
mineral
Milky quartz
Quartz (silicon dioxide, SiO₂)
AI-generated identification · may be incorrectWhite to translucent, vitreous-to-waxy luster, uneven fracture, and no obvious cleavage; Mohs hardness 7 and specific gravity about 2.65. The cloudy appearance comes from microscopic fluid inclusions, fractures, or impurities.
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Physical properties
White to translucent, vitreous-to-waxy luster, uneven fracture, and no obvious cleavage; Mohs hardness 7 and specific gravity about 2.65. The cloudy appearance comes from microscopic fluid inclusions, fractures, or impurities.
Formation & geological history
Forms when silica-rich hydrothermal fluids crystallize in veins and cavities, commonly in igneous and metamorphic rocks. Individual specimens may range from ancient Precambrian material to much younger geological formations.
Uses & applications
Used as a decorative and collectible mineral, aggregate, and source material for glass and silicon products; attractive pieces may be polished, though this specimen appears rough and common.
Geological facts
Quartz is one of Earth’s most abundant minerals and is chemically resistant to weathering. Milky quartz commonly occurs with feldspar, mica, metallic ores, and other vein minerals.
Field identification & locations
Likely milky quartz based on its white, translucent, massive texture; it can be distinguished from calcite by its greater hardness—quartz scratches glass, while calcite does not. 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