
mineral
Tumbled brown jasper
Jasper, microcrystalline quartz (SiO₂), commonly with iron-oxide impurities
AI-generated identification · may be incorrectOpaque chocolate-brown, smooth and rounded from tumbling, with a dull to waxy luster; Mohs hardness about 6.5–7, no visible cleavage, cryptocrystalline quartz structure, and specific gravity near 2.6.
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Physical properties
Opaque chocolate-brown, smooth and rounded from tumbling, with a dull to waxy luster; Mohs hardness about 6.5–7, no visible cleavage, cryptocrystalline quartz structure, and specific gravity near 2.6.
Formation & geological history
Jasper forms when silica-rich fluids replace or cement volcanic ash, sediment, or fractured rock, with iron oxides producing the brown color. Deposits occur in many ages and regions, including India, Madagascar, Brazil, and the western United States.
Uses & applications
Used as inexpensive ornamental stone, beads, cabochons, carvings, and lapidary material; polished pieces are popular in collections and crafts.
Geological facts
Jasper is technically an opaque variety of chalcedony or microcrystalline quartz. Color and patterns reflect impurities such as hematite, goethite, clay, and other minerals.
Field identification & locations
Identify it by its opaque earthy color, glassy-to-waxy polish, absence of cleavage, and ability to scratch ordinary glass. The pictured piece is likely commercially tumbled rather than naturally rounded.
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