
mineral
Clear Quartz (Tumbled)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Colorless to white/milky; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None
- Hardness
- 7 on Mohs scale
- Color
- Colorless to white/milky
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless to white/milky; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None
Formation & geological history
Forms in a wide range of geological environments, most commonly from the cooling of magma or in hydrothermal veins and pegmatites. Found across all geological ages.
Uses & applications
Used in electronics (oscillators), clocks, glassmaking, and extensively in jewelry, lapidary arts, and spiritual practice.
Geological facts
Quartz is one of the most abundant minerals in Earth's continental crust. Pure clear quartz is also known as 'Rock Crystal', a name derived from the Greek word 'krystallos' meaning ice.
Field identification & locations
Identify by its hardness (scratches glass), glassy luster, and lack of cleavage. Tumbled stones like this are commonly found in gift shops and mineral kits globally.
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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