mineral

Likely dyed or naturally vivid-blue copper mineral specimen

Possibly chrysocolla (hydrated copper silicate); image alone cannot confirm the mineral or whether the color is treated

AI-generated identification · may be incorrect

Bright blue, rough and porous with an earthy-to-vitreous luster; hardness and crystal structure cannot be determined visually. Chrysocolla is typically soft (about 2–4 Mohs) and lacks distinct cleavage.

Identified October 1, 2026More mineral →

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At a glance

Common name: Likely dyed or naturally vivid-blue copper mineral specimen
Scientific name: Possibly chrysocolla (hydrated copper silicate); image alone cannot confirm the mineral or whether the color is treated
Category: mineral
Identified: October 1, 2026
Method: Standard

AI Estimated Value

About $2–$15 for a small common rough specimen; treated or unidentified pieces may be worth less.

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 in oxidized zones of copper deposits as a secondary mineral; its age depends on the host deposit. Similar-looking blue copper minerals or dyed material are also possible.

Uses & applications

Copper minerals are collected and sometimes used as ornamental stone; softer chrysocolla may be stabilized for jewelry. This small rough piece is mainly a display or teaching specimen.

Geological facts

Chrysocolla commonly occurs with malachite, azurite, and quartz, and its color can range from turquoise to deep blue-green.

Field identification & locations

Check for color transfer, dye concentrated in cracks, and hardness before identifying; copper-bearing minerals often occur in arid-region oxidized ore zones. A definitive ID requires testing or laboratory analysis.