
mineral
Quartz (Milky/Gravel variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous (glassy) to waxy; Crystal structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous (glassy) to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous (glassy) to waxy; Crystal structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Quartz forms in all types of environments (igneous, metamorphic, sedimentary) but often crystallizes from cooling magma or hydrothermal veins. This specific rounded specimen likely originated as a vein mineral and was polished by water erosion in a river or stream bed over thousands of years.
Uses & applications
Used in glassmaking, electronics (piezoelectric properties), abrasives, and as a common component in concrete. In small gravel form, it is used for landscaping or as a basic pocket stone for collectors.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is clear; the 'milky' appearance of this specimen is caused by tiny fluid inclusions of gas or liquid trapped during the crystal's growth.
Field identification & locations
Identify in the field by its hardness (it should easily scratch glass) and lack of cleavage planes. Found globally in riverbeds, mountains, and beaches. For collectors, look for the 'conchoidal' fracture—the way it breaks like glass.
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