
sedimentary
Jasper with Quartz inclusions
Silicon Dioxide (SiO2) with impurities
AI-generated identification · may be incorrectHardness: 6.5-7 on the Mohs scale. Color: Red (hematite inclusions) and creamy white/yellow. Luster: Dull to vitreous. Crystal Structure: Trigonal/Microcrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Red (hematite inclusions) and creamy white/yellow
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 on the Mohs scale. Color: Red (hematite inclusions) and creamy white/yellow. Luster: Dull to vitreous. Crystal Structure: Trigonal/Microcrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.91.
Formation & geological history
Formed through the process of hydrothermal replacement or silicification within sedimentary or volcanic rock beds. The red coloring indicates iron oxide content. Most jasper formed during various geological eras, notably the Mesozoic and Cenozoic.
Uses & applications
Used primarily for lapidary work, jewelry (cabochons), interior decoration, and as a popular specimen for rock collectors and metaphysical use.
Geological facts
Jasper is an opaque variety of chalcedony. The name comes from the Greek 'iaspis', meaning 'spotted stone.' Many ancient civilizations used jasper for seals and amulets because of its durability.
Field identification & locations
Identify in the field by its waxy to dull luster, conchoidal fracture (curved breaks), and hardness (cannot be scratched by a steel knife). Commonly found in riverbeds or volcanic regions like those in the Western USA (Oregon, Idaho) and India.
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