Rock Identifier
Jasper (specifically Polychrome or Desert Jasper) (Silicon Dioxide (SiO2) with iron oxide and other mineral impurities) — sedimentary (chemical/biological origin)
sedimentary (chemical/biological origin)

Jasper (specifically Polychrome or Desert Jasper)

Silicon Dioxide (SiO2) with iron oxide and other mineral impurities

Hardness: 6.5-7 on Mohs scale. Color: Multicolored (red, yellow, brown, grey). Luster: Vitreous to waxy. Crystal structure: Cryptocrystalline (microscopic quartz crystals). Cleavage: None (conchoidal fracture). Specific gravity: 2.58-2.91.

Hardness
6
Color
Multicolored (red, yellow, brown, grey)
Luster
Vitreous to waxy

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Physical properties

Hardness: 6.5-7 on Mohs scale. Color: Multicolored (red, yellow, brown, grey). Luster: Vitreous to waxy. Crystal structure: Cryptocrystalline (microscopic quartz crystals). Cleavage: None (conchoidal fracture). Specific gravity: 2.58-2.91.

Formation & geological history

Formed when silica-rich fluids permeate volcanic ash or sedimentary rock, slowly replacing organic or mineral matter while retaining high concentrations of iron oxides. These typically date from the Jurassic to the Tertiary periods.

Uses & applications

Predominantly used for lapidary work, jewelry (cabochons), ornamental carvings, and as decorative rough for rock collectors.

Geological facts

Jasper has been used by ancient civilizations for thousands of years to create seals and amulets. The name 'Jasper' is derived from the Greek word 'iaspis', meaning 'spotted stone'. It is an opaque variety of chalcedony.

Field identification & locations

Identify in the field by its smooth, shell-like (conchoidal) fracture surfaces and its inability to be scratched by a steel knife. It is commonly found in the deserts of Madagascar, Oregon, and the Southwestern United States. Collectors should look for vibrant banding and lack of transparency.