Rock Identifier
Likely pink granite or granitic gneiss pebble (Granite: quartz, potassium feldspar, plagioclase, and minor dark minerals; exact identification is uncertain from the image.) — igneous
igneous

Likely pink granite or granitic gneiss pebble

Granite: quartz, potassium feldspar, plagioclase, and minor dark minerals; exact identification is uncertain from the image.

AI-generated identification · may be incorrect

Rounded, coarse-grained pebble with pink and gray coloring and dark flecks; typical granite is Mohs 6–7, with a granular crystalline texture and no prominent cleavage.

Identified More igneous →
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Physical properties

Rounded, coarse-grained pebble with pink and gray coloring and dark flecks; typical granite is Mohs 6–7, with a granular crystalline texture and no prominent cleavage.

Formation & geological history

Granite forms when silica-rich magma cools slowly underground; some pink, banded material may instead be metamorphosed granite (gneiss). Its age and original source cannot be determined from the photo.

Uses & applications

Granite is widely used as dimension stone, paving, countertops, and aggregate; this small pebble is mainly suitable for collecting or landscaping.

Geological facts

Pink color commonly comes from potassium feldspar, while dark flecks may be biotite or amphibole.

Field identification & locations

Look for interlocking visible mineral grains and a hard, gritty surface; rounded edges suggest transport by water or weathering. Granitic rocks occur worldwide.