
mineral
Quartz Vein in Sedimentary Matrix
Silicon Dioxide (SiO2) with host rock
Hardness 7 on Mohs scale (quartz) vs 3-4 (matrix), milky white to tan color, vitreous to dull luster, hexagonal crystal system in quartz, no cleavage, conchoidal fracture
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Physical properties
Hardness 7 on Mohs scale (quartz) vs 3-4 (matrix), milky white to tan color, vitreous to dull luster, hexagonal crystal system in quartz, no cleavage, conchoidal fracture
Formation & geological history
Formed through hydrothermal processes where silica-rich hot fluids are injected into fractures of existing sedimentary or metamorphic rocks, cooling to form crystalline quartz. This sample shows layers suggesting distinct depositional events.
Uses & applications
Quartz is used extensively in glassmaking, electronics (piezoelectric properties), abrasives, and as a gemstone. This specific rough specimen is primarily used as a decorative collector's piece or geological study sample.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Vein quartz often acts as a 'host' for precious metals like gold, which can be deposited by the same hydrothermal fluids.
Field identification & locations
Can be identified in the field by its ability to scratch glass and its resistance to weathering compared to the surrounding rock. Common in mountain belts and areas with past tectonic activity. Collectors look for the sharp contact line between the white mineral and the tan host rock.
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