
sedimentary
Jasper
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5 to 7 on the Mohs scale, Color: Varies widely including red, brown, yellow, green, and multicolored, Luster: Vitreous to dull, Crystal structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: None (exhibits conchoidal fracture), Specific gravity: 2.58 to 2.91
- Hardness
- 6
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale, Color: Varies widely including red, brown, yellow, green, and multicolored, Luster: Vitreous to dull, Crystal structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: None (exhibits conchoidal fracture), Specific gravity: 2.58 to 2.91
Formation & geological history
Forms from the precipitation of silica-rich fluids in sedimentary environments, or as a primary filling in volcanic rocks and hydrothermal veins. Often associated with ancient marine deposits and can range in geological age from Precambrian to recent.
Uses & applications
Used widely in ornamental carvings, cabochons for jewelry, decorative objects, and as a popular specimen for lapidary work and rock tumbling.
Geological facts
Jasper has been used by ancient civilizations for thousands of years to create tools, seals, and ornate jewelry. Its name comes from the ancient Greek word iaspis, meaning 'spotted stone'.
Field identification & locations
Can be identified in the field by its smooth, water-worn appearance in riverbeds, waxy or dull luster, lack of cleavage, and high hardness which scratches glass. Found worldwide, particularly in river gravels, volcanic regions, and areas with ancient sedimentary deposits.
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