
mineral
Milky quartz (likely quartzite or massive quartz)
Quartz, SiO₂
AI-generated identification · may be incorrectWhite to translucent, vitreous-to-waxy luster, massive texture, and no obvious cleavage; Mohs hardness 7, specific gravity about 2.65. The cloudy appearance is caused by microscopic fluid inclusions or fractures; the image does not show diagnostic crystal faces.
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Physical properties
White to translucent, vitreous-to-waxy luster, massive texture, and no obvious cleavage; Mohs hardness 7, specific gravity about 2.65. The cloudy appearance is caused by microscopic fluid inclusions or fractures; the image does not show diagnostic crystal faces.
Formation & geological history
Quartz forms in hydrothermal veins, pegmatites, and metamorphic rocks; quartzite forms when sandstone recrystallizes. Its exact geological age and whether it is quartz or quartzite cannot be determined from the photograph.
Uses & applications
Used as a silica source for glass, ceramics, and silicon production; quartzite is used for aggregate, paving, and countertops. Attractive translucent pieces have modest lapidary and collecting appeal.
Geological facts
Quartz is one of Earth’s most abundant minerals and is piezoelectric. Milky quartz commonly develops rounded, irregular masses rather than well-formed crystals.
Field identification & locations
A glassy surface, hardness sufficient to scratch ordinary glass, and lack of cleavage support quartz; quartzite usually shows a granular, fused sandstone texture. Common worldwide, especially in hydrothermal veins and metamorphic belts.
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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