Chrysocolla, Azurite, and Malachite Point · 17×10 mm

Chrysocolla, Azurite, and Malachite Point from Kaokoveld (Namibia), 17×10×6 mm. Sky blue chrysocolla, deep blue azurite, and intense green malachite all in one piece, with brown iron oxide inclusions. Hand-carved in our lapidary workshop.

Piece Details

This particular piece

The distribution of the three minerals in this point creates a map of colors: the sky blue of chrysocolla occupies the widest areas, the dark blue of azurite appears in compact patches, and the green of malachite emerges in veins and thin bands.

With a length of 17 mm and a base of 10×6 mm, the point has an organic proportion that does not follow any regular geometric axis —a reflection of the natural structure of the mineral aggregate from which it was carved.

How this mineral mix is formed

Chrysocolla, azurite, and malachite are secondary copper minerals: they all form in the oxidation zone of copper sulfide deposits (chalcopyrite, bornite) when water and CO₂ from the air react with the primary sulfides.

What mounting works for this

• Closed bezel setting (925 silver or other precious metals) — protects the edges of the three minerals, which have different hardnesses (chrysocolla is the softest). A silver bezel with a rustic finish complements the organic nature of the piece well.
• Pendants with copper mounting — metallic copper has narrative consistency with the minerals in the piece (all are copper silicates or carbonates) and adds warmth to the blue-green.
• Wire wrap with copper or silver wire — works well for those who work with wire; allows for a presentation that leaves the organic profile of the point visible.

Copper minerals in lapidary tradition

Azurite was the most important blue pigment in Europe before the synthesis of Prussian blue: it was ground to make pigment for medieval and Renaissance paintings (the "German blue" or "azzurro della Magna" of 15th-century Italian painting recipes). Malachite was the equivalent green pigment.

The symbolic properties attributed to minerals belong to cultural and historical traditions. They are shared for educational purposes, not as medical advice or a substitute for professional care.

How to recognize this genuine mineral mix

Genuine chrysocolla is opaque or semi-opaque and has a variable blue, never uniform. Genuine azurite has a darker, richer blue than any dye. Malachite has concentric or radial green bands visible under magnification.

Frequently Asked Questions

Have the minerals been treated?

No. The colors —blue, green, brown— are natural to each mineral phase. No detectable treatment. Statement based on lapidary observation; the piece does not include formal gemological certification.

What setting do you recommend for this point?

We recommend a closed bezel setting. With three minerals of slightly different hardnesses (3.5–4 Mohs), the edges in transition zones between phases are particularly vulnerable to scratches and impacts. The bezel protects them uniformly.

What is the difference between chrysocolla, azurite, and malachite?

All three are secondary copper minerals. Chrysocolla (sky blue, opaque, silicate) is the softest. Azurite (dark blue, carbonate) is slightly harder. Malachite (green, carbonate) is the most common of the three and exhibits characteristic banding.

Is the piece unique?

Yes. The distribution of colors and phases in this point is unrepeatable. Dimensional tolerance ±0.5 mm.

What are the dimensions?

17×10×6 mm. Tolerance ±0.5 mm in any dimension due to being hand-carved.

How do I care for it?

Clean only with a dry cloth. No water, soap, or chemicals —azurite and malachite react with acids, even mild ones. Store in an individual padded case. More information: jewelry care guide.

See also: complete lapidary collection · rough minerals.