
mineral
Clear Quartz (Rock Crystal)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal (prism with pyramidal ends); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Colorless/Transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal (prism with pyramidal ends); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through the crystallization of molten magma or from hydrothermal veins. It can occur in nearly every geological environment and is found in all three rock types (igneous, sedimentary, and metamorphic).
Uses & applications
Used in glassmaking, gemstone jewelry, precision electronics (piezoelectric properties for oscillators), ceramics, and as a popular metaphysical or decorative specimen.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure clear quartz is known as 'Rock Crystal' and has been used for carving crystal balls and cameos since antiquity.
Field identification & locations
Identify in the field by its hardness (it can scratch glass), lack of cleavage, and vertical striations on crystal faces. It is commonly found in Arkansas (USA), Brazil, and the Alps.
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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