sedimentary

Red Jasper (Tumbled)

Silicon Dioxide (SiO2) with iron oxide inclusions

AI-generated identification · may be incorrect

Hardness: 6.5-7 (Mohs); Color: Deep red to brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline quartz); Cleavage: None, conchoidal fracture

Hardness: 6
Color: Deep red to brownish-red
Luster: Vitreous to dull

Identified July 12, 2026More sedimentary →

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Physical properties

Hardness: 6.5-7 (Mohs); Color: Deep red to brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline quartz); Cleavage: None, conchoidal fracture

Formation & geological history

Formed through the deposition of silica in hydrothermal veins or volcanic ash, combined with iron inclusions that provide the red hue. Typically sedimentary but can be associated with volcanic environments.

Uses & applications

Used primarily in jewelry (cabochons, beads), decorative objects, and is highly valued in metaphysical communities as a 'supreme nurturer'.

Geological facts

The vibrant red color is caused by the presence of iron oxide (hematite). It has been used for centuries in seals, amulets, and ring stones for its believed protective qualities.

Field identification & locations

Identify by its opaque quality and deep brick-red color. It is common in riverbeds and arid regions globally; massive deposits are found in India, Russia, Brazil, and the USA (Southwest).