Rock Identifier
Likely feldspar-rich granite or pegmatite fragment (Granite/pegmatite; chiefly quartz and feldspar, possibly mica) — igneous
igneous

Likely feldspar-rich granite or pegmatite fragment

Granite/pegmatite; chiefly quartz and feldspar, possibly mica

AI-generated identification · may be incorrect

Brown, coarse and irregularly crystalline with a dull-to-glassy luster. Typical hardness is about 6–7 Mohs; exact mineral proportions and cleavage cannot be determined from the photo.

Identified More igneous →
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Physical properties

Brown, coarse and irregularly crystalline with a dull-to-glassy luster. Typical hardness is about 6–7 Mohs; exact mineral proportions and cleavage cannot be determined from the photo.

Formation & geological history

Likely crystallized slowly from silica-rich magma, allowing visible grains to grow. Such rocks commonly formed in continental crust over a wide range of geological ages.

Uses & applications

Granite is used as building and paving stone, countertops, aggregate, and decorative material; small fragments are mainly collected or studied as specimens.

Geological facts

The image does not show enough detail for a reliable identification; several coarse-grained rocks can look similar when weathered.

Field identification & locations

Look for interlocking grains and distinguishable quartz, feldspar, and mica; a fresh surface and closer view would improve identification. Granite and pegmatite occur widely in continental regions.