
mineral
Polished brown jasper (probable brecciated jasper)
Microcrystalline quartz/chalcedony, SiO₂, with iron-oxide inclusions
AI-generated identification · may be incorrectOpaque brown to black, waxy to vitreous luster, with mottled iron staining and possible brecciation; Mohs hardness about 6.5–7, no visible cleavage, conchoidal fracture, and specific gravity near 2.6. The rounded shape indicates tumbling or natural abrasion.
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Physical properties
Opaque brown to black, waxy to vitreous luster, with mottled iron staining and possible brecciation; Mohs hardness about 6.5–7, no visible cleavage, conchoidal fracture, and specific gravity near 2.6. The rounded shape indicates tumbling or natural abrasion.
Formation & geological history
Jasper forms when silica-rich fluids replace or cement volcanic ash, sediment, or fractured rock, commonly with hematite or goethite producing the brown color. Formation ages vary widely, from Precambrian to younger volcanic and hydrothermal settings.
Uses & applications
Used for cabochons, beads, carvings, ornaments, and lapidary specimens; rarely used as a minor decorative stone or aggregate.
Geological facts
Its color and patterns arise mainly from iron oxides rather than distinct large crystals. The specimen may also be iron-rich chert if its texture is especially fine-grained.
Field identification & locations
Identify by its opacity, fine texture, hardness, lack of cleavage, and inability to scratch it with a steel knife; quartz or glass should scratch it. Common sources include India, Madagascar, Brazil, the western United States, and Australia.
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