
mineral
Quartz with Metallic Inclusion
Silicon Dioxide (SiO2) with associated metallic sulfide or oxide
Hardness: 7 (Quartz body), White to off-white body with metallic grey/black inclusion, Vitreous to dull luster, Trigonal/Hexagonal crystal system, Conchoidal fracture, Specific gravity ~2.65 for the quartz.
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Physical properties
Hardness: 7 (Quartz body), White to off-white body with metallic grey/black inclusion, Vitreous to dull luster, Trigonal/Hexagonal crystal system, Conchoidal fracture, Specific gravity ~2.65 for the quartz.
Formation & geological history
Quartz forms in a wide variety of environments, most commonly from hydrothermal veins and cooling igneous magmas. The inclusion likely formed during the late-stage cooling of mineral-rich fluids.
Uses & applications
This specimen is primarily a decorative or geological sample. Pure quartz is used in glassmaking, electronics, and construction.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Inclusions like the metallic one seen here can sometimes contain trace amounts of galena, pyrite, or iron oxides which provide clues to the mineral deposit origin.
Field identification & locations
Identify by its ability to scratch glass and the lack of cleavage in the white quartz portion. Look for it in areas with high tectonic activity or near historic mining sites.
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