
mineral
Milky quartz
Quartz (silicon dioxide, SiO₂)
AI-generated identification · may be incorrectWhite to translucent, vitreous-to-waxy luster with irregular fracture and no obvious cleavage; Mohs hardness 7, trigonal crystal structure, and specific gravity about 2.65. The cloudy appearance comes from microscopic fluid inclusions or defects.
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Physical properties
White to translucent, vitreous-to-waxy luster with irregular fracture and no obvious cleavage; Mohs hardness 7, trigonal crystal structure, and specific gravity about 2.65. The cloudy appearance comes from microscopic fluid inclusions or defects.
Formation & geological history
Forms in hydrothermal veins, pegmatites, and cavities in igneous and metamorphic rocks; quartz is common from Precambrian terrains through the present. The pictured piece may also be a weathered vein fragment.
Uses & applications
Used for glass, ceramics, foundry materials, abrasives, engineered stone, and electronics; attractive pieces are sold as inexpensive display or lapidary specimens.
Geological facts
Quartz is one of Earth’s most abundant minerals and is piezoelectric. Milky quartz commonly occurs with feldspar, mica, metallic sulfides, or other vein minerals.
Field identification & locations
Identify by its hardness, glassy appearance, lack of cleavage, and inability to scratch it with a steel knife while it can scratch ordinary glass; common worldwide, especially in quartz veins and granitic pegmatites.
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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