Rock Identifier
Gold-colored mineral specimen, likely pyrite or weathered mica schist (Tentatively pyrite (FeS₂); identification is uncertain from the obscured image) — mineral
mineral

Gold-colored mineral specimen, likely pyrite or weathered mica schist

Tentatively pyrite (FeS₂); identification is uncertain from the obscured image

AI-generated identification · may be incorrect

Brassy yellow color and metallic-looking luster suggest pyrite, Mohs hardness 6–6.5, cubic crystal structure, and poor cleavage. If flaky and easily split into sheets, it may instead be biotite mica in schist; mica has Mohs hardness 2.5–3 and perfect basal cleavage.

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Physical properties

Brassy yellow color and metallic-looking luster suggest pyrite, Mohs hardness 6–6.5, cubic crystal structure, and poor cleavage. If flaky and easily split into sheets, it may instead be biotite mica in schist; mica has Mohs hardness 2.5–3 and perfect basal cleavage.

Formation & geological history

Pyrite forms in hydrothermal veins and sedimentary or metamorphic rocks; mica schist forms when clay-rich sediments undergo regional metamorphism. Ages vary widely by locality, commonly Precambrian to younger.

Uses & applications

Pyrite is collected and historically mined for sulfur and minor metals; mica is used in electrical insulation, fillers, and cosmetics. Neither is typically used as a gemstone except in decorative specimens.

Geological facts

Pyrite is commonly called “fool’s gold,” but it is harder and more brittle than true gold. Gold is malleable and leaves a yellow streak, whereas pyrite produces a dark greenish-black streak.

Field identification & locations

Test streak on unglazed porcelain, hardness, brittleness, and crystal shape; avoid relying on color alone. Common localities include Peru, Spain, Italy, China, and the United States.