
mineral
Red Jasper
Silicon Dioxide (SiO2) with Hematite inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Brick red to brownish red due to iron; Luster: Vitreous to dull; Crystal Structure: Hexagonal (trigonal) microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to brownish red due to iron
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Brick red to brownish red due to iron; Luster: Vitreous to dull; Crystal Structure: Hexagonal (trigonal) microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from hydrothermal solutions or in sedimentary environments where volcanic ash or fine sediment is replaced by silica. Its red color comes from high iron content. It can be found in rocks from the Precambrian to recent geological eras.
Uses & applications
Commonly used in jewelry making for cabochons and beads, ornamental carvings, pocket stones for metaphysical practices, and historically as a component in mosaics and architectural decoration.
Geological facts
Ancient Egyptians wore Red Jasper amulets shaped like the knot of Isis to protect the wearer. It is known as the 'Supreme Nurturer' in gemstone folklore. It is a variety of chalcedony that is opaque, unlike agates which are translucent.
Field identification & locations
Identify in the field by its deep red color, extreme hardness (it will scratch glass), and opaque nature. It is commonly found in riverbeds, desert pavements, and rocky beaches worldwide, notably in India, Brazil, and the Southwestern USA.
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