
sedimentary
Red Jasper
Silicon dioxide (SiO2) with iron oxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Brick red to deep terracotta; Luster: Dull to vitreous; Crystal structure: Hexagonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to deep terracotta
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Brick red to deep terracotta; Luster: Dull to vitreous; Crystal structure: Hexagonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from hydrothermal solutions or within volcanic and sedimentary rocks. The red color is caused by the inclusion of hematite (iron) during the silicification process.
Uses & applications
Commonly used as a gemstone for jewelry (cabochons, beads), decorative carvings, spiritual/metaphysical practices, and as an ornamental stone in polished mosaics.
Geological facts
Jasper is an opaque variety of chalcedony. It has been used since antiquity; ancient Egyptians used red jasper to create amulets associated with the blood of Isis. It is often found in large chunks or boulders rather than as individual crystals.
Field identification & locations
Identify by its opaque red color, smooth waxy feel when polished, and conchoidal (shell-like) fracture edges. It can be found worldwide, with major deposits in India, Russia, Brazil, and the USA.
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