
sedimentary
Jasper
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 on the Mohs scale. Color: Brown, yellowish-brown, red, or multicolored. Luster: Waxy to vitreous. Crystal structure: Trigonal (microcrystalline/cryptocrystalline aggregate). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.58-2.91.
- Hardness
- 7 on the Mohs scale
- Color
- Brown, yellowish-brown, red, or multicolored
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on the Mohs scale. Color: Brown, yellowish-brown, red, or multicolored. Luster: Waxy to vitreous. Crystal structure: Trigonal (microcrystalline/cryptocrystalline aggregate). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.58-2.91.
Formation & geological history
Formed through the deposition of silica-rich fluids in sedimentary environments, often involving the alteration of volcanic ash or silica precipitation in marine sediments. Geological age varies widely from Precambrian to Cenozoic.
Uses & applications
Used for making decorative objects, cabochons, carvings, and jewelry. Also collected by rockhounds and lapidary enthusiasts.
Geological facts
Jasper has been used since ancient times to create seals, signet rings, and ornamental weapons due to its toughness and ability to take a high polish. Brown varieties are sometimes referred to as picture jasper or ferruginous chert.
Field identification & locations
Can be identified in the field by its hardness (scratches glass), lack of visible crystals even under magnification, waxy luster, and conchoidal fracture. Commonly found in riverbeds, beaches, and mountainous regions worldwide.
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