Rock Identifier
Weathered granite or granodiorite fragment (Granite–granodiorite, chiefly quartz, feldspar, and dark biotite/amphibole) — igneous
igneous

Weathered granite or granodiorite fragment

Granite–granodiorite, chiefly quartz, feldspar, and dark biotite/amphibole

AI-generated identification · may be incorrect

Coarse-grained, speckled gray-beige rock with a dull to slightly granular luster; likely Mohs hardness 6–7, massive texture, and no obvious cleavage as a whole (individual feldspars may cleave). Exact mineral proportions cannot be confirmed from the image alone.

Identified More igneous
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Physical properties

Coarse-grained, speckled gray-beige rock with a dull to slightly granular luster; likely Mohs hardness 6–7, massive texture, and no obvious cleavage as a whole (individual feldspars may cleave). Exact mineral proportions cannot be confirmed from the image alone.

Formation & geological history

An intrusive igneous rock crystallized slowly from silica-rich magma deep in the crust, commonly during Precambrian to Mesozoic mountain-building events; the rounded shape and surface suggest stream or beach abrasion and weathering.

Uses & applications

Used widely as crushed aggregate, building stone, paving, monuments, and countertops; this small weathered piece has little commercial value but may be a useful teaching or collecting specimen.

Geological facts

Granite is defined by abundant quartz and alkali feldspar, whereas granodiorite contains more plagioclase; hand specimens can be difficult to distinguish without mineral identification or a thin section.

Field identification & locations

Look for interlocking visible crystals, glassy gray quartz, pink/white feldspar, and black biotite or amphibole. Common worldwide, especially in exposed mountain batholiths; a fresh broken surface and hand lens improve identification.