
mineral
Cloudy Quartz / Quartz Tumble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent white to lavender/greyish. Luster: Vitreous/Glassy. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent white to lavender/greyish
- Luster
- Vitreous/Glassy
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent white to lavender/greyish. Luster: Vitreous/Glassy. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed from the crystallization of silica-rich magma or via hydrothermal activity in veins. Quartz is found in almost all geological ages and environments, particularly in igneous and metamorphic rocks.
Uses & applications
Commonly used in crystal healing, home decor, and tumbled for beginner geology collections. High-purity quartz is used in glassmaking and electronics (piezoelectric properties).
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. When purple, it is called Amethyst, and when milky white, it is called Milky Quartz; the specimen in the image appears to be a tumbled fragment of translucent quartz with some light scattering.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and vitreous luster. Commonly found worldwide in riverbeds, mountains, and mines. Collectors often find these as 'pocket stones.'
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary