Crocoite

Crocoite specimens for sale

18 for sale ยท $65โ€“$2,300 USD

188 in the gallery

Crocoite is a mineral composed of lead chromate, typically forming long, slender, orange-red to reddish-orange crystals that glisten with a vitreous to resinous luster. The crystal habit is commonly tabular to prismatic, often developing elongated forms that catch the light and display strong color. In well-cut specimens, the orange hues can be vivid and saturated, making Crocoite a striking centerpiece for mineral cabinets.

Formula
PbCr6+O4
Rarity
Rare
Stability
Stable
Collector interest
Very High Interest
Classification notes
Chromate mineral; lead chromate (Strunz: 6.BA)

Key characteristics

Crystal system
monoclinic
Mohs hardness
2.5โ€“3
Specific gravity
5.9โ€“6.1
Luster
adamantine, vitreous, resinous
Transparency
transparent, translucent
Color
red, orange, yellow
Streak
orange, yellow
Cleavage
distinct
Fracture
conchoidal, uneven
Crystal habit
prismatic, acicular, granular, massive
  • Classic / historic

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Where Crocoite is found

Top localities

  1. Adelaide Mine40 specimens
  2. Beryozovsky32 specimens
  3. Red Lead Mine31 specimens
  4. Callenberg3 specimens
  5. Dundas Extended Mine2 specimens
  6. Franklin1 specimen
  7. Le Cantonnier vein1 specimen
  8. Sverdlovsk Oblast1 specimen
  9. Berezovskii, Ekaterinburg1 specimen
  10. Natural History Museum, London1 specimen

About Crocoite

Notable occurrences include classic pockets in the Dundas region of Australia and historic finds in the Urals of Russia, where the mineral has been sought after for generations. Collectors prize Crocoite for its intense color, dramatic crystal forms, and the way light plays along its faces. The mineralโ€™s rarity in pristine, well-formed specimens contributes to its appeal, and peak examples are often associated with distinctive, well-preserved crystal terminations.

Collectors value Crocoite for its bold presence, the aesthetic contrast against darker matrixes, and the historical associations of Australian and Russian locales. It pairs well with specimens of related chromates and can serve as a vivid highlight in mineral displays, illustrating how chemistry and crystal form combine to produce striking color in the mineral world.