Descloizite

Descloizite specimens for sale

50 for sale · $50–$15,000 USD

183 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
Classification notes
Vanadate; adelite-descloizite group

Key characteristics

Crystal system
orthorhombic
Mohs hardness
3–3.5
Specific gravity
6.18–6.22
Luster
vitreous, resinous, greasy
Transparency
translucent, opaque
Color
brown, red, orange, yellow, green, black
Streak
yellow, orange, brown
Cleavage
none
Fracture
conchoidal, uneven
Crystal habit
prismatic, pyramidal, tabular, druzy, granular, massive
  • Classic / historic

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Where Descloizite is found

Top localities

  1. Berg Aukas Mine22 specimens
  2. Erupción Mine7 specimens
  3. Aurora mine4 specimens
  4. Apache Mine3 specimens
  5. Ahumada Mine2 specimens
  6. Aurora Mine2 specimens
  7. Los Lamentos Mts2 specimens
  8. Ajax Mine1 specimen
  9. Anarak District1 specimen
  10. Bustillos mine1 specimen

About 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.