Rock Identifier
Likely graphite-rich schist (Graphite-bearing schist, composed mainly of graphite with possible mica and quartz) — metamorphic
metamorphic

Likely graphite-rich schist

Graphite-bearing schist, composed mainly of graphite with possible mica and quartz

AI-generated identification · may be incorrect

Dark gray to black, shiny and strongly foliated with flaky or wrinkled surfaces; graphite is very soft (Mohs 1–2) and leaves a dark mark, while mica-rich grains may be harder. The photo alone cannot confirm the mineral composition or identify the shiny grains.

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Physical properties

Dark gray to black, shiny and strongly foliated with flaky or wrinkled surfaces; graphite is very soft (Mohs 1–2) and leaves a dark mark, while mica-rich grains may be harder. The photo alone cannot confirm the mineral composition or identify the shiny grains.

Formation & geological history

Formed when carbon-rich sedimentary rock was metamorphosed under heat and pressure, aligning platy minerals into foliation; age depends on the local geologic setting.

Uses & applications

Graphite-bearing rock may be collected as a specimen; graphite is used in pencils, lubricants, batteries, and refractory materials. Schist can also be used as decorative or building stone.

Geological facts

Graphite’s metallic-looking sheen can resemble sulfide minerals, but graphite is notably soft and often marks paper.

Field identification & locations

Look for flaky foliation and test a small surface for a dark, slippery mark; graphite-rich schist occurs in metamorphic belts worldwide. Confirmatory testing or a closer view would be needed to distinguish it from other shiny schists or ore minerals.