Rock Identifier
Likely weathered granite or granitic pebble (Granite, chiefly quartz, feldspar, and mica) — igneous
igneous

Likely weathered granite or granitic pebble

Granite, chiefly quartz, feldspar, and mica

AI-generated identification · may be incorrect

Gray, granular, and weakly speckled with a dull to slightly vitreous luster; typical granite hardness is about 6–7 Mohs, with no obvious cleavage as a whole and specific gravity around 2.63–2.75. The image is insufficient for precise mineral identification.

Identified More igneous
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Physical properties

Gray, granular, and weakly speckled with a dull to slightly vitreous luster; typical granite hardness is about 6–7 Mohs, with no obvious cleavage as a whole and specific gravity around 2.63–2.75. The image is insufficient for precise mineral identification.

Formation & geological history

Granite crystallizes slowly from silica-rich magma deep in the crust, commonly during Precambrian to Phanerozoic mountain-building events; this rounded specimen was likely later transported and weathered by water or ice.

Uses & applications

Used extensively as dimension stone, countertops, monuments, aggregate, and landscaping rock; small rounded pieces are common decorative or collection specimens.

Geological facts

The visible dark and light grains suggest interlocking quartz, feldspar, and mafic minerals, but the surface could also represent another light-colored igneous rock such as diorite or gneiss.

Field identification & locations

Identify it by coarse interlocking grains, quartz-like translucent grains, and feldspar-rich pink or white areas; common in stream gravels, glacial deposits, and eroded uplands worldwide. A close-up and scratch or acid tests would improve confidence.