
mineral
Milky Quartz with Chlorite/Mica inclusions
Silicon Dioxide (SiO2) with inclusions
Hardness: 7 (Mohs scale); Color: White to grey with green/black veining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- White to grey with green/black veining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: White to grey with green/black veining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from hydrothermal veins and igneous intrusions. The quartz crystallized from silica-rich fluids deep in the Earth's crust, often trapping minerals like chlorite or mica during the growth process.
Uses & applications
Decorative stone, landscape rock, high-quality quartz is used in jewelry and quartz-based glass manufacturing.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz gets its opaque color from microscopic fluid inclusions trapped during crystal growth.
Field identification & locations
Can be identified in the field by its hardness (it will easily scratch glass) and lack of cleavage. Commonly found in riverbeds, mountain ranges, and near volcanic sites worldwide.
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