
sedimentary
Polychrome Jasper (Desert Jasper)
Silicon Dioxide (SiO2) with iron and mineral inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Swirls of red, brown, tan, grey, and teal; Luster: Vitreous to waxy (when polished); Crystal Structure: Hexagonal (Microcrystalline); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Swirls of red, brown, tan, grey, and teal
- Luster
- Vitreous to waxy (when polished)
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Swirls of red, brown, tan, grey, and teal; Luster: Vitreous to waxy (when polished); Crystal Structure: Hexagonal (Microcrystalline); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic ash or fine sediment, followed by slow cooling and pressure. These specimens typically originate from the Cretaceous period (approx. 66-145 million years ago) in the Norcross area of Madagascar.
Uses & applications
Primarily used as a lapidary material for decorative carvings, palm stones, jewelry cabochons, and as a metaphysical/collector's stone.
Geological facts
Discovered relatively recently (around 2006) during a search for new deposits of Ocean Jasper in Madagascar. It is known for its unique 'landscape' patterns that look like desert paintings.
Field identification & locations
Identify in the field by its opaque, multi-colored circular or wavy patterns and high hardness that cannot be scratched by a steel pocket knife. Found almost exclusively in Madagascar. For collectors, look for high color contrast and absence of cracks.
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