
mineral
Milky and Smoky Quartz Cobble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: mix of white (milky) and grey/black (smoky); Luster: Vitreous to greasy; Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); SG: 2.65
- Hardness
- 7 on Mohs scale
- Color
- mix of white (milky) and grey/black (smoky)
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: mix of white (milky) and grey/black (smoky); Luster: Vitreous to greasy; Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); SG: 2.65
Formation & geological history
Formed from silica-rich hydrothermal fluids or within igneous pegmatites. This specimen shows significant rounding, suggesting it was transported and eroded in a high-energy water environment like a riverbed or shoreline.
Uses & applications
Quartz is used in glassmaking, electronics (piezoelectric properties), and as an abrasive. While this cobble is not gem-quality, it has decorative and educational value for collectors.
Geological facts
The smoky coloration is caused by natural radiation from surrounding rocks acting on trace aluminum impurities within the crystal structure. It is one of the most abundant minerals on Earth.
Field identification & locations
Identify by its hardness (it will scratch glass), lack of cleavage, and translucent zones. Commonly found in gravel pits, riverbanks, and glacial till. Look for the characteristic glassy luster on broken faces.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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