
mineral
Tumbled black-and-white stone, likely dendritic agate or jasper
Cryptocrystalline quartz (SiO₂), possibly chalcedony with manganese-oxide dendrites
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; opaque cream-white with black branching or irregular inclusions and a dull-to-waxy polish. It has no visible cleavage and a fine microcrystalline quartz structure; exact identification is limited by the photograph.
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Physical properties
Hardness about 6.5–7 Mohs; opaque cream-white with black branching or irregular inclusions and a dull-to-waxy polish. It has no visible cleavage and a fine microcrystalline quartz structure; exact identification is limited by the photograph.
Formation & geological history
Silica-rich groundwater filled cavities or fractures in volcanic rock, while manganese or iron oxides produced the dark patterns; formation commonly occurred during the Cenozoic or older volcanic episodes. Tumbled surfaces are human-processed.
Uses & applications
Used primarily as a decorative stone, lapidary material, cabochon, and inexpensive collectible; it has little industrial value in this form.
Geological facts
Dendritic patterns are mineral inclusions, not fossils or plant material. Similar black-and-white tumbled stones may also be Picasso jasper, zebra jasper, or dyed chalcedony.
Field identification & locations
Commonly found as tumbled material from Brazil, Madagascar, India, Mexico, and the western United States. A glassy scratch-resistant surface, waxy luster, and lack of cleavage support chalcedony; a streak, translucency test, and magnification would refine identification.
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