
gemstone
Tumbled jasper (likely brecciated or red jasper)
Microcrystalline quartz/chalcedony, SiO₂, with iron-oxide inclusions
AI-generated identification · may be incorrectOpaque reddish-brown to tan, vitreous-to-waxy luster, and rounded tumbled surfaces. Mohs hardness is about 6.5–7; no visible cleavage and typically massive, cryptocrystalline structure.
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Physical properties
Opaque reddish-brown to tan, vitreous-to-waxy luster, and rounded tumbled surfaces. Mohs hardness is about 6.5–7; no visible cleavage and typically massive, cryptocrystalline structure.
Formation & geological history
Jasper forms when silica-rich fluids replace or cement sediments and volcanic material, with iron oxides producing red and brown colors. Its exact geological age cannot be determined from the photograph; specimens occur in many ancient and younger volcanic-sedimentary terrains.
Uses & applications
Used for cabochons, beads, carvings, ornaments, and inexpensive polished specimens; historically used for tools and decorative stone.
Geological facts
The upper piece may be brecciated jasper or a jasper variety mixed with lighter chalcedony, while the lower piece appears predominantly red jasper. Tumble polishing can obscure natural textures and diagnostic features.
Field identification & locations
Identify jasper by its opacity, earthy red coloration, fine texture, and lack of visible crystal grains; it should not scratch easily with a steel knife. Common sources include India, Madagascar, Brazil, the United States, and Australia.
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