
mineral
Yellow or Honey Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Translucent golden-yellow to honey-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Translucent golden-yellow to honey-brown
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: Translucent golden-yellow to honey-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or igneous pegmatites. This specific specimen appears water-worn (tumbled), common in riverbeds or coastal environments where erosion rounds the edges over centuries.
Uses & applications
Used in semi-precious jewelry, as lapidary material, for crystal healing collecting, and in some industrial abrasive applications.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Honey-colored quartz is often mistaken for citrine, though the latter is rarer and usually clearer.
Field identification & locations
Identify by its hardness (will scratch glass), lack of cleavage, and translucent quality. Commonly found in gravel pits, beaches, and mountain streams.
More like this
Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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