Rock Identifier
Tumbled orange-brown feldspathic rock, likely granite or weathered syenite (Feldspar-rich granitoid; chiefly K-feldspar and plagioclase with minor quartz and dark biotite/amphibole) — igneous
igneous

Tumbled orange-brown feldspathic rock, likely granite or weathered syenite

Feldspar-rich granitoid; chiefly K-feldspar and plagioclase with minor quartz and dark biotite/amphibole

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; orange-tan, mottled, opaque, with a dull to waxy polished luster. Interlocking crystalline texture is partly obscured by tumbling; no obvious cleavage is visible at this scale.

Identified More igneous
Explore Tumbled orange-brown feldspathic rock, likely granite or weathered syenite in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness about 6–7 Mohs; orange-tan, mottled, opaque, with a dull to waxy polished luster. Interlocking crystalline texture is partly obscured by tumbling; no obvious cleavage is visible at this scale.

Formation & geological history

An intrusive igneous rock that crystallized slowly from magma deep underground, commonly during Precambrian to Phanerozoic continental crust formation. The orange color likely reflects iron staining or alteration of feldspar.

Uses & applications

Used as decorative stone, landscaping aggregate, countertops, and inexpensive tumbled-stone material; generally little gem value.

Geological facts

The specimen’s rounded shape and glossy surface are mechanically tumbled, not naturally weathered. Dark flecks may be biotite or amphibole, while the orange matrix strongly suggests iron-stained feldspar.

Field identification & locations

Identify by its coarse crystalline appearance, feldspar-rich orange color, hardness, and lack of layering or vesicles; a steel file should barely scratch it. Common in continental shield regions and granite gravel deposits.