
sedimentary
Jasper
Opaque Cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Brownish-red to tan. Luster: Dull to vitreous. Crystal Structure: Trigonal/Microcrystalline. Specific Gravity: 2.58-2.91. Cleavage: None (Conchoidal fracture).
- Hardness
- 6
- Color
- Brownish-red to tan
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Brownish-red to tan. Luster: Dull to vitreous. Crystal Structure: Trigonal/Microcrystalline. Specific Gravity: 2.58-2.91. Cleavage: None (Conchoidal fracture).
Formation & geological history
Jasper is typically formed in sedimentary environments when silica-rich fluids precipitate into porous rocks or volcanic ash. The brown and red tones are primarily caused by iron oxide (limonite or hematite) impurities within the silica structure.
Uses & applications
Used primarily as a gemstone for jewelry, lapidary cabochons, and decorative ornamental carvings. Historically used for making tools due to its hardness and sharp fracture edges.
Geological facts
The name 'Jasper' originates from the Greek word 'iaspis', meaning spotted stone. It has been used since antiquity for seals and amulets, and was mentioned in the Bible as a stone of the High Priest's breastplate.
Field identification & locations
Identify in the field by its opacity (even on thin edges), its hardness (it will scratch glass), and its smooth, waxy fracture surface. Commonly found in riverbeds and desert environments where volcanic activity once met water.
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