
mineral
Weathered quartz-rich rock fragment
Likely milky quartz–bearing quartzite or silica-rich chert; exact identification requires testing
AI-generated identification · may be incorrectTan-brown, opaque to weakly translucent, with a dull to slightly vitreous luster and irregular fracture; apparent hardness about 6–7 Mohs, but grain size and cleavage are not resolvable from the image.
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Physical properties
Tan-brown, opaque to weakly translucent, with a dull to slightly vitreous luster and irregular fracture; apparent hardness about 6–7 Mohs, but grain size and cleavage are not resolvable from the image.
Formation & geological history
Probably a natural siliceous fragment formed by cementation or metamorphism of quartz-rich sediment, later weathered and iron-stained; its geological age cannot be determined visually.
Uses & applications
Common material has little commercial value; quartzite may be used as aggregate, building stone, or decorative material, while attractive pieces can be collected.
Geological facts
The brown coloration is consistent with iron-oxide staining along fractures or grain boundaries. A glassy edge and lack of obvious cleavage favor quartz over feldspar or mica.
Field identification & locations
Look for abundant quartz grains, no cleavage, and the ability to scratch ordinary glass; quartzite typically shows fused grains, whereas chert is smoother and microcrystalline. Common worldwide, especially in quartz-rich sedimentary and metamorphic terrains.
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