
sedimentary
Red Jasper
Jasper (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Brick red to brownish-red; Luster: Dull to vitreous; Crystal Structure: Microcrystalline; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to brownish-red
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Brick red to brownish-red; Luster: Dull to vitreous; Crystal Structure: Microcrystalline; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the accumulation of volcanic ash or fine silica-rich sediments. Often found in hydrothermal veins or as nodules in sedimentary rocks. Usually associated with aged volcanic activity or silica-charged waters in sedimentary environments.
Uses & applications
Commonly used for lapidary work, jewelry (beads, cabochons), carvings, and as a popular collector's stone. Historically used for seals and amulets.
Geological facts
The red color is caused by iron inclusions (Hematite). In ancient times, it was known as the 'rain bringer' and was highly valued by many cultures for its supposed protective properties.
Field identification & locations
Identify in the field by its deep red color, conchoidal (shell-like) fracture, and the fact that it cannot be scratched by a steel knife. Frequently found in stream beds or gravel deposits.
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