
metamorphic
Polished orbicular jasper
Jasper, microcrystalline quartz (SiO₂), with iron oxides and altered volcanic inclusions
AI-generated identification · may be incorrectOpaque olive-brown, cream, and dark patterned stone with a glossy polish; hardness about 6.5–7 Mohs, cryptocrystalline quartz, no visible cleavage, specific gravity roughly 2.6. The mottled/orbicular pattern reflects mineral-rich inclusions or replacement textures.
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Physical properties
Opaque olive-brown, cream, and dark patterned stone with a glossy polish; hardness about 6.5–7 Mohs, cryptocrystalline quartz, no visible cleavage, specific gravity roughly 2.6. The mottled/orbicular pattern reflects mineral-rich inclusions or replacement textures.
Formation & geological history
Jasper forms when silica-rich fluids replace or cement volcanic and sedimentary material; orbicular varieties develop concentric or radiating mineral patterns. Geological ages vary, commonly Precambrian to Phanerozoic depending on locality.
Uses & applications
Used for cabochons, worry stones, carvings, beads, and decorative objects; rarely used as aggregate because attractive specimens are collectible.
Geological facts
The photographed piece is shaped and highly polished, so surface appearance is enhanced and field identification is limited. Similar material may be sold as ocean jasper, leopard jasper, or rainforest jasper, though trade names are not always scientifically precise.
Field identification & locations
Common sources include Madagascar, Australia, India, Mexico, Brazil, and the western United States. Identify by its opaque silica-rich body, waxy-to-glassy polish, hardness, and inability to scratch easily with a steel blade; acid produces no reaction.
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