
mineral
Milky Quartz (Carved Star Beads)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent white to milky white. Luster: Vitreous to waxy. Crystal structure: Trigonal/Hexagonal (though carved here). Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent white to milky white
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent white to milky white. Luster: Vitreous to waxy. Crystal structure: Trigonal/Hexagonal (though carved here). Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
Formation & geological history
Forms in hydrothermal veins, pegmatites, and metamorphic rock environments across many geological periods. The milky appearance is caused by tiny fluid inclusions trapped during crystal growth.
Uses & applications
Carved and drilled into star-shaped beads used for jewelry making, crafts, and decorative items. Quartz is also widely used in optics, electronics, and abrasives.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Fluid inclusions in milky quartz contain microscopic bubbles of liquid and gas that were present when the crystal formed millions of years ago.
Field identification & locations
Identified by its hardness (scratches glass, cannot be scratched by steel), milky translucent appearance, and lack of cleavage. Commonly found worldwide in Brazil, Madagascar, the USA, and India.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary