
mineral
Yellow Quartz (Citrine/Yellow Jasper)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: yellowish-brown to tan; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- yellowish-brown to tan
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: yellowish-brown to tan; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through hydrothermal processes or crystalization from igneous magma. Can also be found as a secondary mineral in sedimentary environments and riverbeds as water-worn pebbles.
Uses & applications
Used widely in lapidary work, jewelry making, ornamental carvings, and as a healing stone in metaphysical practices.
Geological facts
Yellow quartz is often mistaken for gold by novices, though it is much harder. Most commercial 'citrine' is actually heat-treated amethyst, but natural yellow quartz maintains its color through iron impurities or natural irradiation.
Field identification & locations
Identify by its ability to scratch glass and its lack of cleavage. In the field, look for conchoidal (shell-like) fractures on broken edges. Commonly found in quartz veins or as rounded stream pebbles.
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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