Rock Identifier
Mixed beach pebbles; likely quartzite, granite, and iron-stained metamorphic rock (Predominantly quartzite (SiO₂), granite (quartz–feldspar–mica), and weathered iron-rich rock) — metamorphic and igneous rocks
metamorphic and igneous rocks

Mixed beach pebbles; likely quartzite, granite, and iron-stained metamorphic rock

Predominantly quartzite (SiO₂), granite (quartz–feldspar–mica), and weathered iron-rich rock

AI-generated identification · may be incorrect

Rounded, water-worn pebbles with earthy brown, gray, cream, and speckled colors; surfaces are mostly dull to glassy. Quartzite is about Mohs 7 with no cleavage; granite is about Mohs 6–7 and has interlocking crystals, while iron oxides create rusty coloration.

Identified More metamorphic and igneous rocks
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Physical properties

Rounded, water-worn pebbles with earthy brown, gray, cream, and speckled colors; surfaces are mostly dull to glassy. Quartzite is about Mohs 7 with no cleavage; granite is about Mohs 6–7 and has interlocking crystals, while iron oxides create rusty coloration.

Formation & geological history

These are natural sedimentary deposits of older rocks transported and rounded by waves or rivers; the source rocks formed millions to billions of years ago, depending on locality. The image does not provide enough detail for a precise age or species-level identification.

Uses & applications

Commonly used as decorative landscaping stone, aquarium or craft material, and teaching specimens; attractive pieces may be collected but are generally low-value.

Geological facts

The brown pebble likely contains quartz with iron-oxide staining, while the pale speckled pebble resembles granite or granitic gneiss. Rounding and smoothness indicate prolonged abrasion in water or surf.

Field identification & locations

Test suspected quartzite with a steel file or knife: it should resist scratching; granite shows visible quartz, feldspar, and dark mica grains. Exact identification requires a close view, streak, hardness, and locality information.