
sedimentary
Jasper
Jasper (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale. Color: Greenish-brown and tan with mottled patterns. Luster: Dull to waxy. Crystal Structure: Microcrystalline/cryptocrystalline (trigonal). Cleavage: None; exhibits conchoidal fracture. Specific Gravity: 2.58–2.91.
- Hardness
- 6
- Color
- Greenish-brown and tan with mottled patterns
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5–7 on Mohs scale. Color: Greenish-brown and tan with mottled patterns. Luster: Dull to waxy. Crystal Structure: Microcrystalline/cryptocrystalline (trigonal). Cleavage: None; exhibits conchoidal fracture. Specific Gravity: 2.58–2.91.
Formation & geological history
Formed from the deposition of silica-rich solutions in sedimentary environments or volcanic ash. The color variations result from mineral inclusions like iron oxides or silicates during the consolidation process. Ages vary from Precambrian to Cenozoic.
Uses & applications
Commonly used in lapidary work for cabochons, beads, and ornamental carvings. Historically used for making tools and seals. Industrial use includes minor abrasive applications.
Geological facts
Jasper is an opaque variety of chalcedony. The name comes from the Greek 'iaspis', meaning 'spotted stone'. It was one of the stones in the High Priest's breastplate in biblical times.
Field identification & locations
Identify in the field by its opacity (it does not transmit light even on thin edges), its hardness (can scratch glass), and its distinctive smooth, shell-like fracture pattern. Often found in riverbeds or gravel deposits.
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