Rock Identifier
Schist (Chlorite-Mica Schist) — metamorphic
metamorphic

Schist

Chlorite-Mica Schist

Hardness: 3.5-5; Color: Greenish-gray with silver sheen; Luster: Pearly to sub-metallic; Crystal structure: Sheet-like (foliated); Cleavage: Perfect in one direction (slaty/schistose); Specific gravity: 2.7-2.9

Hardness
3
Color
Greenish-gray with silver sheen
Luster
Pearly to sub-metallic
Identified More metamorphic

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Physical properties

Hardness: 3.5-5; Color: Greenish-gray with silver sheen; Luster: Pearly to sub-metallic; Crystal structure: Sheet-like (foliated); Cleavage: Perfect in one direction (slaty/schistose); Specific gravity: 2.7-2.9

Formation & geological history

Formed through the regional metamorphism of shale or mudstone under intermediate to high temperatures and pressures, typically during orogenic (mountain-building) events.

Uses & applications

Historically used for flagstones, decorative building stone, and occasionally as a source of graphite or certain industrial minerals. Small river-tumbled pieces are primarily used for education or personal collections.

Geological facts

The word 'schist' is derived from the Greek word 'schizein', meaning 'to split', referring to the ease with which these rocks can be layered or split. It is often filled with accessory minerals like garnets or staurolite.

Field identification & locations

Identify by its distinct 'schistosity' or layered, glittery appearance. It is commonly found in crystalline basement rocks of mountain ranges like the Appalachians or the Alps. Look for the alignment of mica flakes which create its characteristic shine.