
mineral
Raw smoky quartz (likely iron-stained quartz)
Quartz, SiO₂; brown coloration may reflect irradiation-related smoky quartz and iron-oxide inclusions
AI-generated identification · may be incorrectTranslucent dark brown to smoky gray, vitreous luster, conchoidal fracture, no obvious cleavage, Mohs hardness 7, trigonal crystal structure, specific gravity about 2.65. The irregular shape suggests a naturally fractured or partially worked fragment.
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Physical properties
Translucent dark brown to smoky gray, vitreous luster, conchoidal fracture, no obvious cleavage, Mohs hardness 7, trigonal crystal structure, specific gravity about 2.65. The irregular shape suggests a naturally fractured or partially worked fragment.
Formation & geological history
Quartz crystallizes from silica-rich hydrothermal fluids, pegmatites, and cavities in igneous or metamorphic rocks; smoky coloration commonly develops from natural radiation acting on aluminum impurities. Exact geological age and locality cannot be determined from the image.
Uses & applications
Used as a decorative and lapidary material, gemstone, ornamental carving stone, and mineral specimen; quartz is also important industrially in glass, electronics, and abrasives.
Geological facts
Quartz commonly shows conchoidal fracture and can scratch ordinary glass. The brown appearance may also indicate quartz-rich chalcedony or iron-stained material rather than true smoky quartz.
Field identification & locations
Look for glassy luster, hardness near 7, translucent edges, and conchoidal fracture; a steel knife should not scratch it. Common worldwide, especially in Brazil, Madagascar, the Alps, the United States, and hydrothermal veins.
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