
sedimentary
Jasper (Red/Brown Variety)
Jasper (Microcrystalline Quartz, SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale; Color: Reddish-brown with variegated patterns; Luster: Vitreous to waxy; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.91
- Hardness
- 6
- Color
- Reddish-brown with variegated patterns
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Reddish-brown with variegated patterns; Luster: Vitreous to waxy; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.91
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic ash or fine-grained sediments, typically undergoing low-grade metamorphism or hydrothermal replacement over millions of years (often Proterozoic to Cenozoic eras).
Uses & applications
Used extensively in jewelry (cabochons), lapidary art, decorative ornaments, and as a metaphysical healing stone. Historically used for making tools and seals.
Geological facts
Jasper’s name is derived from the Greek word 'iaspis', meaning spotted stone. It is almost always opaque and contains up to 20% foreign materials which determine its unique color and pattern.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), opacity, and smooth, waxy feel when polished or tumbled. Commonly found in riverbeds, desert regions, and volcanic areas in the USA (Oregon, Idaho), India, and Brazil.
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