
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Hematite (Fe2O3) inclusions
Hardness: 6.5-7 (Mohs scale); Color: Brick red to brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Brick red to brownish-red
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Brick red to brownish-red; Luster: Vitreous to dull; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91.
Formation & geological history
Formed through the deposition of silica-rich fluids in cracks and cavities within other rocks, typically during hydrothermal processes or as sedimentary deposits. The red color is caused by the oxidation of iron (hematite) during formation.
Uses & applications
Primarily used in jewelry for cabochons, beads, and wire-wrapped pendants; also used in decorative ornaments, stone carvings, and as a popular specimen for crystal healing and mineral collectors.
Geological facts
Jasper has been used as a gemstone since antiquity and is mentioned in various historical texts, including the Bible. King's seals in ancient Mesopotamia were often carved from Red Jasper due to its durability.
Field identification & locations
Identify in the field by its opaque nature (unlike agate), smooth waxy feel when tumbled, and a streak test that usually produces a white or pale color despite the red body. It is commonly found in India, Russia, Brazil, and the USA (southwestern states).
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