
mineral
Smoky quartz crystal (probable)
Quartz, silicon dioxide (SiO₂), likely iron-colored smoky quartz
AI-generated identification · may be incorrectTranslucent gray-brown fragment with a vitreous luster and conchoidal-looking fracture; quartz hardness is 7 Mohs, lacks cleavage, and has hexagonal crystal structure. The apparent metallic/dark coating may be matrix, iron staining, or surface alteration.
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Physical properties
Translucent gray-brown fragment with a vitreous luster and conchoidal-looking fracture; quartz hardness is 7 Mohs, lacks cleavage, and has hexagonal crystal structure. The apparent metallic/dark coating may be matrix, iron staining, or surface alteration.
Formation & geological history
Forms in silica-rich hydrothermal veins, pegmatites, and cavities in igneous rocks; coloration commonly results from natural irradiation affecting aluminum impurities. The specimen’s exact age and locality cannot be determined from the image.
Uses & applications
Used as a collector mineral and occasionally in jewelry; quartz is also important industrially in glass, electronics, abrasives, and engineered stone.
Geological facts
Smoky quartz ranges from pale champagne to nearly black “morion.” A glass fragment can look similar, but quartz is harder and typically shows natural crystal faces or distinctive conchoidal fracture.
Field identification & locations
Common localities include Brazil, Switzerland, Madagascar, the United States, and Scotland. Confirm with a hardness test, crystal-face inspection, and specific-gravity measurement; avoid scratching valuable specimens.
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