
sedimentary
Zebra Jasper
Silicon dioxide (microcrystalline quartz), SiO2
AI-generated identification · may be incorrectHardness: 6.5 to 7 on the Mohs scale. Color: Brown, tan, and white banded or striped patterns. Luster: Vitreous to dull when polished. Crystal structure: Trigonal (microcrystalline). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.65.
- Hardness
- 6
- Color
- Brown, tan, and white banded or striped patterns
- Luster
- Vitreous to dull when polished
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale. Color: Brown, tan, and white banded or striped patterns. Luster: Vitreous to dull when polished. Crystal structure: Trigonal (microcrystalline). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.65.
Formation & geological history
Formed through the deposition and compaction of silica-rich sediments or volcanic ash in ancient environments, often altered by hydrothermal solutions over millions of years.
Uses & applications
Commonly used in lapidary arts, tumbled stones, beaded jewelry, carvings, and as a decorative ornamental stone.
Geological facts
Despite being called jasper, it is technically an opaque, impure variety of microcrystalline quartz or sometimes a fine-grained banded siltstone. The striking contrast gives it a resemblance to zebra stripes, highly favored in metaphysical and crystal healing communities.
Field identification & locations
Easily identified by its distinct brown and white striping and high polish retention. Found worldwide with notable deposits in India, Australia, and Africa.
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