
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs), Color: Translucent grey/brown (smoky variety), Luster: Vitreous to waxy (water-worn), Crystal System: Hexagonal (trigonal), No cleavage, Conchoidal fracture.
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Physical properties
Hardness: 7 (Mohs), Color: Translucent grey/brown (smoky variety), Luster: Vitreous to waxy (water-worn), Crystal System: Hexagonal (trigonal), No cleavage, Conchoidal fracture.
Formation & geological history
Formed in various geological environments but predominantly in igneous and metamorphic rocks; this specific specimen has been smoothed and rounded by long-term water erosion in a river or beach environment.
Uses & applications
Used in construction aggregate, landscaping, glass making, and as decorative river stones. High-purity quartz is used in electronics.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. These rounded smooth pebbles are often called 'river rocks' and can survive millions of years of erosion due to their high hardness.
Field identification & locations
Identify by its hardness (scratches glass), translucent appearance, and lack of visible grains. Commonly found in riverbeds, glacial deposits, and coastal beaches.
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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