallic luster due to abundant mica flakes, foliated crystal structure with prominent schistosity, excellent cleavage along planes, specific gravity around 2.7-2.9

Identified More metamorphic
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Physical properties

Hardness of 3-4 on the Mohs scale, silvery-gray to brown color, pearly or metallic luster due to abundant mica flakes, foliated crystal structure with prominent schistosity, excellent cleavage along planes, specific gravity around 2.7-2.9

Formation & geological history

Formed through regional metamorphism of argillaceous rocks like pelitic clay and shale, typically occurring during mountain-building events (orogenies) at elevated temperatures and pressures.

Uses & applications

Used primarily in decorative garden stone, as a source of scrap mica, sometimes in construction fill, and popular in geological education and specimen collecting.

Geological facts

The prominent shimmering appearance is caused by the alignment of reflective muscovite or biotite mica crystals perpendicular to the direction of maximum principal stress.

Field identification & locations

Easily identified in the field by its distinct foliation and sparkly, sheet-like mica minerals covering the cleavage surfaces. Found globally in ancient mountain belts and shield areas.