
sedimentary
Jasper with Agate Inclusions
Jasper (Silicon Dioxide, SiO2) with Chalcedony/Agate
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Red, brown, and translucent white; Luster: Vitreous to waxy (especially when polished); Crystal Structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Red, brown, and translucent white
- Luster
- Vitreous to waxy (especially when polished)
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Red, brown, and translucent white; Luster: Vitreous to waxy (especially when polished); Crystal Structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.58-2.91.
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic or sedimentary rock cavities. Often associated with rhythmic precipitation of iron oxides and silica during the cooling of hydrothermal fluids.
Uses & applications
Primarily used for lapidary work, jewelry (cabochons), interior decoration, and as a popular semi-precious gemstone for mineral collectors.
Geological facts
Jasper is an opaque variety of chalcedony. When it shows translucent 'windows' or banding like this specimen, it is often called 'Agatized Jasper'. Red coloration typically comes from iron inclusions (hematite).
Field identification & locations
Identify in the field by its hardness (cannot be scratched by a steel knife), smooth conchoidal fracture, and opaque to semi-translucent patterns. Commonly found in riverbeds and volcanic regions in Oregon, Idaho (USA), Brazil, and Madagascar.
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