Rock Identifier
Lepidolite (K(Li,Al)3(Si,Al)4O10(F,OH)2) — mineral
mineral

Lepidolite

K(Li,Al)3(Si,Al)4O10(F,OH)2

AI-generated identification · may be incorrect

Lepidolite has a Mohs hardness of 2.5 to 4, a pearly to vitreous luster, and a distinct lilac to rose-gray color. It exhibits perfect basal cleavage, yielding flexible thin sheets, and crystallizes in the monoclinic system.

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Physical properties

Lepidolite has a Mohs hardness of 2.5 to 4, a pearly to vitreous luster, and a distinct lilac to rose-gray color. It exhibits perfect basal cleavage, yielding flexible thin sheets, and crystallizes in the monoclinic system.

Formation & geological history

Lepidolite forms in granite pegmatites and high-temperature quartz veins through the hydrothermal alteration of lithium-bearing minerals.

Uses & applications

It serves as a primary ore of the alkali metal lithium and is frequently cut into cabochons or collected as mineral specimens.

Geological facts

Because of its high lithium content, lepidolite is structurally related to micas and often occurs alongside tourmaline and spodumene in pegmatite pockets.

Field identification & locations

Field identification relies on its characteristic lilac-pink color, micaceous flaky cleavage, and association with pegmatite zones. Common localities include Brazil, Madagascar, and the United States.