Rock Identifier
Uncertain coarse-grained igneous fragment (Likely granite or granitic pegmatite; quartz–feldspar–mica assemblage) — igneous
igneous

Uncertain coarse-grained igneous fragment

Likely granite or granitic pegmatite; quartz–feldspar–mica assemblage

AI-generated identification · may be incorrect

Light gray to pink, granular texture with dark mica-like specks; likely Mohs 6–7, vitreous to dull luster, massive structure, and no obvious cleavage at this scale. The image is insufficient for reliable mineral identification.

Identified More igneous
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Physical properties

Light gray to pink, granular texture with dark mica-like specks; likely Mohs 6–7, vitreous to dull luster, massive structure, and no obvious cleavage at this scale. The image is insufficient for reliable mineral identification.

Formation & geological history

Probably crystallized slowly from silica-rich magma deep in the crust, generally during Precambrian to Phanerozoic intrusive events; the fragment may have weathered from a larger plutonic body.

Uses & applications

Granite is widely used as crushed stone, aggregate, building stone, countertops, and monuments. This small fragment has negligible commercial or jewelry value.

Geological facts

Pink areas commonly represent potassium feldspar, gray translucent grains quartz, and black flakes biotite or amphibole. A fresh broken surface and hand lens would improve identification.

Field identification & locations

Common in continental crust and found worldwide, especially in mountain belts and exposed plutons. Confirm with visible interlocking quartz/feldspar grains, a streak test, and hardness testing; the apparent specimen may also be a piece of concrete or paving material.