Rock Identifier
Mixed river-worn rock collection (Uncertain; likely quartzite, sandstone, basalt, and weathered granite or gneiss) — igneous, sedimentary, metamorphic
igneous, sedimentary, metamorphic

Mixed river-worn rock collection

Uncertain; likely quartzite, sandstone, basalt, and weathered granite or gneiss

AI-generated identification · may be incorrect

Rounded cobbles with gray, tan, pink, blue-gray, and reddish colors; mostly dull to slightly silky luster, massive textures, and no obvious cleavage. Likely hardness ranges from Mohs 5–7, with quartz-rich pieces hardest; exact identification requires tests such as streak, acid reaction, and magnification.

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Physical properties

Rounded cobbles with gray, tan, pink, blue-gray, and reddish colors; mostly dull to slightly silky luster, massive textures, and no obvious cleavage. Likely hardness ranges from Mohs 5–7, with quartz-rich pieces hardest; exact identification requires tests such as streak, acid reaction, and magnification.

Formation & geological history

These are probably glacial or stream-transported cobbles, rounded by abrasion and weathering; their ages depend on source bedrock and may range from millions to billions of years. The pink specimen may be iron-stained sandstone or feldspathic rock, while the dark gray pieces may be basalt or quartzite.

Uses & applications

Commonly used for landscaping, garden decoration, drainage, aquarium décor, craft projects, and educational collections; attractive pieces may be polished or cut.

Geological facts

The visible white patches could be quartz or feldspar, whereas the speckled gray cobbles may contain mafic minerals. Surface color alone is insufficient for reliable species identification.

Field identification & locations

Look for grain size, layering, foliation, visible crystals, and acid fizz; a glass scratch test can distinguish quartz-rich rocks from softer materials. Such rounded cobbles are common in riverbeds, beaches, and glacial deposits worldwide.