
sedimentary
Red Jasper
Chalcedony (SiO2 with Iron inclusions)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Brick red to brownish red; Luster: Dull to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to brownish red
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Brick red to brownish red; Luster: Dull to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic ash or fine-grained sediments, where the presence of iron oxide (hematite) provides the red pigmentation. It is often found in prehistoric sedimentary beds or hydrothermal veins.
Uses & applications
Used widely in ornamental crafts, jewelry (beads, cabochons), landscaping stones, and as a 'grounding' stone in metaphysical practices.
Geological facts
Jasper has been used by ancient civilizations for thousands of years; the Minoans used it for seal stones, and it is mentioned in the Bible as one of the stones in the High Priest's breastplate.
Field identification & locations
Identify it by its distinctive opaque red color, inability to be scratched by a steel knife, and smooth, waxy texture when wet. Commonly found in riverbeds and desert environments.
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