
mineral
Quartz (Microcrystalline variety)
Silicon Dioxide (SiO2)
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
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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
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral