Rock Identifier
Polished pink-and-gray stone, possibly granite or rhyolite (Probable felsic igneous rock; likely quartz–feldspar–mica aggregate, but exact identification is uncertain from the image) — igneous
igneous

Polished pink-and-gray stone, possibly granite or rhyolite

Probable felsic igneous rock; likely quartz–feldspar–mica aggregate, but exact identification is uncertain from the image

AI-generated identification · may be incorrect

Small rounded, polished pebble with pink/orange and dark gray-black patches; likely Mohs hardness 6–7, granular texture, and dull to slightly vitreous luster. No clear crystal faces or cleavage are visible.

Identified More igneous
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Physical properties

Small rounded, polished pebble with pink/orange and dark gray-black patches; likely Mohs hardness 6–7, granular texture, and dull to slightly vitreous luster. No clear crystal faces or cleavage are visible.

Formation & geological history

Likely formed by cooling of silica-rich magma, producing interlocking quartz and feldspar crystals; age depends on source locality and may range from Precambrian to recent geological periods. Polishing and rounding are human- or water-produced.

Uses & applications

Used as a decorative tumbled stone, craft material, or inexpensive collectible; comparable granite and rhyolite are also used for aggregate, countertops, monuments, and landscaping.

Geological facts

The pink coloration commonly reflects potassium feldspar, while dark areas may be biotite, amphibole, or iron-oxide staining. A photograph cannot reliably distinguish granite from rhyolite, jasper, or another mixed silicate pebble.

Field identification & locations

Test hardness against glass, inspect grain size with magnification, and use a streak test, though a fresh surface or laboratory analysis may be needed. Commonly found in glacial deposits, stream gravels, landscaping stones, and lapidary collections.