
mineral
Milky Quartz with Algae/Iron Staining
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: White to yellowish-green due to surface staining; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- White to yellowish-green due to surface staining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: White to yellowish-green due to surface staining; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Found in hydrothermal veins and pegmatites. This specimen likely weathered out of a vein and spent time in a damp or river environment, leading to the green algae growth and iron oxide staining on the surface.
Uses & applications
Used in glassmaking, abrasives, and as a common landscaping stone. High-purity quartz is used in electronics for its piezoelectric properties.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz gets its cloudiness from tiny fluid inclusions of gas or liquid trapped during crystal growth.
Field identification & locations
Identify by its hardness (it will scratch glass) and lack of cleavage. Common in riverbeds and mountainous regions globally. Look for the waxy or glassy luster on fresh breaks.
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