
sedimentary
Leopard Skin Jasper
Silicon Dioxide (SiO2) with mineral inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Cream, tan, brown, reddish-brown, and green in orbicular or spotted patterns; Luster: Vitreous to waxy when polished; Crystal structure: Trigonal (microcrystalline/cryptocrystalline quartz); Cleavage: None, exhibits conchoidal fracture.
- Hardness
- 6
- Luster
- Vitreous to waxy when polished
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Cream, tan, brown, reddish-brown, and green in orbicular or spotted patterns; Luster: Vitreous to waxy when polished; Crystal structure: Trigonal (microcrystalline/cryptocrystalline quartz); Cleavage: None, exhibits conchoidal fracture.
Formation & geological history
Formed through hydrothermal deposition of silica within volcanic cavities or ash beds, where iron oxides and other mineral impurities aggregate in distinct orbicular or blotched patterns during precipitation.
Uses & applications
Used primarily as decorative lapidary material, in polished cabochons for jewelry, tumbled stones, carvings, and popular among gemstone collectors and metaphysical enthusiasts.
Geological facts
Also known as Leopardite or Orbicular Jasper, its distinctive spotted appearance resembles the coat of a leopard. It is actually a form of orbicular chalcedony mixed with various iron and manganese oxide inclusions.
Field identification & locations
Identified by its distinctive multi-colored blotched or leopard-like spotted markings on an opaque chalcedony base. Commonly found in Mexico, Peru, Brazil, and South Africa. Easily polished for tumbled stone collections.
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