
mineral
Quartz (Chalcedony)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: translucent white to grayish, Luster: waxy to vitreous, Crystal System: Hexagonal (cryptocrystalline), Cleavage: None (conchoidal fracture)
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Physical properties
Hardness: 7 (Mohs scale), Color: translucent white to grayish, Luster: waxy to vitreous, Crystal System: Hexagonal (cryptocrystalline), Cleavage: None (conchoidal fracture)
Formation & geological history
Formed from the deposition of silica-rich fluids in volcanic cavities or sedimentary environments at relatively low temperatures.
Uses & applications
Used in jewelry as gemstones, in decorative lapidary arts, and as a source of high-purity silica for industrial electronics and glass manufacturing.
Geological facts
Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen without high magnification. It has been used since the Bronze Age for making cylinder seals and jewelry.
Field identification & locations
Look for a translucent, waxy appearance and a smooth, curved fracture surface (conchoidal). It is common in riverbeds, desert pavements, and volcanic regions globally.
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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