
mineral
Milky quartz
Quartz (SiO₂), likely massive or drusy quartz
AI-generated identification · may be incorrectTypically white to translucent with a vitreous luster; Mohs hardness 7, no cleavage, conchoidal fracture, and hexagonal crystal structure. The specimen appears irregular and granular, possibly coated with iron-oxide staining or attached matrix.
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Physical properties
Typically white to translucent with a vitreous luster; Mohs hardness 7, no cleavage, conchoidal fracture, and hexagonal crystal structure. The specimen appears irregular and granular, possibly coated with iron-oxide staining or attached matrix.
Formation & geological history
Forms when silica-rich fluids crystallize in fractures, veins, cavities, or pegmatites; individual pieces may range from ancient Precambrian to much younger hydrothermal deposits. Exact age and locality cannot be determined from the image.
Uses & applications
Common quartz is used in glass, ceramics, abrasives, electronics, and engineered stone; attractive pieces are sold as inexpensive mineral specimens or lapidary material.
Geological facts
Quartz is one of Earth’s most abundant minerals and is chemically identical to amethyst, citrine, and rock crystal, with color determined mainly by impurities or defects.
Field identification & locations
Identify by its glassy luster, hardness sufficient to scratch ordinary glass, lack of cleavage, and white translucency. Common worldwide in quartz veins, granites, pegmatites, and metamorphic rocks.
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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