
Mineral
Red Jasper
SiO2 (Microcrystalline Quartz)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale, Color: Red to brownish-red with white or gray veins, Luster: Vitreous to dull, Crystal structure: Trigonal (microcrystalline), Cleavage: None
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 on Mohs scale, Color: Red to brownish-red with white or gray veins, Luster: Vitreous to dull, Crystal structure: Trigonal (microcrystalline), Cleavage: None
Formation & geological history
Formed from silica-rich fluids that percolate through rocks, depositing microcrystalline quartz in veins and cavities. The red color is due to iron inclusions. Can form in various environments.
Uses & applications
Used in lapidary arts for cabochons, beads, and carvings. Also popular as a healing stone and for collecting.
Geological facts
Red jasper has been used since antiquity for engraved gems and seals. It was a favorite stone in the ancient world and is referenced in biblical texts.
Field identification & locations
Identify by its solid red color and opacity. Look for subconchoidal fracture and hardness greater than glass. Commonly found worldwide, notably in India, Russia, Brazil, and the USA.
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Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary