
mineral
Quartz (Citrine or Iron-Stained variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Yellowish-tan to brownish-orange; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Yellowish-tan to brownish-orange
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Yellowish-tan to brownish-orange; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed in igneous or metamorphic environments through hydrothermal processes. Silica-rich fluids crystallize in veins or cavities within rocks. Geological age varies from millions to billions of years depending on the host rock formation.
Uses & applications
Common industrial use in glassmaking and abrasives. In this specimen's form, it is primarily used for jewelry, crystal healing, or amateur mineral collecting.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. This specific specimen appears to be a 'double-terminated' crystal or a river-worn fragment, naturally shaped by water erosion or growth in a pocket.
Field identification & locations
Identify in the field by its hardness (it will scratch glass) and lack of cleavage. This specimen shows a characteristic translucent tan translucency common in iron-included quartz found in gravel pits or dry riverbeds.
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