
sedimentary
Jasper (Zebra Jasper)
Silicon Dioxide (SiO2) with impurities
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Creamy white to tan with dark grey or brown banding, Luster: Vitreous to waxy, Crystal Structure: Trigonal (microcrystalline/cryptocrystalline quartz), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.9.
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Creamy white to tan with dark grey or brown banding, Luster: Vitreous to waxy, Crystal Structure: Trigonal (microcrystalline/cryptocrystalline quartz), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.9.
Formation & geological history
Formed from the consolidation of microcrystalline quartz or volcanic ash. The unique 'zebra' patterns are created by the secondary deposition of iron oxides or other mineral impurities as the host rock undergoes chemical changes over millions of years.
Uses & applications
Commonly used in lapidary arts for beads, cabochons, and tumbled stones. Due to its hardness, it is also popular for decorative carvings, palm stones, and meditation tools.
Geological facts
Jasper is a variety of chalcedony. The name 'Jasper' is derived from the Greek word 'iaspis', meaning spotted stone. Zebra Jasper specifically is often associated with balance because of its contrasting colors.
Field identification & locations
Identify in the field by its distinctive 'swirled' or striped pattern, high hardness (it cannot be scratched by a steel knife), and smooth, waxy feel when polished. It is widely found in India, Russia, and Africa.
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