
sedimentary
Zebra Jasper
Silicon Dioxide (SiO2) with Manganese/Iron oxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Creamy white with black or dark brown stripes, Luster: Dull to vitreous, Crystal Structure: Trigonal (microcrystalline), 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 with black or dark brown stripes, Luster: Dull to vitreous, Crystal Structure: Trigonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.9
Formation & geological history
Formed from the deposition of silica-rich sediments in alternating layers or through the infiltration of mineral oxides into cracks in a host rock. Often dates to the Precambrian or Paleozoic eras.
Uses & applications
Used primarily in lapidary arts for beads, pendants, cabochons, and decorative ornamental carvings. Highly valued in the metaphysical community as a grounding stone.
Geological facts
Despite the name, Zebra Jasper is often technically a type of siltstone or marble rather than a true jasper, but it is traded under the Jasper name due to its opacity and hardness. It is frequently sourced from Western Australia.
Field identification & locations
Identify in the field by its distinct high-contrast linear banding and smooth, waxy texture when wet. Found commonly in Australia, Brazil, Russia, and India. Collectors look for sharp, clean transitions between the black and white bands.
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