
sedimentary
Red Jasper
Jasper (Silicon Dioxide with Iron Oxide inclusions), SiO2
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Brick red to deep brownish-red; Luster: Dull to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to deep brownish-red
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Brick red to deep brownish-red; Luster: Dull to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from water-rich environments, often in volcanic ash or sedimentary beds. The red color is derived from high iron oxide (hematite) content during its formation over millions of years.
Uses & applications
Used widely in lapidary arts for cabochons, beads, and carvings; historically used for ornamental jewelry, amulets, and architectural inlays. Also popular as a decorative landscaping stone.
Geological facts
Red Jasper has been used since ancient times for its supposed protective qualities; it was known as the 'mother of all stones' in some cultures and was used in the seal of the Hebrew High Priest.
Field identification & locations
Identify by its opaque red color, smoothness when weathered, and lack of visible crystalline grain. It cannot be scratched by a steel knife. Common in diverse geological settings worldwide, especially in riverbeds or coastal areas.
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