
mineral
Iron-stained quartz with possible mica
Quartz (SiO₂), with iron-oxide staining and possible mica or feldspar inclusions
AI-generated identification · may be incorrectSmall rough specimen with translucent gray-white quartz, rusty orange-brown staining, and uneven fracture; quartz is Mohs 7, vitreous, and trigonal. The image is not sufficient to confirm the inclusions or exact mineral identity.
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Physical properties
Small rough specimen with translucent gray-white quartz, rusty orange-brown staining, and uneven fracture; quartz is Mohs 7, vitreous, and trigonal. The image is not sufficient to confirm the inclusions or exact mineral identity.
Formation & geological history
Quartz commonly forms in hydrothermal veins and fractures as silica-rich fluids cool; iron oxides can stain it later. The specimen’s age and precise formation environment cannot be determined from the photo.
Uses & applications
Quartz is widely used in glass, electronics, abrasives, and jewelry; this small, irregular piece is mainly suitable for a collection.
Geological facts
Quartz is one of Earth’s most abundant minerals and has no cleavage, typically breaking with a curved or irregular fracture.
Field identification & locations
Look for glassy luster and hardness sufficient to scratch ordinary glass; rusty color may come from iron oxides. Quartz occurs worldwide in veins and many rock types.
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