Rock Identifier
Tumbled feldspar-rich rock, possibly moonstone-bearing granite (Plagioclase feldspar (albite–oligoclase), with probable quartz and dark mica/amphibole; exact identification requires testing) — mineral
mineral

Tumbled feldspar-rich rock, possibly moonstone-bearing granite

Plagioclase feldspar (albite–oligoclase), with probable quartz and dark mica/amphibole; exact identification requires testing

AI-generated identification · may be incorrect

Hardness about 6–6.5 Mohs; gray-white with dark inclusions, vitreous to pearly luster, granular interlocking crystals, and no obvious cleavage visible in the rounded specimen. The silvery flash may indicate weak adularescence from moonstone feldspar.

Identified More mineral
Explore Tumbled feldspar-rich rock, possibly moonstone-bearing granite in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness about 6–6.5 Mohs; gray-white with dark inclusions, vitreous to pearly luster, granular interlocking crystals, and no obvious cleavage visible in the rounded specimen. The silvery flash may indicate weak adularescence from moonstone feldspar.

Formation & geological history

Likely crystallized slowly from silica-rich magma in a coarse-grained igneous body, potentially granite or pegmatite; such rocks commonly formed in Precambrian to Phanerozoic continental crust. Surface rounding appears human-produced by tumbling or natural abrasion.

Uses & applications

Used mainly as a teaching or collector specimen; feldspar-rich rocks are also used as aggregate, dimension stone, and ceramic/glass raw material. If genuine moonstone is present, cleaner translucent pieces may be cut for jewelry.

Geological facts

The image alone cannot distinguish moonstone from ordinary reflective feldspar, quartz, or mica. A glass-scratch test, streak, cleavage inspection, and close examination of the flash under changing light would improve identification.

Field identification & locations

Look for feldspar’s two cleavage directions, pale streak, hardness near 6, and blocky grains; quartz is harder and lacks cleavage. Comparable material occurs in granites and pegmatites worldwide, including India, Madagascar, Norway, and the United States.