
mineral
Tumbled brown jasper (likely brecciated jasper)
Microcrystalline quartz/chalcedony, SiO₂, with iron-oxide and other mineral inclusions
AI-generated identification · may be incorrectOpaque brown to reddish-brown, mottled and faintly brecciated, with a vitreous-to-waxy luster and no visible cleavage. Hardness is approximately 6.5–7 Mohs; density about 2.6 g/cm³. The rounded, glossy surface indicates tumbling or polishing.
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Physical properties
Opaque brown to reddish-brown, mottled and faintly brecciated, with a vitreous-to-waxy luster and no visible cleavage. Hardness is approximately 6.5–7 Mohs; density about 2.6 g/cm³. The rounded, glossy surface indicates tumbling or polishing.
Formation & geological history
Forms when silica-rich fluids cement and replace fine-grained sediments or fractured volcanic material, with iron oxides producing the brown-red coloration. Jasper deposits commonly formed from Paleozoic to Cenozoic volcanic or sedimentary systems.
Uses & applications
Used for cabochons, beads, carvings, decorative stones, and lapidary collections; occasionally used as architectural or ornamental material.
Geological facts
Jasper is a variety of opaque chalcedony and may contain hematite, goethite, clay minerals, or remnants of volcanic rock. The precise variety cannot be confirmed from the photograph alone.
Field identification & locations
Identify by its opaque earthy colors, very fine texture, quartz-like hardness, and absence of cleavage; it should scratch glass but not be scratched by a steel knife. Common sources include India, Madagascar, Brazil, Mexico, Australia, and the western United States.
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