
mineral
Milky quartz
Quartz (silicon dioxide, SiO₂)
AI-generated identification · may be incorrectHardness 7 Mohs; white to translucent with a vitreous-to-waxy luster and irregular fracture. Trigonal crystal system, though this small rough fragment shows no obvious crystal form or cleavage.
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Physical properties
Hardness 7 Mohs; white to translucent with a vitreous-to-waxy luster and irregular fracture. Trigonal crystal system, though this small rough fragment shows no obvious crystal form or cleavage.
Formation & geological history
Forms when silica-rich fluids crystallize in veins or cavities, and is also common in igneous and metamorphic rocks. Quartz is widespread across rocks of many geological ages.
Uses & applications
Used for ornaments, beads, and mineral collecting; industrial quartz is important in glass, ceramics, and electronics, though this fragment is too small for most industrial uses.
Geological facts
Quartz is one of Earth’s most abundant minerals and has no true cleavage, commonly breaking with curved or uneven surfaces.
Field identification & locations
The white, cloudy appearance and glassy luster are consistent with milky quartz, but the photo alone cannot confirm identification. Common worldwide, especially in quartz veins and granitic or metamorphic terrain.
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Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
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sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Unidentified pink-and-gray mineral or rock specimen
Undetermined; the image is too blurry for reliable identification
mineral