
mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale), Color: White to translucent gray, Luster: Vitreous to greasy, Crystal Structure: Hexagonal (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: White to translucent gray, Luster: Vitreous to greasy, Crystal Structure: Hexagonal (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Forms in hydrothermal veins, pegmatites, and as a primary constituent in igneous rocks like granite. It crystallizes from silica-rich fluids deep within the Earth's crust across all geological ages.
Uses & applications
Used in glass manufacturing, electronics (piezoelectric properties), abrasives, construction aggregates, and as decorative gravel or low-cost gemstones in jewelry.
Geological facts
Milky quartz gets its cloudy appearance from microscopic inclusions of gas or liquid trapped during crystal growth. It is one of the most abundant minerals on the Earth's surface.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), various shades of white, and lack of cleavage. It is commonly found in riverbeds, mountain ranges, and quartz veins within host rocks.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral