Rock Identifier
Orange feldspar pebble (likely potassium feldspar) (K-feldspar, chiefly orthoclase or microcline (KAlSi₃O₈), in a granitic rock fragment) — igneous
igneous

Orange feldspar pebble (likely potassium feldspar)

K-feldspar, chiefly orthoclase or microcline (KAlSi₃O₈), in a granitic rock fragment

AI-generated identification · may be incorrect

Opaque, mottled salmon-orange and brown with a dull to slightly vitreous luster; feldspar hardness is about 6 Mohs, with two near-right-angle cleavage directions. The small, rounded specimen’s grain boundaries and exact composition are not clear from the image.

Identified More igneous →
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Physical properties

Opaque, mottled salmon-orange and brown with a dull to slightly vitreous luster; feldspar hardness is about 6 Mohs, with two near-right-angle cleavage directions. The small, rounded specimen’s grain boundaries and exact composition are not clear from the image.

Formation & geological history

Likely weathered from feldspar-rich granite or pegmatite and rounded by transport in water or sediment. Its source rock may have formed during ancient magma cooling; the pebble’s age cannot be determined from appearance alone.

Uses & applications

Feldspar is used in ceramics and glass; attractive pieces may be collected or used in simple jewelry, though this specimen appears chiefly of interest as a field find.

Geological facts

Orange color commonly results from iron staining or inclusions rather than being diagnostic of a particular feldspar variety.

Field identification & locations

Look for salmon-pink color, blocky cleavage, and hardness near 6; feldspar-bearing pebbles occur in river and beach gravels worldwide. A scratch test and fresh fracture would help distinguish it from quartz or other orange stones.