Rock Identifier
Weathered granite cobble (Granite, typically quartz–feldspar–mica assemblage) — igneous
igneous

Weathered granite cobble

Granite, typically quartz–feldspar–mica assemblage

AI-generated identification · may be incorrect

Coarse, speckled texture with pale feldspar/quartz and dark biotite or hornblende; Mohs hardness about 6–7, vitreous to dull luster, massive structure, and no cleavage as a whole rock. The brown-orange surface is likely iron-oxide weathering.

Identified More igneous
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Physical properties

Coarse, speckled texture with pale feldspar/quartz and dark biotite or hornblende; Mohs hardness about 6–7, vitreous to dull luster, massive structure, and no cleavage as a whole rock. The brown-orange surface is likely iron-oxide weathering.

Formation & geological history

Intrusive igneous rock crystallized slowly from silica-rich magma deep in the crust, commonly during Precambrian to Phanerozoic mountain-building events; later erosion and weathering rounded it into a cobble.

Uses & applications

Used as crushed aggregate, building stone, paving, monuments, and landscaping rock; attractive polished pieces may be used decoratively but this specimen has limited gemstone value.

Geological facts

Granite’s visible crystals indicate slow underground cooling. Its rounded shape and weathered rind suggest transport by a river, beach, or glacial system.

Field identification & locations

Identify by interlocking visible quartz and feldspar grains, dark mica/hornblende, high hardness, and lack of layering or vesicles; common worldwide in continental mountain belts and granite terrains.