
mineral
Quartz crystal fragment
Quartz (SiO₂), likely a small clear-to-gray crystal fragment
AI-generated identification · may be incorrectHardness 7 Mohs; translucent grayish-clear with a vitreous luster and irregular, sharp fracture surfaces. The small, partly reflective fragment does not show enough detail to determine crystal form or cleavage reliably.
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Physical properties
Hardness 7 Mohs; translucent grayish-clear with a vitreous luster and irregular, sharp fracture surfaces. The small, partly reflective fragment does not show enough detail to determine crystal form or cleavage reliably.
Formation & geological history
Quartz commonly crystallizes from silica-rich fluids in veins and cavities within igneous and metamorphic rocks, over a wide range of geological ages. The fragment’s source and age cannot be determined from the photograph.
Uses & applications
Quartz is widely used in glass, electronics, abrasives, and construction; attractive, larger crystals are used in jewelry and collections. This piece appears too small and irregular for significant commercial use.
Geological facts
Quartz is one of Earth’s most abundant minerals and lacks true cleavage, typically breaking with a curved or irregular fracture.
Field identification & locations
A translucent appearance and glassy luster are consistent with quartz, but the image cannot rule out another clear mineral or glass. A hardness test on an inconspicuous spot—quartz can scratch glass—could help distinguish it; common sources include veins, river gravels, and weathered rock.
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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