
Mineral
Jasper
Jasper (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Reddish-brown, tan, and cream bands; Luster: Vitreous to waxy; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Reddish-brown, tan, and cream bands
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Reddish-brown, tan, and cream bands; Luster: Vitreous to waxy; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the process of mineralization of volcanic ash or silica-rich sediments. It typically develops in hydrothermal veins or as nodules in volcanic and sedimentary rocks. Age varies from Precambrian to modern formations.
Uses & applications
Used primarily in lapidary work, jewelry (cabochons), interior decoration, and as a semi-precious collector stone. Historically used for making tools and seals.
Geological facts
Jasper is an opaque variety of chalcedony. The name comes from the Greek word 'iaspis', meaning 'spotted stone.' It has been a sacred stone in many cultures throughout history, used for amulets and ornaments.
Field identification & locations
Identify by its hardness (will scratch glass), opaque nature, and smooth conchoidal fractures. Commonly found in riverbeds, desert regions, and near volcanic outcrops. Collectors look for unique banding or color patterns.
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