mineral

Likely polished copper-bearing mineral specimen (possibly chrysocolla with iron-oxide staining)

Chrysocolla, Cu₂H₂Si₂O₅(OH)₄·nH₂O; identification uncertain from image

AI-generated identification · may be incorrect

Rounded, apparently polished pebble with mottled orange-brown, cream, and dark patches. Chrysocolla is typically blue-green, Mohs 2–4, and has a vitreous to dull luster; the pictured colors may reflect iron oxides or another mineral, so hardness and composition cannot be confirmed visually.

Identified October 11, 2026More mineral →

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At a glance

Common name: Likely polished copper-bearing mineral specimen (possibly chrysocolla with iron-oxide staining)
Scientific name: Chrysocolla, Cu₂H₂Si₂O₅(OH)₄·nH₂O; identification uncertain from image
Category: mineral
Identified: October 11, 2026
Method: Standard

AI Estimated Value

About $2–$20 for a small, common polished specimen; more if verified and especially attractive.

Not an official valuation

AI estimate for general interest only — not an appraisal. Actual value depends on condition, provenance, and market demand. Verify with a professional before buying, selling, or insuring.

This identification was generated by AI and may contain errors. Verify important details before relying on them — and never use an AI result to judge whether a specimen is safe to handle. Read the full disclaimer

Physical properties

Formation & geological history

Chrysocolla forms as a secondary copper mineral in oxidized zones of copper deposits, commonly alongside iron oxides; these deposits range in age and occur in arid regions.

Uses & applications

Copper ores are used in electrical, construction, and industrial applications; attractive chrysocolla-bearing material is cut for cabochons and collected.

Geological facts

The image shows a small, rounded specimen with an orange, dark, and pale mottled surface; no diagnostic crystal structure is visible.

Field identification & locations

Copper minerals are commonly found in weathered copper deposits, including areas of the southwestern United States, Chile, and Peru. Confirm identity with a hardness, streak, or mineralogical test; the image alone is insufficient for a reliable field identification.