
metamorphic
Yellow-brown quartz-rich pebble (possibly iron-stained chert or quartzite)
Quartz (SiO₂), likely with iron-oxide staining; exact identification requires hardness and acid tests
AI-generated identification · may be incorrectMassive, fine-grained, dull to slightly vitreous surface; yellow-brown coloration is likely from limonite/goethite. Quartz hardness is 7, with no cleavage and conchoidal to uneven fracture; specific gravity about 2.65.
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Physical properties
Massive, fine-grained, dull to slightly vitreous surface; yellow-brown coloration is likely from limonite/goethite. Quartz hardness is 7, with no cleavage and conchoidal to uneven fracture; specific gravity about 2.65.
Formation & geological history
Probably a naturally weathered silica-rich pebble formed from sedimentary chert or metamorphosed quartz sandstone, later stained by oxidized iron. Precise age and formation environment cannot be determined from the photograph.
Uses & applications
Suitable mainly as a curiosity, lapidary rough, or polished stone; iron-stained quartz-rich material has limited commercial value and is not typically used structurally.
Geological facts
The specimen may scratch ordinary glass if predominantly quartz. A streak test, magnification, and examination of grain texture would help distinguish chert from quartzite.
Field identification & locations
Common in stream gravels and weathered outcrops worldwide. Test whether it scratches glass, inspect for visible interlocking grains, and apply dilute hydrochloric acid only if carbonate minerals are suspected.
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