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

Red Jasper

Microcrystalline Quartz (Chalcedony), SiO2

Mohs hardness of 6.5 to 7, typically red, reddish-brown, or brick-red with minor white or dark banding, waxy to vitreous luster, cryptocrystalline or microfibrous crystal structure, conchoidal fracture, specific gravity of 2.58 to 2.91.

Identified More sedimentary
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Physical properties

Mohs hardness of 6.5 to 7, typically red, reddish-brown, or brick-red with minor white or dark banding, waxy to vitreous luster, cryptocrystalline or microfibrous crystal structure, conchoidal fracture, specific gravity of 2.58 to 2.91.

Formation & geological history

Forms through the hydrothermal deposition of silica-rich solutions or the accumulation of silica in marine sedimentary environments, often replacing organic material or filling fractures in volcanic rock. Geological age varies widely depending on the deposit.

Uses & applications

Widely used for making ornamental objects, cabochons, beads, small carvings, and polished display pieces in the jewelry and lapidary arts.

Geological facts

Red jasper has been used since ancient times by various civilizations for amulets, seals, and weaponry. The red color is primarily due to iron oxide (hematite) inclusions within the silica matrix.

Field identification & locations

Easily identified by its opaque red color, hardness that easily scratches glass, and smooth conchoidal fracture. Found worldwide, particularly in Brazil, India, Russia, and the United States.