
mineral
Yellow Quartz (Chalcedony)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Pale yellow to honey-orange; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.64.
- Hardness
- 6
- Color
- Pale yellow to honey-orange
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Pale yellow to honey-orange; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.64.
Formation & geological history
Formed by the deposition of silica-rich fluids in volcanic cavities, sedimentary veins, or through the weathering of larger quartz crystals. This specimen appears water-worn, suggesting secondary transport in a river or stream bed.
Uses & applications
Used primarily for lapidary work (cabochons), jewelry, and as decorative stone ('tumble stones'). Also highly popular in the metaphysical and collecting communities as a solar plexus chakra stone.
Geological facts
When chalcedony displays this specific translucent yellow hue, it is often commercially labeled as 'Yellow Jasper' or 'Yellow Quartzite' despite being technically a microcrystalline quartz. It is extremely resistant to chemical weathering.
Field identification & locations
Identify by its waxy luster, translucency when held to light, and inability to be scratched by a steel knife. It is commonly found in gravel beds, beaches, and desert washes worldwide.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
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Granite
Granite (Phaneritic intrusive igneous rock)
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