Rock Identifier
Tumbled feldspar-rich rock, possibly granite or gneiss (Indeterminate feldspar–quartz rock; exact identification requires testing) — igneous
igneous

Tumbled feldspar-rich rock, possibly granite or gneiss

Indeterminate feldspar–quartz rock; exact identification requires testing

AI-generated identification · may be incorrect

Smooth, rounded, translucent gray-green body with pale cream patches and a subdued vitreous-to-waxy luster. Visible grains suggest quartz and feldspar; hardness likely around 6–7 Mohs if quartz-bearing, but cannot be confirmed from the image.

Identified More igneous →
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Physical properties

Smooth, rounded, translucent gray-green body with pale cream patches and a subdued vitreous-to-waxy luster. Visible grains suggest quartz and feldspar; hardness likely around 6–7 Mohs if quartz-bearing, but cannot be confirmed from the image.

Formation & geological history

Likely a naturally weathered pebble that has been tumbled or polished. If granite, it crystallized from slowly cooled magma; if gneiss, it was recrystallized under metamorphic heat and pressure; age is unknown.

Uses & applications

Small polished specimens are used for collecting, crafts, and decorative displays; comparable unpolished rock may be used as aggregate or building stone.

Geological facts

The image does not show enough diagnostic detail to distinguish granite, gneiss, or another feldspar-rich stone reliably.

Field identification & locations

Look for interlocking grains, quartz hardness (scratches glass), and any mineral banding; a fresh surface or simple hardness test would improve identification. Such pebbles occur widely in glacial and river deposits.