
mineral
Weathered quartz-rich pebble
Microcrystalline quartz (SiO₂), possibly chert or chalcedony
AI-generated identification · may be incorrectPale yellow-tan, fine-grained and opaque to slightly translucent, with a dull/waxy luster and rounded weathering. Quartz hardness is about 7 Mohs; no visible cleavage, conchoidal fracture, and specific gravity near 2.65.
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Physical properties
Pale yellow-tan, fine-grained and opaque to slightly translucent, with a dull/waxy luster and rounded weathering. Quartz hardness is about 7 Mohs; no visible cleavage, conchoidal fracture, and specific gravity near 2.65.
Formation & geological history
Likely a naturally weathered silica-rich fragment, formed from microcrystalline quartz during sedimentary silicification or volcanic hydrothermal activity; its exact geological age cannot be determined from the photograph.
Uses & applications
Common material for decorative pebbles, lapidary carving, tumbling, and occasional low-grade gemstone use; not suitable for major construction identification from this specimen alone.
Geological facts
The yellow coloration may result from iron-oxide staining or finely distributed impurities. A steel file should not scratch quartz, while quartz can scratch ordinary glass.
Field identification & locations
Common in gravel beds and weathered outcrops worldwide, especially regions containing chert, agate, or quartz veins. Confirm with a hardness test, streak test, and inspection for waxy texture or conchoidal fractures.
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