
mineral
Milky quartz
Quartz (SiO₂), typically massive rather than visibly crystalline
AI-generated identification · may be incorrectHardness 7 Mohs; white to translucent with a vitreous-to-greasy luster and no cleavage. It has a trigonal crystal structure, though this piece appears granular or massive.
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Physical properties
Hardness 7 Mohs; white to translucent with a vitreous-to-greasy luster and no cleavage. It has a trigonal crystal structure, though this piece appears granular or massive.
Formation & geological history
Forms when silica-rich fluids crystallize in fractures and veins, or during cooling of silica-rich magma; quartz is common in rocks of many geological ages.
Uses & applications
Used in glassmaking, electronics, and decorative stone; small rough pieces are mainly collected or used for crafts.
Geological facts
Quartz is one of Earth’s most abundant minerals and resists weathering, so it commonly persists in soils and stream sediments.
Field identification & locations
The pale, glassy appearance and hardness are consistent with milky quartz; a scratch test against glass can help distinguish it from softer minerals. It occurs worldwide, especially in quartz veins and granitic terrains.
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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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Granite
Granite (Phaneritic intrusive igneous rock)
igneous