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

Likely granite or granitic gneiss fragment

Quartz–feldspar–mica aggregate; possibly granitic gneiss

AI-generated identification · may be incorrect

Light gray, fine-to-medium granular texture with visible dark mica grains; likely vitreous quartz and feldspar luster, no obvious cleavage at specimen scale. Estimated hardness 6–7 Mohs and specific gravity about 2.6–2.8.

Identified More igneous
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Physical properties

Light gray, fine-to-medium granular texture with visible dark mica grains; likely vitreous quartz and feldspar luster, no obvious cleavage at specimen scale. Estimated hardness 6–7 Mohs and specific gravity about 2.6–2.8.

Formation & geological history

Granite crystallizes slowly from silica-rich magma deep underground; granitic gneiss is a metamorphosed equivalent showing mineral alignment. Such rocks are commonly Precambrian to Phanerozoic in age, depending on locality.

Uses & applications

Used extensively as crushed aggregate, building stone, countertops, monuments, and paving; this small fragment has negligible practical value.

Geological facts

The speckled appearance reflects interlocking quartz, feldspar, and biotite crystals formed during slow cooling or recrystallization.

Field identification & locations

Identify by its hard, grainy, interlocking texture and inability to fizz in dilute acid; granite is common worldwide, while gneiss often shows banding or foliation. A clear identification would require a closer view and locality information.