Rock Identifier
Greenstone (likely serpentinite or greenstone pebble) (Serpentinite-rich ultramafic rock; commonly dominated by serpentine-group minerals, with possible chlorite, actinolite, or magnetite) — metamorphic
metamorphic

Greenstone (likely serpentinite or greenstone pebble)

Serpentinite-rich ultramafic rock; commonly dominated by serpentine-group minerals, with possible chlorite, actinolite, or magnetite

AI-generated identification · may be incorrect

Fine-grained, rounded and polished naturally; mottled gray-green color with dull to waxy luster. Typical hardness is about 2.5–5.5 Mohs, with no visible cleavage and variable specific gravity around 2.5–2.8.

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Physical properties

Fine-grained, rounded and polished naturally; mottled gray-green color with dull to waxy luster. Typical hardness is about 2.5–5.5 Mohs, with no visible cleavage and variable specific gravity around 2.5–2.8.

Formation & geological history

Likely formed by hydration and low-temperature metamorphism of mantle-derived peridotite, commonly in oceanic crust or tectonic suture zones. Serpentinite ranges from ancient Precambrian to geologically recent formations.

Uses & applications

Used as decorative stone, carvings, tumbled specimens, aggregate, and occasionally architectural stone; attractive pieces have modest lapidary value.

Geological facts

The green color commonly comes from serpentine minerals and iron-bearing alteration products. Magnetite may make some specimens weakly magnetic.

Field identification & locations

Identify by its green mottling, soft-to-medium hardness, waxy feel, and tendency to scratch with steel; vinegar produces no reaction. Common sources include California, Italy, New Zealand, Canada, and Japan.