Rock Identifier
Red Jasper (Silicon Dioxide with iron impurities (Quartz variety, SiO2)) — sedimentary
sedimentary

Red Jasper

Silicon Dioxide with iron impurities (Quartz variety, SiO2)

Hardness: 6.5-7 on Mohs scale; Color: Red, reddish-brown, brick red with white/lighter quartz or chalcedony veins; Luster: Vitreous to dull; Crystal structure: Microcrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91

Hardness
6
Luster
Vitreous to dull
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 on Mohs scale; Color: Red, reddish-brown, brick red with white/lighter quartz or chalcedony veins; Luster: Vitreous to dull; Crystal structure: Microcrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91

Formation & geological history

Formed through the hydrothermal deposition of silica-rich fluids or accumulation of silica-rich radiolarian ooze in marine environments, often associated with iron-rich sedimentary deposits. Geological age varies widely depending on the formation site, ranging from Precambrian to Cenozoic.

Uses & applications

Used primarily in lapidary work, decorative carvings, cabochons for jewelry, and ornamental objects. Also popular as a specimen for rock collectors.

Geological facts

Jasper has been used since ancient times (dating back over 5,000 years) for amulets, seals, and tools. Red jasper is specifically mentioned in various historical texts and mythologies for its supposed grounding and protective properties.

Field identification & locations

Can be identified in the field by its opaque red color, microcrystalline texture, and hardness that scratches glass. Common locations include India, Brazil, Russia, Madagascar, and various parts of the United States.