
sedimentary
Red Jasper
Jasper (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale; Color: Red due to iron inclusions; Luster: Dull to vitreous; Crystal Structure: Trigonal (microcrystalline quartz); Cleavage: None; Specific Gravity: 2.58–2.91
- Hardness
- 6
- Color
- Red due to iron inclusions
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Red due to iron inclusions; Luster: Dull to vitreous; Crystal Structure: Trigonal (microcrystalline quartz); Cleavage: None; Specific Gravity: 2.58–2.91
Formation & geological history
Formed from the deposition of silica-rich fluids in volcanic or sedimentary environments. Its red color comes from iron oxide (hematite) impurities integrated during formation, often millions of years old.
Uses & applications
Used primarily as a gemstone in jewelry, for lapidary work (cabochons), as an ornamental stone, and in spiritual/metaphysical collections.
Geological facts
Jasper was a favorite gemstone in the ancient world, mentioned in biblical texts and used by early civilizations for seals and talismans. It is an opaque variety of chalcedony.
Field identification & locations
Identify by its waxy to dull luster, lack of transparency, and high hardness (it cannot be scratched by a steel knife). Commonly found in river beds, beaches, and desert areas worldwide.
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