Rock Identifier
Likely biotite mica in a host rock (Biotite, a dark mica-group mineral; composition varies, broadly K(Mg,Fe)₃AlSi₃O₁₀(F,OH)₂) — mineral
mineral

Likely biotite mica in a host rock

Biotite, a dark mica-group mineral; composition varies, broadly K(Mg,Fe)₃AlSi₃O₁₀(F,OH)₂

AI-generated identification · may be incorrect

Dark brown to black, shiny platy surfaces and pronounced sheet cleavage are visible; Mohs hardness 2.5–3, monoclinic crystal system, specific gravity about 2.7–3.3. The image is too close and indistinct to identify the host rock confidently.

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Physical properties

Dark brown to black, shiny platy surfaces and pronounced sheet cleavage are visible; Mohs hardness 2.5–3, monoclinic crystal system, specific gravity about 2.7–3.3. The image is too close and indistinct to identify the host rock confidently.

Formation & geological history

Biotite crystallizes in many igneous and metamorphic rocks as magma cools or during metamorphism; its age depends on the host and may range from recent to billions of years.

Uses & applications

Used chiefly as a geological indicator and collector mineral; mica also has industrial uses as an insulating and filler material, though biotite is less commonly used than lighter mica.

Geological facts

Mica splits into thin, flexible sheets because of its perfect basal cleavage.

Field identification & locations

Look for dark, reflective flakes that peel into sheets; common in granite, schist, and gneiss worldwide. The green patch and surrounding material are not clear enough here to identify reliably.