
sedimentary
Jasper
Jasper (Silica/Quartz) - SiO2
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs); Color: Reddish-brown to orange-brown due to iron inclusions; Luster: Vitreous to waxy; Structure: Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91.
- Hardness
- 6
- Color
- Reddish-brown to orange-brown due to iron inclusions
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 (Mohs); Color: Reddish-brown to orange-brown due to iron inclusions; Luster: Vitreous to waxy; Structure: Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.91.
Formation & geological history
Formed from silica-rich fluids filling fissures or voids in volcanic rock or sedimentary layers. Its color is derived from high concentrations of iron oxide (hematite) or goethite. It can form in various geological ages depending on local silica deposition.
Uses & applications
Used primarily as a gemstone for jewelry (cabochons), ornamental carvings, and historical use in making tools like seals and scrapers due to its hardness and smooth fracture.
Geological facts
Ancient civilizations called Jasper the 'mother of all stones.' It is an opaque variety of chalcedony that never lets light pass through, even at thin edges, distinguishing it from carnelian or agate.
Field identification & locations
Identify in the field by its waxy texture, smooth conchoidal (shell-like) fracture, and inability to be scratched by a steel knife. Common in riverbeds, desert pavements, and volcanic regions globally.
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