
sedimentary
Red Jasper
Microcrystalline Quartz (Chalcedony), SiO2
AI-generated identification · may be incorrectHardness: 6.5 to 7 on the Mohs scale. Color: Red, brownish-red, or reddish-brown due to iron oxide impurities. Luster: Vitreous to dull. Crystal structure: Trigonal (microcrystalline). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.58 to 2.91.
- Hardness
- 6
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale. Color: Red, brownish-red, or reddish-brown due to iron oxide impurities. Luster: Vitreous to dull. Crystal structure: Trigonal (microcrystalline). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.58 to 2.91.
Formation & geological history
Formed through the hydrothermal deposition of silica-rich fluids or precipitation of silica in marine environments, often associated with iron formations and volcanic activity, dating from various geological eras including the Precambrian.
Uses & applications
Used for ornamental objects, cabochons, carved items, jewelry, and as a popular specimen for rock collectors.
Geological facts
Jasper has been used since ancient times for talismans, seals, and weaponry. Red jasper was particularly valued by ancient Egyptians and Native Americans for its protective and grounding symbolism.
Field identification & locations
Can be identified in the field by its opaque red color, waxy-to-dull luster, hardness that scratches glass, and smooth conchoidal fracture. Commonly found in stream beds, gravel deposits, and sedimentary rock formations worldwide.
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