
mineral
Tumbled reddish-brown quartz (likely iron-stained quartz)
Quartz, SiO₂; likely colored by iron-oxide inclusions or surface staining
AI-generated identification · may be incorrectMohs hardness 7; translucent to opaque reddish-brown with cloudy white areas and a vitreous luster. Quartz has a trigonal crystal structure and no prominent cleavage; tumbling has rounded its edges. Exact identification is limited by the photo.
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Physical properties
Mohs hardness 7; translucent to opaque reddish-brown with cloudy white areas and a vitreous luster. Quartz has a trigonal crystal structure and no prominent cleavage; tumbling has rounded its edges. Exact identification is limited by the photo.
Formation & geological history
Quartz forms in igneous and hydrothermal settings and in veins; iron oxides can stain or color it. Its age and precise geological source cannot be determined from the image.
Uses & applications
Commonly sold as a polished/tumbled collector stone or used in crafts and inexpensive jewelry; quartz also has major industrial uses in glass and electronics.
Geological facts
Quartz is one of Earth’s most abundant minerals. Iron impurities and coatings can produce a wide range of red, brown, and yellow colors.
Field identification & locations
The rounded, polished surface and cloudy translucence are consistent with tumbled quartz. Quartz occurs worldwide; hardness and lack of cleavage help distinguish it from softer lookalikes.
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