Olivenite specimens for sale

157 for sale · $75–$12,500 USD

66 in the gallery

Olivenite is a copper arsenate mineral that forms as green to olive-brown, often vitreous to pearly crystals. It typically occurs as prismatic, elongated crystals or radiating clusters and can display a resinous to sub-metallic luster. The mineral commonly appears in hanging or fibrous aggregates within fissures of copper-bearing rocks, frequently alongside secondary copper minerals that form in oxidative zones.

Formula
Cu2(AsO4)(OH)
Rarity
Common
Stability
Stable
Collector interest
Moderate Interest
Classification notes
Arsenate mineral; Cu-arsenate hydroxide, Strunz 08.BA.05

Buy Olivenite specimens

View all 157
Olivenite image
Olivenite
Crystal Classics
Listed 3d ago
$1,750
Olivenite image
Olivenite
Crystal Classics
Listed 3d ago
$1,750
Olivenite image
Olivenite
Crystal Classics
Listed 3d ago
$1,750
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$240
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$450
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$250
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$240
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$450
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$250
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$400
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$240
Olivenite image
Olivenite
Crystal Classics
Updated 3d ago
$450

Where Olivenite is found

About Olivenite

Notable specimens have come from several classic localities globally, including arid or desert regions where secondary arsenates develop in oxide-rich environments. Namibia, the United Kingdom, the United States, Mexico, and Greece are among the places known for well-crystallized Olivenite and associated assemblages, sometimes yielding eye-catching, saturated color and crisp crystal form. Collectors prize Olivenite for its rich color range, striking termination shapes, and its historical association with copper deposits observed in old mines and secondary mineral parageneses.