Rock Identifier
Weathered granite (probable) (Granite; chiefly quartz, potassium feldspar, plagioclase, and biotite/hornblende) — igneous
igneous

Weathered granite (probable)

Granite; chiefly quartz, potassium feldspar, plagioclase, and biotite/hornblende

AI-generated identification · may be incorrect

A coarse-grained, tan-gray intrusive rock with speckled crystalline texture and dull weathered surfaces; typical hardness is about 6–7 Mohs, with no prominent cleavage as a whole and density around 2.6–2.7 g/cm³.

Identified More igneous
Explore Weathered granite (probable) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

A coarse-grained, tan-gray intrusive rock with speckled crystalline texture and dull weathered surfaces; typical hardness is about 6–7 Mohs, with no prominent cleavage as a whole and density around 2.6–2.7 g/cm³.

Formation & geological history

Formed when silica-rich magma cooled slowly deep underground, allowing visible crystals to grow; most granite formed during Precambrian to Phanerozoic plutonic events and was later exposed by uplift and erosion.

Uses & applications

Used extensively as dimension stone, countertops, monuments, building stone, and crushed aggregate; ordinary hand specimens have minimal commercial value.

Geological facts

The photograph is somewhat out of focus, so closely related rocks such as weathered granodiorite or quartz monzonite cannot be ruled out.

Field identification & locations

Look for interlocking visible grains: glassy gray quartz, pink/tan feldspar, and black mica or amphibole. Common worldwide in continental mountain belts, including the Sierra Nevada, New England, Scotland, and parts of India and Australia.