
mineral
Milky Quartz (Water-worn Pebble)
Quartz (Silicon Dioxide) - SiO2
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Cloudy white to grayish with dark inclusions; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Cloudy white to grayish with dark inclusions
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Cloudy white to grayish with dark inclusions; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal veins or as a primary constituent in igneous and metamorphic rocks. This specific specimen has been rounded and smoothed through fluvial or marine erosion (water-worn).
Uses & applications
Industrial use as an abrasive, in glassmaking, and electronics (due to piezoelectric properties). In this tumbled form, it is used for landscaping, aquarium gravel, and low-cost lapidary work.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. The 'milky' appearance is caused by tiny fluid inclusions of gas or liquid trapped during crystal growth.
Field identification & locations
Identify in the field by its ability to scratch glass, lack of cleavage, and smooth, rounded surface if found in riverbeds. It is found globally in almost all geological environments.
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