
mineral
Milky quartz
Quartz, silicon dioxide (SiO₂)
AI-generated identification · may be incorrectHardness 7; white to translucent, vitreous-to-pearly luster, commonly massive with irregular fracture and no cleavage. The specimen appears to be coarse, sugary milky quartz, possibly with minor feldspar or calcite inclusions.
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Physical properties
Hardness 7; white to translucent, vitreous-to-pearly luster, commonly massive with irregular fracture and no cleavage. The specimen appears to be coarse, sugary milky quartz, possibly with minor feldspar or calcite inclusions.
Formation & geological history
Forms when silica-rich hydrothermal fluids or late-stage igneous fluids crystallize in veins and cavities, commonly during Precambrian to younger mountain-building events. Quartz veins occur in many rock types worldwide.
Uses & applications
Used for glass, ceramics, abrasives, engineered stone, and silicon production; attractive pieces are sold as cabinet specimens, though this rough material has limited gemstone value.
Geological facts
Its milky appearance results from microscopic fluid inclusions, fractures, and impurities scattering light. Quartz is one of Earth’s most abundant and chemically durable minerals.
Field identification & locations
Identify by its glassy translucence, hardness sufficient to scratch ordinary glass, lack of cleavage, and six-sided crystals when developed. Common localities include Brazil, Madagascar, the United States, China, and the Alps.
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Sandstone (with potential mineral staining/concretions)
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Calcite–fluorite mineral specimen with iron-oxide staining
Calcite (CaCO₃), likely fluorite (CaF₂), with possible quartz and iron/manganese oxides
mineral
Septarian Pebble
Septarian nodule / Concretion
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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