
mineral
Yellow Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Yellow to golden-yellow; Luster: Vitreous; Crystal System: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Yellow to golden-yellow
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Yellow to golden-yellow; Luster: Vitreous; Crystal System: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins and pegmatites through the crystallization of silica-rich solutions under high pressure and temperature over millions of years.
Uses & applications
Used in gemstone and jewelry creation, metaphysical practices, and mineral collections.
Geological facts
Yellow quartz is often naturally colored by iron impurities within the silicon dioxide crystal lattice. It is sometimes confused with citrine, though natural citrine is rarer and typically results from natural heat treatment of smoky quartz.
Field identification & locations
Can be identified by its distinctive yellow-to-amber color, conchoidal fracture, glassy luster, and ability to scratch glass due to its high hardness. Commonly found worldwide in association with pegmatites and hydrothermal deposits.
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Other mineral specimens
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