
mineral
Yellow Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Yellow to golden-brown; Luster: Vitreous (glassy); Crystal Structure: Trigonal; Cleavage: None (exhibits conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Yellow to golden-brown
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Yellow to golden-brown; Luster: Vitreous (glassy); Crystal Structure: Trigonal; Cleavage: None (exhibits conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins, pegmatites, and sedimentary environments through the precipitation of silica-rich solutions under varying temperatures and pressures.
Uses & applications
Used in jewelry, ornamental carvings, lapidary arts, and mineral specimen collecting.
Geological facts
The yellow color in quartz is typically caused by natural irradiation acting on aluminum impurities or microscopic inclusions of iron oxide/hydroxide.
Field identification & locations
Can be identified by its distinct yellow coloration, high hardness (scratches glass), and glassy luster. Commonly found worldwide in pegmatites and quartz veins.
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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