
sedimentary
Red Jasper
Silicon dioxide (SiO2) with Iron inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Deep red to brownish-red; Luster: Dull to vitreous (waxy when polished); Crystal Structure: Microcrystalline/Trigonal; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Deep red to brownish-red
- Luster
- Dull to vitreous (waxy when polished)
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Deep red to brownish-red; Luster: Dull to vitreous (waxy when polished); Crystal Structure: Microcrystalline/Trigonal; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica-rich fluids in volcanic ash or sedimentary basins. The red color is caused by the inclusion of iron oxide (hematite) during the formation process millions of years ago.
Uses & applications
Used primarily as a gemstone for jewelry (cabochons), lapidary art, decorative carvings, and as a popular specimen for crystal collecting and metaphysical purposes.
Geological facts
In ancient times, Red Jasper was known as the 'stone of endurance' and was frequently used by warriors to decorate their weapons and breastplates for protection.
Field identification & locations
Identify in the field by its opaque nature (light does not pass through it), smooth conchoidal fractures, and distinct red color that does not scratch easily. Commonly found in riverbeds and arid regions globally, including India, Brazil, and the USA.
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