
mineral
Iron-stained quartz (likely quartz-rich rock)
Quartz, SiO₂, with iron-oxide staining; exact specimen uncertain from the image
AI-generated identification · may be incorrectOpaque to translucent tan-brown, rough and irregular, with a dull to vitreous luster. Quartz hardness is 7 Mohs; its crystals are trigonal and it has no cleavage, breaking with uneven to conchoidal fracture.
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Physical properties
Opaque to translucent tan-brown, rough and irregular, with a dull to vitreous luster. Quartz hardness is 7 Mohs; its crystals are trigonal and it has no cleavage, breaking with uneven to conchoidal fracture.
Formation & geological history
Likely silica-rich material stained by iron oxides during weathering or groundwater flow. The specimen’s geological age and precise formation setting cannot be determined visually.
Uses & applications
Quartz is widely used in glass, electronics, abrasives, and jewelry; this rough piece is mainly suitable for collecting or lapidary evaluation.
Geological facts
Brown and ochre colors commonly come from hematite or goethite coatings or inclusions rather than the quartz itself.
Field identification & locations
Quartz is common worldwide; look for hardness greater than glass, lack of cleavage, and a glassy fresh fracture. The photo does not establish a specific locality or confirm that the piece is solid quartz.
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