
sedimentary
Banded Jasper
Silicon Dioxide (SiO2) with iron oxide impurities
AI-generated identification · may be incorrectHardness: 6.5 to 7 on Mohs scale; Color: Reddish-brown with white and yellow swirls; Luster: Vitreous to waxy (when polished); Crystal Structure: Microcrystalline/Trigonal (Cryptocrystalline); Cleavage: None; Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Reddish-brown with white and yellow swirls
- Luster
- Vitreous to waxy (when polished)
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Physical properties
Hardness: 6.5 to 7 on Mohs scale; Color: Reddish-brown with white and yellow swirls; Luster: Vitreous to waxy (when polished); Crystal Structure: Microcrystalline/Trigonal (Cryptocrystalline); Cleavage: None; Specific Gravity: 2.58-2.91
Formation & geological history
Formed via the accumulation of silica-rich fluids in volcanic ash or sedimentary deposits, where iron oxides create the distinct banding. These often form in Precambrian to Cenozoic geological ages.
Uses & applications
Used primarily in jewelry (cabochons, beads), decorative carvings, and as a popular pocket stone or meditation aid in crystal healing communities.
Geological facts
Jasper is an opaque variety of chalcedony. The name 'Jasper' is derived from the Greek word 'iaspis', meaning 'spotted stone'. It was a favorite gem in the ancient world, mentioned in the Bible and worn by Babylonian kings.
Field identification & locations
Identified in the field by its opacity (unlike translucent agate), conchoidal fracture, and smooth patterns that do not follow clean lines. Commonly found in riverbeds and desert environments such as those in India, Brazil, and the Southwestern USA.
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