Rock Identifier
Tumbled green feldspar or serpentine (Likely microcline feldspar (KAlSi₃O₈) or green serpentine-group mineral; exact identification requires testing) — mineral
mineral

Tumbled green feldspar or serpentine

Likely microcline feldspar (KAlSi₃O₈) or green serpentine-group mineral; exact identification requires testing

AI-generated identification · may be incorrect

Opaque blue-green to yellow-green, waxy to slightly vitreous luster, rounded by tumbling, with mottled color and possible pale feldspar veins. Estimated hardness is about 2.5–6 Mohs depending on composition; no crystal faces are visible.

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Physical properties

Opaque blue-green to yellow-green, waxy to slightly vitreous luster, rounded by tumbling, with mottled color and possible pale feldspar veins. Estimated hardness is about 2.5–6 Mohs depending on composition; no crystal faces are visible.

Formation & geological history

Green feldspar forms in potassium-rich igneous and metamorphic rocks, while serpentine forms when ultramafic mantle rocks undergo hydration; ages vary widely by locality. The specimen has been human-polished/tumbled.

Uses & applications

Used as an inexpensive decorative stone, cabochon, craft material, or collector specimen; serpentine is also used ornamentally in carvings and tiles.

Geological facts

The image alone cannot reliably distinguish green feldspar from serpentine, jade-like rocks, or dyed material. It does not show the translucency or fibrous texture typical of high-quality jadeite.

Field identification & locations

Check hardness, streak, density, and reaction to dilute acid; feldspar commonly scratches glass weakly, whereas serpentine is much softer. Common sources include India, China, Russia, Canada, and the western United States.