Rock Identifier
Weathered greenish-gray rock fragment, likely chlorite-rich schist (Tentatively chlorite schist; exact identification requires closer examination) — metamorphic
metamorphic

Weathered greenish-gray rock fragment, likely chlorite-rich schist

Tentatively chlorite schist; exact identification requires closer examination

AI-generated identification · may be incorrect

Fine-grained, pale green-gray, dull to slightly sparkly, with a foliated or layered texture. Likely hardness around 2–4 Mohs if chlorite-rich; crystal structure and specific gravity cannot be determined reliably from the image.

Identified More metamorphic →
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Physical properties

Fine-grained, pale green-gray, dull to slightly sparkly, with a foliated or layered texture. Likely hardness around 2–4 Mohs if chlorite-rich; crystal structure and specific gravity cannot be determined reliably from the image.

Formation & geological history

Likely formed when clay-rich sediment or volcanic rock was metamorphosed at low grade, producing aligned chlorite and other minerals. Its age and precise formation environment cannot be determined from appearance alone.

Uses & applications

This small fragment has no evident commercial use; schist may be used locally as building or landscaping stone, and attractive pieces may be collected.

Geological facts

Green color can result from chlorite, but several other minerals and weathering can produce a similar appearance.

Field identification & locations

Look for thin, aligned mineral layers and a tendency to split along them; a fresh surface and magnification would help distinguish schist from altered volcanic rock. Schists occur in metamorphic belts worldwide.