Rock Identifier
Mica (likely biotite-rich mica aggregate) (Biotite, a potassium–iron–magnesium mica; approximate formula K(Mg,Fe)₃AlSi₃O₁₀(F,OH)₂) — mineral
mineral

Mica (likely biotite-rich mica aggregate)

Biotite, a potassium–iron–magnesium mica; approximate formula K(Mg,Fe)₃AlSi₃O₁₀(F,OH)₂

AI-generated identification · may be incorrect

Brown, shiny, flaky sheets with perfect basal cleavage and a platy, layered structure; Mohs hardness about 2.5–3. The small specimen’s exact mineral identity cannot be confirmed from the image alone.

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Physical properties

Brown, shiny, flaky sheets with perfect basal cleavage and a platy, layered structure; Mohs hardness about 2.5–3. The small specimen’s exact mineral identity cannot be confirmed from the image alone.

Formation & geological history

Mica forms in igneous and metamorphic rocks as magma cools or during recrystallization under heat and pressure; biotite is found in rocks spanning a wide range of geological ages.

Uses & applications

Mica is used as an electrical and thermal insulator, in fillers and cosmetics, and as a collector specimen; this small piece is mainly of educational or decorative interest.

Geological facts

Mica’s layers split into thin, flexible sheets, a property that made it useful in early electrical equipment and stove windows.

Field identification & locations

The glittering brown plates and sheet-like cleavage suggest mica; biotite commonly occurs in granite, schist, and gneiss worldwide. Confirming biotite rather than another mica requires closer examination.