
sedimentary
Red Jasper
Silicon Dioxide (Microcrystalline Quartz, SiO2)
Hardness: 6.5 to 7 on the Mohs scale; Color: Red to reddish-brown due to iron inclusions; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.58 to 2.91
- Hardness
- 6
- Color
- Red to reddish-brown due to iron inclusions
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale; Color: Red to reddish-brown due to iron inclusions; Luster: Vitreous to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.58 to 2.91
Formation & geological history
Formed through the hydrothermal deposition of silica-rich fluids or the accumulation of silica-rich radiolarian ooze on ocean floors, often occurring within sedimentary or volcanic environments over millions of years.
Uses & applications
Used primarily in lapidary work, making cabochons, beads, small carvings, ornamental objects, and as a semi-precious gemstone.
Geological facts
Red jasper has been used since ancient times for talismans, seals, and jewelry. The ancient Egyptians carved amulets from it, associating the stone with the blood of the goddess Isis.
Field identification & locations
Can be identified in the field by its opaque red color, waxy-to-dull luster, and high hardness (scratches glass). It is commonly found in riverbeds, glacial tills, and areas with ancient marine or volcanic deposits.
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