
sedimentary
Jasper
Silicon dioxide (SiO2) with impurities, microcrystalline quartz
Hardness: 6.5 to 7 on the Mohs scale; Color: Red, brown, yellow, green, or multicolored; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline quartz); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.58 to 2.91
- Hardness
- 6
- Color
- Red, brown, yellow, green, or multicolored
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale; Color: Red, brown, yellow, green, or multicolored; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline quartz); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.58 to 2.91
Formation & geological history
Formed through the silification of sedimentary or volcanic rocks where silica-rich fluids replace organic material or fill cavities over millions of years.
Uses & applications
Used in ornamental carvings, jewelry, lapidary arts, and as decorative aggregate.
Geological facts
Jasper has been used since ancient times to create seals, signet rings, and intricate talismans. Red varieties get their distinct color from iron oxide inclusions.
Field identification & locations
Can be identified in the field by its hardness (scratches glass), waxy to dull luster, and smooth conchoidal fracture. Commonly found in riverbeds, glacial tills, and areas with ancient volcanic or hydrothermal activity.
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