
mineral
Weathered quartz-bearing rock fragment
Indeterminate; likely quartz-rich granite or silicified host rock with iron-oxide staining
AI-generated identification · may be incorrectTan-brown, irregular, granular specimen with pale translucent grains and rusty surface coating; likely hardness about 6–7 Mohs, vitreous to dull luster, no obvious cleavage, and moderate specific gravity around 2.6–2.8.
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Physical properties
Tan-brown, irregular, granular specimen with pale translucent grains and rusty surface coating; likely hardness about 6–7 Mohs, vitreous to dull luster, no obvious cleavage, and moderate specific gravity around 2.6–2.8.
Formation & geological history
Probably a naturally weathered fragment of quartz-rich igneous or hydrothermal rock; its exact geological age and formation environment cannot be determined from the photograph.
Uses & applications
Primarily a casual geological specimen or teaching sample; no significant industrial or jewelry use is apparent at this size and quality.
Geological facts
The rusty coloration commonly results from oxidation of iron-bearing minerals into limonite or goethite. A glassy grain that scratches ordinary glass would support quartz identification.
Field identification & locations
Commonly encountered in weathered outcrops, gravel, and stream deposits worldwide; inspect a fresh broken surface and test hardness, streak, magnetism, and acid reaction for better identification.
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