Rock Identifier
Red Jasper (Microcrystalline Quartz (Chalcedony), SiO2) — sedimentary
sedimentary

Red Jasper

Microcrystalline Quartz (Chalcedony), SiO2

Hardness of 6.5 to 7 on the Mohs scale, deep red to brownish-red color due to iron oxide impurities, waxy to dull luster, cryptocrystalline or microcrystalline structure with conchoidal fracture, specific gravity of 2.58 to 2.91.

Identified More sedimentary
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Physical properties

Hardness of 6.5 to 7 on the Mohs scale, deep red to brownish-red color due to iron oxide impurities, waxy to dull luster, cryptocrystalline or microcrystalline structure with conchoidal fracture, specific gravity of 2.58 to 2.91.

Formation & geological history

Forms in silica-rich aqueous environments, often through the precipitation of silica in sedimentary rocks, hydrothermal veins, or volcanic ash beds, where iron oxide impurities become trapped during crystallization.

Uses & applications

Widely used for ornamental objects, cabochons, beads, carvings, and polished display pieces in lapidary arts as well as a popular specimen for mineral collectors.

Geological facts

Red jasper has been utilized since ancient times for talismans, seals, and jewelry. The ancient Egyptians often carved it into amulets representing the girdle of Isis.

Field identification & locations

Easily identified by its opaque deep red color, conchoidal fracture, and hard scratch resistance (scratches glass). Found worldwide, with notable deposits in India, Brazil, Russia, Australia, and the western United States.