Rock Identifier
Mottled purple-and-cream rough mineral specimen, likely lepidolite-bearing pegmatite (Probably lepidolite (lithium mica; K(Li,Al)₃(Si,Al)₄O₁₀(F,OH)₂) with light-colored quartz or feldspar; identification uncertain from image) — mineral
mineral

Mottled purple-and-cream rough mineral specimen, likely lepidolite-bearing pegmatite

Probably lepidolite (lithium mica; K(Li,Al)₃(Si,Al)₄O₁₀(F,OH)₂) with light-colored quartz or feldspar; identification uncertain from image

AI-generated identification · may be incorrect

Purple patches in a pale matrix; uneven, partly platy surface with a pearly to vitreous luster. Lepidolite is typically Mohs 2.5–4, monoclinic, with perfect basal cleavage; specimen hardness and specific gravity cannot be established visually.

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Physical properties

Purple patches in a pale matrix; uneven, partly platy surface with a pearly to vitreous luster. Lepidolite is typically Mohs 2.5–4, monoclinic, with perfect basal cleavage; specimen hardness and specific gravity cannot be established visually.

Formation & geological history

Lepidolite commonly crystallizes in lithium-rich granitic pegmatites as late-stage magma cools; such deposits span a wide range of geological ages.

Uses & applications

Lithium mica is collected as a mineral specimen and historically served as a minor lithium source; attractive pieces may be used decoratively, but this rough fragment is not visibly gem quality.

Geological facts

Lepidolite’s lilac-to-purple color is associated with trace manganese, and it commonly occurs with quartz, feldspar, and other lithium minerals.

Field identification & locations

The mottled color suggests a mica-bearing pegmatite, but a close inspection for tiny reflective mica flakes and laboratory testing would be needed to confirm the identification. Lepidolite-bearing pegmatites occur in regions including Brazil, Madagascar, and the United States.