Rock Identifier
Likely tumbled pale-green mineral specimen (Indeterminate; possibly serpentine, calcite, or pale jade/nephrite) — mineral
mineral

Likely tumbled pale-green mineral specimen

Indeterminate; possibly serpentine, calcite, or pale jade/nephrite

AI-generated identification · may be incorrect

Opaque cream-to-pale-green, matte to weakly waxy luster, fine-grained appearance, and rounded rectangular shaping. Hardness cannot be determined reliably from the image: calcite is Mohs 3, serpentine 2.5–4, and nephrite 6–6.5.

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Physical properties

Opaque cream-to-pale-green, matte to weakly waxy luster, fine-grained appearance, and rounded rectangular shaping. Hardness cannot be determined reliably from the image: calcite is Mohs 3, serpentine 2.5–4, and nephrite 6–6.5.

Formation & geological history

The specimen appears cut or polished from a natural mineral, but its geological origin and age cannot be established visually. Serpentine forms by hydrothermal alteration of ultramafic rocks; calcite commonly precipitates in veins and sedimentary settings; jade forms in high-pressure metamorphic environments.

Uses & applications

Small pieces may be used for carving, lapidary practice, décor, or collecting; only confirmed high-quality jade has substantial jewelry value.

Geological facts

The block-like shape and uniform surface may also indicate a processed mineral sample rather than a natural crystal. Identification requires hardness, streak, specific-gravity, and possibly refractive-index testing.

Field identification & locations

Check translucency, streak, and hardness: calcite scratches easily and fizzes in dilute acid, serpentine is softer with a waxy feel, while nephrite is notably tough and resists scratching. Common source regions include Italy, the United States, Canada, China, and New Zealand, depending on composition.