

Descloizite specimens for sale
47 for sale · $50–$15,000 USD
104 in the gallery
Descloizite is a lead zinc vanadate hydroxide mineral that forms prismatic to tabular crystals, often with a resinous to adamantine lustre. Crystals can exhibit rich colors ranging from olive-yellow to brownish-yellow, and may occur in zoned aggregates or solo prisms set against contrasting matrix. The mineral commonly forms in secondary hydrothermal veins and near oxidized zones, with notable crystalline habits that reward careful cleaning and display.
- Formula
- PbZn(VO4)(OH)
- Rarity
- Rare
- Stability
- Moderately Stable
- Collector interest
- High Interest
Buy Descloizite specimens
View all 47Where Descloizite is found
Top localities
- Berg Aukas Mine37 specimens
- Sobral da Adiça37 specimens
- Erupción Mine6 specimens
- Aurora mine4 specimens
- Anarak District3 specimens
- Apache Mine3 specimens
- Oshikoto Region3 specimens
- Otjozondjupa Region3 specimens
- Tsumeb2 specimens
- Ajax Mine1 specimen
Guides
All guides


Descloizite from Berg Aukas Mine, Namibia
Berg Aukas descloizite is one of the great “species-defining” classics: the locality by which serious collectors judge descloizite. The best pieces have a sculptural, almost architectural presence—dark brown to nearly black spear-point cry…Read guideAbout Descloizite
Significant specimens come from Namibia, Portugal, the USA, Mexico and Iran, among other locales. Classic localities include the Zechstein and scattered carbonate veins where Descloizite crystals populate matrix-rich pockets, sometimes displaying attractive parallel growth or twinned forms. High-quality material showcases vibrant color and crisp termination, making aesthetically compelling assemblages for collectors who appreciate horn-like luster and mineral diversity.
Collectors value Descloizite for its combination of color, crystal form, and locality association. The mineral’s varied habit and historically important collecting sites enhance its appeal as a specimen for cabinet displays and reference collections alike, offering a tangible link to hydrothermal processes and ore-oreite environments.





















