
mineral
Quartz (Microcrystalline variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: tan to milky white, Luster: Vitreous to waxy when wet, Crystal Structure: Trigonal (often massive in this form), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: tan to milky white, Luster: Vitreous to waxy when wet, Crystal Structure: Trigonal (often massive in this form), Specific Gravity: 2.65
Formation & geological history
Formed through the cooling of silica-rich magma or from hydrothermal solutions in voids of other rocks. Can be found in almost all geological environments and ages.
Uses & applications
Used in glassmaking, electronics (piezoelectric properties), abrasives, and as decorative gravel or gemstones.
Geological facts
Quartz is one of the most abundant minerals in Earth's crust. It is highly resistant to chemical and physical weathering, which is why it is commonly found as pebbles in riverbeds.
Field identification & locations
Identify by its ability to scratch glass and lack of cleavage. Commonly found in riverbeds, mountains, and beaches worldwide. This specific specimen appears to be a water-worn quartz pebble.
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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