
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Hematite inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Brick red with occasional quartz veining; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red with occasional quartz veining
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Brick red with occasional quartz veining; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed via the deposition of silica from water into subterranean cavities or during the metamorphism of organic-rich sediments or volcanic ash. The red color is caused by iron (hematite) inclusions incorporated during the solidification process.
Uses & applications
Commonly used as a gemstone for jewelry, in lapidary work for cabochons and tumbled stones, and as decorative architectural accents or stone carvings.
Geological facts
Red Jasper has been used since antiquity as a 'warrior's stone' for protection. It is a dense, opaque variety of chalcedony that is valued for its deep, rich color and ability to take a high polish.
Field identification & locations
Identifiable in the field by its opacity (unlike translucent carnelian), lack of cleavage, and resistance to scratching steel. Often found in riverbeds, desert pavements, and near iron-rich volcanic deposits.
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