
sedimentary
Red Jasper
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brick red to brownish red due to iron inclusions; Luster: Vitreous to waxy; Crystal structure: Trigonal (Microcrystalline quartz); Cleavage: None/Conchoidal fracture; Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to brownish red due to iron inclusions
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brick red to brownish red due to iron inclusions; Luster: Vitreous to waxy; Crystal structure: Trigonal (Microcrystalline quartz); Cleavage: None/Conchoidal fracture; Specific gravity: 2.58-2.91
Formation & geological history
Formed from the deposition of silica-rich fluids in volcanic or sedimentary environments, often associated with iron-rich deposits. Its red color comes from high concentrations of iron oxide (hematite).
Uses & applications
Used primarily in jewelry (cabochons, beads), decorative carvings, and as a popular stone for tumbling and crystal healing collections.
Geological facts
Red Jasper has been used for millennia as a sacred stone. In ancient Egypt, it was often used for amulets and scarabs, believed to represent the blood of Isis. It is a variety of chalcedony that is opaque.
Field identification & locations
Identifiable by its deep red color, opacity, and extreme hardness (cannot be scratched by a steel knife). Commonly found in riverbeds or as pebbles in desert environments worldwide, especially in the US, Brazil, and India.
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