
mineral
Clear quartz (rock crystal)
Quartz, silicon dioxide (SiO₂)
AI-generated identification · may be incorrectColorless to smoky-clear with a glassy luster and irregular fracture; quartz is trigonal and has no cleavage. Hardness is 7 on the Mohs scale and specific gravity is about 2.65.
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Physical properties
Colorless to smoky-clear with a glassy luster and irregular fracture; quartz is trigonal and has no cleavage. Hardness is 7 on the Mohs scale and specific gravity is about 2.65.
Formation & geological history
Quartz crystallizes from silica-rich fluids in veins and cavities, and also occurs in many igneous and metamorphic rocks. The pictured fragment alone does not establish its geological age or exact origin.
Uses & applications
Quartz is used in glassmaking, electronics, abrasives, and as a gemstone or mineral specimen.
Geological facts
Quartz is one of Earth’s most abundant minerals; its crystals can form six-sided prisms, though this fragment shows no clear crystal termination.
Field identification & locations
The hand-sized, transparent-to-gray fragment is consistent with quartz, but the photo cannot rule out other clear minerals. Check for hardness (it scratches glass) and lack of cleavage; common sources include quartz veins and pegmatites worldwide.
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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