
mineral
Quartz (Water-worn Pebbles)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, vitreous to greasy luster, translucent to transparent, conchoidal fracture, and distinct lack of cleavage. Specific gravity is approximately 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, vitreous to greasy luster, translucent to transparent, conchoidal fracture, and distinct lack of cleavage. Specific gravity is approximately 2.65.
Formation & geological history
Formed in a wide variety of geological environments, including igneous, metamorphic, and sedimentary rocks. These particular specimens are water-worn alluvial or beach pebbles shaped by prolonged mechanical weathering and transport in water.
Uses & applications
Used in glassmaking, electronics, abrasive materials, ornamental objects, and lapidary arts.
Geological facts
Quartz is one of the most abundant minerals in the Earth's continental crust. While the user suggested 'topaz', these smooth, rounded pebbles lack the perfect basal cleavage and higher specific gravity of topaz, aligning instead with common water-worn quartz or potentially water-worn beryl/topaz given the locality, though visually and physically quartz is the most direct match.
Field identification & locations
Can be identified in the field by its hardness (scratches glass easily), lack of cleavage, and resistance to chemical and mechanical weathering. Found worldwide in riverbeds, beaches, and sedimentary deposits.
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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