
mineral
Milky Quartz Pebble with Inclusions
Quartz (SiO2) with chlorite or mica inclusions
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Off-white to milky white with greyish-green inclusions. Luster: Vitreous to dull/waxy when weathered. Crystal structure: Trigonal (microcrystalline/massive). Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- Off-white to milky white with greyish-green inclusions
- Luster
- Vitreous to dull/waxy when weathered
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Physical properties
Hardness: 7 on Mohs scale. Color: Off-white to milky white with greyish-green inclusions. Luster: Vitreous to dull/waxy when weathered. Crystal structure: Trigonal (microcrystalline/massive). Cleavage: None (conchoidal fracture).
Formation & geological history
Formed in hydrothermally active veins or pegmatites where silica-rich fluids crystallized slowly underground, enclosing secondary minerals like chlorite or mica, before being eroded into a smooth river/beach pebble.
Uses & applications
Mainly collected as a beach pebble or decorative specimen. Pure quartz is used in glassmaking, electronics, and abrasives.
Geological facts
Milky quartz gets its cloudy appearance from microscopic liquid or gas inclusions trapped during crystal growth millions of years ago.
Field identification & locations
Can be identified in the field by its hardness (scratches glass readily and cannot be scratched by steel), smooth water-worn texture, and distinct whitish matrix contrast with dark mineral veins or inclusions.
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