Chrysocolla

Crystal system · Orthorhombic

Chrysocolla is a silicate mineral prized by collectors for its exceptional color range, with notable Chinese occurrences.

Chrysocolla specimen
Photo: Robert M. Lavinsky · CC BY-SA 3.0 via Wikimedia Commons

Chrysocolla is a blue-green copper silicate, a popular ornamental and collector mineral from oxidised copper deposits worldwide, including Bisbee and the Congo.

About Chrysocollaextended article

Chrysocolla is a hydrous copper silicate valued for its vivid blue-to-green colour. It often forms botryoidal crusts and is frequently intergrown with quartz (gem chrysocolla chalcedony) or malachite.

Where it comes from

Fine chrysocolla comes from oxidised copper orebodies worldwide — Bisbee in Arizona, the Katanga Copperbelt in the DR Congo, and many others.

What collectors look for

Intense blue-green botryoidal chrysocolla, and gem chrysocolla-in-chalcedony, are the most prized; colour and polish potential drive value.

About Chrysocolla

Chrysocolla belongs to the silicate class in the chrysocolla group and has the chemical formula Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1. It crystallizes in the orthorhombic system and is one of the most visually varied minerals in the collector market. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.

Identification & care

Specimens usually show cryptocrystalline to amorphous botryoidal, stalactitic, and crusty aggregates; true crystals extremely rare (acicular to fibrous). Its color range is broad, including green, bluish-green, blue, blackish-blue, and rarely brown or yellow. The luster is vitreous, waxy, earthy, the streak is light green, and specimens are typically translucent, opaque. The cleavage is none observed. The fracture is irregular/uneven, sub-conchoidal, which aids identification.

Collector context

How it forms

The geological setting for Chrysocolla is typically secondary mineral in oxidized zones of copper deposits; often coats and replaces primary copper minerals; forms with malachite, azurite, and other copper secondaries. It is commonly found in association with malachite, azurite, cuprite, tenorite, turquoise, quartz.

Classic Chinese localities

Jiama Cu-polymetallic deposit is an important Chinese source for the species.

Why collectors care

Chrysocolla is a frequently-sought species in serious collections because its habit is recognizable, its color often strong, and its best examples unmistakable even at a distance. Chinese material has driven much of the recent visual shift in the species — sharper crystals, deeper colors, cleaner matrix.

What affects value

Value in Chrysocolla is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.

Naming history

The name Chrysocolla has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.

Recently sold Chrysocolla specimens

1 example — for reference