
sedimentary
Jasper
Silicon dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Reddish-brown, earthy tones; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline quartz); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Reddish-brown, earthy tones
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Reddish-brown, earthy tones; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline quartz); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from water-saturated solutions in volcanic ash or hydrothermal veins. Often associated with the replacement of organic materials or sedimentary accumulation over millions of years.
Uses & applications
Used primarily in lapidary work for jewelry, cabochons, and decorative carvings. Historically used for making tools and seals due to its toughness and fracture pattern.
Geological facts
Jasper is an opaque variety of chalcedony. The reddish color is typically caused by iron inclusions. It has been a featured gemstone in religious texts and ancient Mesopotamian cylinder seals.
Field identification & locations
Identify in the field by its opacity (it does not pass light even on thin edges), its hardness (will scratch glass), and its distinctive waxy/smooth feel when broken. Found globally in areas with volcanic or sedimentary history.
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