
sedimentary
Jasper with Quartz Veining
Silicon Dioxide (SiO2) - Microcrystalline Quartz
Hardness: 6.5-7 on Mohs scale. Color: Greenish-grey matrix with white/tan veins. Luster: Dull to waxy. Crystal Structure: Microcrystalline (Trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Greenish-grey matrix with white/tan veins
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Greenish-grey matrix with white/tan veins. Luster: Dull to waxy. Crystal Structure: Microcrystalline (Trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.91.
Formation & geological history
Formed through the deposition of silica from water-rich fluids in cracks and fissures of a host rock. This specimen appears to be a river-tumbled pebble where secondary Quartz or Chalcedony has filled fractures in a metamorphosed sedimentary or volcanic siltstone base.
Uses & applications
Used primarily for lapidary work, decorative landscaping, and as a collectible 'pocket stone'. Polished versions are common in jewelry like cabochons or beads.
Geological facts
Jasper is often referred to as the 'supreme nurturer.' This specific bi-colored appearance is common in areas with high tectonic activity where rocks are crushed and then 'healed' by silica-rich hot water.
Field identification & locations
Identify in the field by its smoothness, lack of visible crystals in the matrix (cryptocrystalline), and its ability to scratch glass. Commonly found in riverbeds, glacial tills, and beaches.
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