
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: White to creamy tan/off-white, Luster: Vitreous to waxy (when weathered), Crystal structure: Trigonal/Hexagonal, Cleavage: None (Conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: White to creamy tan/off-white, Luster: Vitreous to waxy (when weathered), Crystal structure: Trigonal/Hexagonal, Cleavage: None (Conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal fluids or within igneous and metamorphic rocks. This specific specimen is well-rounded, indicating it has undergone significant mechanical weathering and transport in a river or beach environment.
Uses & applications
Commonly used in construction aggregate, landscaping, glass manufacturing, and as a raw material for electronic components. High-purity quartz is essential for semiconductor production.
Geological facts
Quartz is the most abundant and widely distributed mineral found at Earth's surface. Rounded pebbles like this one are often referred to as 'river rocks' and have been smoothed by thousands of years of water erosion.
Field identification & locations
Identify in the field by its hardness (it should scratch glass easily) and its lack of cleavage. It is ubiquitous in riverbeds, glacial deposits, and along coastlines worldwide.
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Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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