
sedimentary
Polished orbicular jasper
Siliceous microcrystalline quartz/chalcedony (SiO₂), commonly with iron-oxide and volcanic inclusions
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; tan, cream, gray, and brown concentric or brecciated patterns; waxy to dull luster; cryptocrystalline, with no visible cleavage and conchoidal fracture. The smooth surface indicates natural or human polishing.
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Physical properties
Hardness about 6.5–7 Mohs; tan, cream, gray, and brown concentric or brecciated patterns; waxy to dull luster; cryptocrystalline, with no visible cleavage and conchoidal fracture. The smooth surface indicates natural or human polishing.
Formation & geological history
Formed when silica-rich fluids replaced or cemented volcanic sediment and filled cavities, preserving orbicular or flow-like patterns; typically Cenozoic to older volcanic-terrain material. Exact age and locality cannot be determined from the photograph.
Uses & applications
Used for cabochons, carvings, beads, polished specimens, and decorative stone; too small for construction use.
Geological facts
Jasper is an opaque variety of chalcedony, and its colors commonly come from hematite, limonite, or other iron minerals. Patterned varieties are often sold under locality-based trade names.
Field identification & locations
Identify it by its opaque silica body, fine grain, hardness, and distinctive rounded or layered markings; it should scratch glass but not be scratched by a steel knife. Common sources include Oregon, Idaho, Madagascar, Mexico, and Australia.
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