Rock Identifier
Likely reddish granite/porphyritic igneous rock fragments (Feldspar–quartz–mica aggregate, possibly pink granite or rhyolite) — igneous
igneous

Likely reddish granite/porphyritic igneous rock fragments

Feldspar–quartz–mica aggregate, possibly pink granite or rhyolite

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; pink to reddish-brown, granular, with visible pale feldspar and dark minerals; generally vitreous to dull luster, no obvious cleavage as a whole, and typical specific gravity around 2.6–2.7.

Identified More igneous
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Physical properties

Hardness about 6–7 Mohs; pink to reddish-brown, granular, with visible pale feldspar and dark minerals; generally vitreous to dull luster, no obvious cleavage as a whole, and typical specific gravity around 2.6–2.7.

Formation & geological history

Formed by cooling of silica-rich magma, likely as intrusive granite or, if fine-grained, volcanic rhyolite; exact age and locality cannot be determined from the photograph.

Uses & applications

Granite is widely used as crushed stone, aggregate, building stone, countertops, and decorative material; attractive pieces have modest collecting value.

Geological facts

The blocky pale grains are probably feldspar, while gray or black specks may be quartz, biotite, or amphibole. Surface weathering can intensify the rusty-red color through iron oxidation.

Field identification & locations

Common worldwide, including India, Brazil, Scandinavia, and North America. Confirm with a hand lens, streak test, and hardness test: quartz should scratch glass, while the rock should show interlocking grains rather than sedimentary layering.