
mineral
Red Jasper
Silicon Dioxide with Hematite impurities (SiO2 + Fe2O3)
AI-generated identification · may be incorrectHardness: 6.5–7 on the Mohs scale; Color: Terracotta red to brownish-red; Luster: Dull to vitreous (waxy when polished); Crystal Structure: Hexagonal (trigonal) microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91
- Hardness
- 6
- Color
- Terracotta red to brownish-red
- Luster
- Dull to vitreous (waxy when polished)
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Physical properties
Hardness: 6.5–7 on the Mohs scale; Color: Terracotta red to brownish-red; Luster: Dull to vitreous (waxy when polished); Crystal Structure: Hexagonal (trigonal) microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91
Formation & geological history
Formed through the deposition of silica from hydrothermal solutions or within sedimentary rocks, where iron inclusions (hematite) provide the red pigment. It can form in various geological ages, often found in ancient volcanic and sedimentary sequences.
Uses & applications
Commonly used in jewelry (beads, cabochons), lapidary arts, decorative ornaments, and as a spiritual 'root chakra' stone in the metaphysical community.
Geological facts
Red Jasper has been used for millennia; it was a favorite for amulets in Ancient Egypt and mentioned in biblical texts. It is considered a variety of chalcedony that is opaque due to its high mineral inclusion content.
Field identification & locations
Identify in the field by its deep red color, characteristic conchoidal fracture (curved breaks), and hardness (it will scratch glass but not quartz). Common locations include India, Brazil, South Africa, and the Southwestern United States.
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