
mineral
Milky Quartz with Mineral Inclusions
Silicon Dioxide (SiO2) with miscellaneous inclusions
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Opaque white to yellowish with dark green/black patches; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Opaque white to yellowish with dark green/black patches
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Opaque white to yellowish with dark green/black patches; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from hydrothermal veins or cooling magma where silica-rich fluids crystallized. The dark inclusions typically represent hydrothermal minerals like chlorite, hornblende, or mica that were trapped during growth.
Uses & applications
Used in glass manufacturing, electronics (as oscillators), abrasives, and as decorative stone or gravel in landscaping.
Geological facts
Milky quartz is the most common variety of crystalline quartz. Its white color is caused by tiny bubbles of gas or liquid trapped during the crystal's formation.
Field identification & locations
Identify in the field by its hardness (will scratch glass), opaque white color, and lack of cleavage. Often found in riverbeds or as veins in igneous rock outcrops.
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Epidote
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Pegmatite with Tourmaline and Quartz
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Granite
Granite (Phaneritic intrusive igneous rock)
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