Rock Identifier
Tumbled greenstone, likely serpentine or altered basalt (Serpentine-group minerals, chiefly Mg₃Si₂O₅(OH)₄; possibly chlorite/epidote-bearing mafic rock) — metamorphic
metamorphic

Tumbled greenstone, likely serpentine or altered basalt

Serpentine-group minerals, chiefly Mg₃Si₂O₅(OH)₄; possibly chlorite/epidote-bearing mafic rock

AI-generated identification · may be incorrect

Olive-green to gray-green, fine-grained, matte to weakly waxy luster, rounded by tumbling; estimated Mohs hardness 3–6 depending on composition. No visible crystals or cleavage are apparent; specific gravity is roughly 2.6–3.2.

Identified More metamorphic
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Physical properties

Olive-green to gray-green, fine-grained, matte to weakly waxy luster, rounded by tumbling; estimated Mohs hardness 3–6 depending on composition. No visible crystals or cleavage are apparent; specific gravity is roughly 2.6–3.2.

Formation & geological history

Most likely formed by hydrothermal metamorphism of ultramafic or mafic rock, with alteration of olivine and pyroxene; age cannot be determined from the photograph. It may also be a small altered basalt or greenstone pebble.

Uses & applications

Used as a decorative tumbled stone, carving material, lapidary cabochon, and occasionally ornamental building stone; typically not valuable as jewelry-grade material.

Geological facts

The term “greenstone” is descriptive rather than a single mineral name. Serpentine can resemble jade, but it is generally softer and less durable.

Field identification & locations

Look for olive coloration, mottled texture, waxy feel, and relatively low hardness; a steel knife may scratch serpentine but not jade. Common sources include serpentinite belts and metamorphic terrains worldwide.