
mineral
Milky quartz
Quartz (silicon dioxide, SiO₂)
AI-generated identification · may be incorrectMohs hardness 7; translucent to opaque white-beige with a vitreous to slightly greasy luster and uneven fracture. Trigonal crystal structure; no cleavage. The rounded shape and frosted surface suggest natural water wear.
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Physical properties
Mohs hardness 7; translucent to opaque white-beige with a vitreous to slightly greasy luster and uneven fracture. Trigonal crystal structure; no cleavage. The rounded shape and frosted surface suggest natural water wear.
Formation & geological history
Forms when silica-rich fluids crystallize in veins and cavities, commonly in igneous and metamorphic rocks; quartz deposits occur across many geological ages.
Uses & applications
Used as a decorative and collectible specimen, and industrial quartz is used in glass, electronics, and engineered stone.
Geological facts
Quartz is among Earth’s most abundant minerals and resists weathering, allowing it to persist in sediments and river gravels.
Field identification & locations
Common worldwide in quartz veins, pegmatites, and stream deposits. Milky color and hardness are useful clues; a glass scratch test can help distinguish it from softer lookalikes.
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
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igneous
Unidentified pink-and-gray mineral or rock specimen
Undetermined; the image is too blurry for reliable identification
mineral