
sedimentary
Picture Jasper
Silicon Dioxide (SiO2) with iron oxide and mineral inclusions
Hardness: 6.5–7 (Mohs); Color: Tan, brown, grey, and black; Luster: Vitreous to waxy; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.91
- Hardness
- 6
- Color
- Tan, brown, grey, and black
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 (Mohs); Color: Tan, brown, grey, and black; Luster: Vitreous to waxy; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.91
Formation & geological history
Formed as a sedimentary process where silica-rich fluids (often from volcanic ash petrification) permeate through sediments or fractures. The 'picture' patterns are caused by the slow oxidation of iron and other mineral impurities during the crystallization process over millions of years.
Uses & applications
Primarily used as a semi-precious gemstone for jewelry, lapidary cabochons, decorative ornaments, and by mineral collectors for its unique landscape-like patterns.
Geological facts
Picture Jasper is often called 'the Earth speaking to its children' because its patterns frequently resemble miniature landscapes, mountains, or deserts. Its unique patterns are unique to each specimen, meaning no two stones are exactly alike.
Field identification & locations
Identify in the field by its opaque, dense appearance and smooth, glass-like fracture surfaces when broken. It is commonly found in the Pacific Northwest of the USA (particularly Idaho and Oregon). Collectors should look for distinct, high-contrast 'scenes' which increase value.
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