
sedimentary
Orbicular jasper (often sold as leopard-skin jasper)
Silicified volcanic tuff/rhyolite; chiefly microcrystalline quartz and chalcedony (SiO₂), with iron oxides and altered volcanic minerals
AI-generated identification · may be incorrectTypically opaque, dark gray-brown with cream, tan, and yellow orbicular patterns; waxy to vitreous luster when polished. Mohs hardness about 6.5–7; cryptocrystalline, massive, with no obvious cleavage; specific gravity roughly 2.5–2.7.
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Physical properties
Typically opaque, dark gray-brown with cream, tan, and yellow orbicular patterns; waxy to vitreous luster when polished. Mohs hardness about 6.5–7; cryptocrystalline, massive, with no obvious cleavage; specific gravity roughly 2.5–2.7.
Formation & geological history
Forms when silica-rich fluids silicify volcanic ash or lava, preserving spherulitic or orb-like textures; generally Cenozoic volcanic material, though age depends on locality. Similar material is commonly associated with altered rhyolitic terrains.
Uses & applications
Used for cabochons, beads, carvings, palm stones, and decorative objects; occasionally marketed as a lapidary jasper. It has little industrial value beyond ornamental stone.
Geological facts
The concentric spots are geological orbicules or altered spherulites, not animal markings. “Leopard-skin jasper” is a commercial name and may refer to several visually similar materials.
Field identification & locations
Identify it by its opaque silica-rich body, hardness, conchoidal fracture, and natural orbicular pattern; it will not fizz in dilute acid. Commonly reported from Mexico, Madagascar, Indonesia, and the western United States.
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