
mineral
Red Jasper
Chalcedony/Quartz (SiO2) with iron inclusions
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale; Color: Dull red to brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.91
- Hardness
- 6
- Color
- Dull red to brownish-red
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Dull red to brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.91
Formation & geological history
Jasper is a microcrystalline variety of quartz that forms when silica-rich fluids permeate porous volcanic or sedimentary rocks. The red coloring comes from high iron oxide (hematite) content during its formation, which typically occurs in hydrothermal environments or where volcanic ash is deposited.
Uses & applications
Commonly used as a gemstone in jewelry (cabochons, beads), decorative carvings, pocket stones, and industrial use in high-end abrasives due to its hardness and durability.
Geological facts
Red Jasper has been used since antiquity; it was known as the 'rain bringer' in some Native American cultures and was frequently used in the ancient world for cylinder seals and amulets. It is an opaque variety of chalcedony.
Field identification & locations
Identify by its deep red color, opacity (it will not let light through even at thin edges), and its glass-like conchoidal fracture if broken. It is a common find in river beds, deserts, and areas with old volcanic activity.
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