
sedimentary
Red Jasper
Microcrystalline Quartz (SiO2) with iron oxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 on the Mohs scale; Color: Deep red, brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Deep red, brownish-red
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 on the Mohs scale; Color: Deep red, brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.58-2.91
Formation & geological history
Formed through the precipitation of silica-rich fluids in sedimentary environments or hydrothermal veins, often associated with banded iron formations. Geological age varies widely from Precambrian to Cenozoic.
Uses & applications
Used in ornamental carvings, cabochons, jewelry, tumbling, and as a decorative stone.
Geological facts
Red jasper is an opaque variety of chalcedony. The rich red color is primarily due to iron(III) inclusion impurities. It has been used historically by ancient peoples for amulets, seals, and tools.
Field identification & locations
Can be identified in the field by its deep red color, waxy-to-dull luster, conchoidal fracture (creating sharp edges), and inability to be scratched by a steel knife. Found worldwide, particularly in regions with ancient marine or volcanic deposits.
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