Rock Identifier
Weathered granite fragment (Granite, chiefly quartz (SiO₂), feldspar, and mica) — igneous
igneous

Weathered granite fragment

Granite, chiefly quartz (SiO₂), feldspar, and mica

AI-generated identification · may be incorrect

Coarse-grained, mottled pink-gray and brown, with vitreous quartz, feldspar, and dark mica; hardness about 6–7 Mohs, no consistent cleavage as a whole, specific gravity approximately 2.6–2.7.

Identified More igneous
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Physical properties

Coarse-grained, mottled pink-gray and brown, with vitreous quartz, feldspar, and dark mica; hardness about 6–7 Mohs, no consistent cleavage as a whole, specific gravity approximately 2.6–2.7.

Formation & geological history

An intrusive igneous rock formed by slow cooling of silica-rich magma deep in the crust, commonly during Precambrian to Phanerozoic mountain-building events. The rough surface indicates weathering or mechanical breakage.

Uses & applications

Used extensively as dimension stone, countertops, monuments, paving, aggregate, and building material; small unattractive fragments have minimal decorative value.

Geological facts

Visible interlocking grains distinguish granite from glass or many fine-grained rocks. Pink coloration commonly reflects potassium feldspar, while dark flakes are biotite or hornblende.

Field identification & locations

Identify it by its coarse interlocking crystals and speckled appearance; a glassy surface, hardness, and lack of bubbles support a natural rock origin. Common worldwide, especially in continental mountain belts.