Rock Identifier
Rounded granite pebble (Granite, chiefly quartz, potassium feldspar, plagioclase, and mica/amphibole) — igneous
igneous

Rounded granite pebble

Granite, chiefly quartz, potassium feldspar, plagioclase, and mica/amphibole

AI-generated identification · may be incorrect

Coarse-grained, speckled gray-green surface with a granular texture and weak vitreous luster; typical hardness is about 6–7 Mohs, with no obvious cleavage as a whole rock and specific gravity around 2.6–2.7.

Identified More igneous
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Physical properties

Coarse-grained, speckled gray-green surface with a granular texture and weak vitreous luster; typical hardness is about 6–7 Mohs, with no obvious cleavage as a whole rock and specific gravity around 2.6–2.7.

Formation & geological history

An intrusive igneous rock crystallized slowly from silica-rich magma deep in Earth’s crust, generally during Precambrian to Phanerozoic plutonic events. Its rounded shape and smoothed surface result from transport and abrasion on a beach or in a gravel deposit.

Uses & applications

Used extensively as building stone, countertops, monuments, paving, aggregate, and decorative landscaping material; this small waterworn piece is mainly a beach or collection specimen.

Geological facts

Individual mineral grains are visible because slow cooling allowed large crystals to form. A fresh surface commonly reacts weakly or not at all with dilute hydrochloric acid, unlike limestone.

Field identification & locations

Identify it by interlocking visible grains of light quartz/feldspar and darker minerals, lack of layering, and a very hard, abrasion-resistant surface; a streak or fresh fracture helps confirm it. Common worldwide in continental crust and glacial, river, and coastal gravels.