
sedimentary
Polychrome Jasper
Silicon Dioxide (SiO2) with impurities
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale; Color: Multi-colored bands (red, tan, grey, green); Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6–2.9
- Hardness
- 6
- Color
- Multi-colored bands (red, tan, grey, green)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Multi-colored bands (red, tan, grey, green); Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6–2.9
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic ash or fine sediment, followed by the oxidation of iron and other minerals which create the 'flame-like' colored patterns. This specific variety is primarily found in Madagascar.
Uses & applications
Used extensively in the lapidary arts for spheres, cabochons, and decorative carvings. It is popular in the metaphysical community for jewelry and meditation aids.
Geological facts
Also known as Desert Jasper, it was discovered relatively recently in 2006 near the coast of Madagascar. Each piece is unique due to the random nature of the mineral impurities seeped into the quartz.
Field identification & locations
Identify by its opaque nature, high polish, and distinct rhythmic swirls or 'flame' patterns of color that blend smoothly into one another. It lacks the geometric lines seen in agate.
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