
mineral
Milky quartz (probable)
Quartz, silicon dioxide (SiO₂)
AI-generated identification · may be incorrectWhite to pale yellow, translucent, and vitreous; likely hardness 7 on the Mohs scale, with no cleavage and irregular/conchoidal fracture. The rough, granular appearance may reflect weathering or attached host rock.
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Physical properties
White to pale yellow, translucent, and vitreous; likely hardness 7 on the Mohs scale, with no cleavage and irregular/conchoidal fracture. The rough, granular appearance may reflect weathering or attached host rock.
Formation & geological history
Quartz crystallizes from silica-rich igneous and hydrothermal fluids and commonly occurs in veins and pegmatites; individual specimens may range from Precambrian to recent geological ages. Exact origin cannot be determined from the photograph.
Uses & applications
Common quartz is used in glass, ceramics, abrasives, engineered stone, and electronics; attractive pieces are collected or used decoratively. This small rough specimen has modest commercial value.
Geological facts
Milky quartz appears cloudy because microscopic fluid inclusions, fractures, or defects scatter light. A steel file should not scratch it, while quartz can scratch ordinary glass.
Field identification & locations
Look for a glassy luster, lack of cleavage, conchoidal fracture, and hardness near 7; acid tests are unnecessary. Common worldwide, especially in hydrothermal 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
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