Rock Identifier
Likely tumbled lepidolite-bearing mica schist (Lepidolite-rich mica schist; chiefly lepidolite/muscovite mica, quartz, and possibly feldspar) — metamorphic
metamorphic

Likely tumbled lepidolite-bearing mica schist

Lepidolite-rich mica schist; chiefly lepidolite/muscovite mica, quartz, and possibly feldspar

AI-generated identification · may be incorrect

Lavender-gray, fine-grained and weakly reflective with a blocky tumbled shape; mica gives a pearly luster and Mohs hardness about 2.5–3, while quartz inclusions are harder (7). Exact identification is uncertain from the image alone.

Identified More metamorphic
Explore Likely tumbled lepidolite-bearing mica schist in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Lavender-gray, fine-grained and weakly reflective with a blocky tumbled shape; mica gives a pearly luster and Mohs hardness about 2.5–3, while quartz inclusions are harder (7). Exact identification is uncertain from the image alone.

Formation & geological history

A metamorphic rock formed when lithium-rich clay or granitic material was altered by heat and pressure, commonly in granite pegmatite zones; typically Precambrian to Phanerozoic depending on locality.

Uses & applications

Used mainly as a lapidary, decorative, or collector specimen; lepidolite is also a minor lithium source, but this small piece has no practical industrial value.

Geological facts

The purple color commonly comes from manganese in lepidolite mica, though purple quartz, fluorite, or dyed material can look similar.

Field identification & locations

Look for glittery, flaky mica layers, uneven cleavage, and a relatively soft surface; a streak, hardness, and acid test—or gemological analysis—would distinguish it from amethyst or fluorite. Common sources include Brazil, Madagascar, the United States, and Zimbabwe.