Rock Identifier
Weathered granite (Granite; interlocking quartz, feldspar, and mica minerals) — igneous
igneous

Weathered granite

Granite; interlocking quartz, feldspar, and mica minerals

AI-generated identification · may be incorrect

Coarse-grained, pinkish tan rock with visible light feldspar/quartz and dark biotite or hornblende; vitreous quartz and feldspar luster, Mohs hardness about 6–7, no strong cleavage as a rock, and specific gravity around 2.6–2.7.

Identified More igneous
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Physical properties

Coarse-grained, pinkish tan rock with visible light feldspar/quartz and dark biotite or hornblende; vitreous quartz and feldspar luster, Mohs hardness about 6–7, no strong cleavage as a rock, and specific gravity around 2.6–2.7.

Formation & geological history

An intrusive igneous rock formed when silica-rich magma cooled slowly deep underground, commonly during Precambrian to younger continental-crust events. The surface appears weathered and iron-stained.

Uses & applications

Widely used as dimension stone, countertops, monuments, paving, aggregate, and building stone; ordinary hand specimens usually have little commercial value.

Geological facts

The pink color commonly comes from potassium feldspar, while dark flecks are mafic minerals. Its coarse texture records slow underground cooling.

Field identification & locations

Identify it by its visible interlocking crystals, pink/white/gray color, and hardness; it should scratch glass and resist a steel knife. Common worldwide in continental mountain ranges and shield regions.