
mineral
Milky Quartz with Mineral Inclusions
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent white to milky with black/grey banding; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture.
- Hardness
- 7 on Mohs scale
- Color
- Translucent white to milky with black/grey banding
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent white to milky with black/grey banding; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture.
Formation & geological history
Formed from silica-rich hydrothermal fluids cooling in veins or cavities within igneous or metamorphic host rocks. The dark bands likely represent structural fractures filled with iron, manganese oxides, or carbonaceous materials.
Uses & applications
Quartz is used extensively in glassmaking, electronics (piezoelectric properties), and as an abrasive. Polished river-worn specimens are popular in decorative landscaping and as beginner collectibles.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. This specific specimen shows 'water-worn' smoothing, indicating it was likely found in a riverbed or coastal area.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), lack of cleavage, and waxy luster. Common in mountainous regions, riverbeds, and gravel deposits worldwide.
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Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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