
mineral
Clear Quartz Point
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 Mohs; Color: Colorless/Transparent; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
- Hardness
- 7 Mohs
- Color
- Colorless/Transparent
- Luster
- Vitreous
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Physical properties
Hardness: 7 Mohs; Color: Colorless/Transparent; Luster: Vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
Formation & geological history
Formed primarily in igneous rocks such as granite pegmatites or in hydrothermal veins where silica-rich fluids cool and crystallize over millions of years.
Uses & applications
Used in electronics for its piezoelectric properties, glassmaking, clocks, healing crystals, and jewelry.
Geological facts
Quartz is one of the most abundant minerals in Earth's crust. 'Rock Crystal' refers to the purest, water-clear variety shown here.
Field identification & locations
Identified by its hexagonal prism shape, lack of cleavage, and ability to scratch glass. Commonly found in mountainous regions worldwide, especially Brazil and Arkansas.
More like this
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