
sedimentary
Red Jasper
Silicon Dioxide with Hematite (SiO2 + Fe2O3)
Hardness: 6.5-7 (Mohs scale); Color: Bricky red to deep brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Conchoidal fracture; Specific gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Bricky red to deep brownish-red
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Bricky red to deep brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Conchoidal fracture; Specific gravity: 2.58-2.91.
Formation & geological history
Formed through the accumulation of fine silica-rich materials and iron oxides. Usually occurs in hydrothermal veins or as a secondary mineral in volcanic rocks and sedimentary deposits via silica-rich groundwater precipitation.
Uses & applications
Primarily used as a gemstone for jewelry, cabochons, beads, and decorative ornaments. Historically used for seals, talismans, and as a material for knapping tools.
Geological facts
The red color is caused by impurities of iron (hematite). In ancient civilizations, it was known as the 'rain bringer' and was frequently mentioned in various religious texts and mythologies as a stone of protection and strength.
Field identification & locations
Identify by its opaque nature (unlike carnelian which is translucent) and dull waxy to vitreous luster. Commonly found in riverbeds or beaches where silica-rich rocks weather out. Major deposits are in India, Brazil, Madagascar, and the southwestern USA.
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