Rock Identifier
Weathered granite or granitic gneiss (Quartz–feldspar–mica aggregate; possibly foliated granitic gneiss) — igneous
igneous

Weathered granite or granitic gneiss

Quartz–feldspar–mica aggregate; possibly foliated granitic gneiss

AI-generated identification · may be incorrect

Coarse-grained, speckled gray, pink-orange, and black material with a dull to slightly granular luster; likely Mohs hardness 6–7. Quartz and feldspar are interlocked, with dark biotite or amphibole; no obvious cleavage as a whole rock.

Identified More igneous
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Physical properties

Coarse-grained, speckled gray, pink-orange, and black material with a dull to slightly granular luster; likely Mohs hardness 6–7. Quartz and feldspar are interlocked, with dark biotite or amphibole; no obvious cleavage as a whole rock.

Formation & geological history

Likely crystallized slowly from silica-rich magma deep in the crust, then exposed by uplift and erosion; if the dark minerals show layering, it may have undergone later high-grade metamorphism as gneiss. Exact age and locality cannot be determined from the image.

Uses & applications

Granite and gneiss are widely used as crushed aggregate, roadstone, dimension stone, countertops, monuments, and landscaping rock; this weathered fragment has little gem value.

Geological facts

The orange coloration is probably iron-oxide staining or weathered potassium feldspar rather than a separate gemstone. The specimen appears natural and unpolished, with visible weathering and possible feldspar alteration.

Field identification & locations

Common in continental crust and glaciated or mountainous regions worldwide. Identify it by coarse interlocking grains, abundant pale quartz/feldspar, and scattered black mica or amphibole; a streak, acid, and fresh-break test would improve confidence.