Rock Identifier
Tumbled river pebble, likely weathered basalt (Basalt; fine-grained mafic volcanic rock, commonly containing plagioclase, pyroxene, and iron oxides) — igneous
igneous

Tumbled river pebble, likely weathered basalt

Basalt; fine-grained mafic volcanic rock, commonly containing plagioclase, pyroxene, and iron oxides

AI-generated identification · may be incorrect

Dark brown-gray, rounded and smoothly weathered, with a dull-to-subvitreous luster and faint speckling; hardness about 5–6 Mohs, no visible cleavage, and typical specific gravity around 2.8–3.0. The image alone cannot confirm the exact rock type.

Identified More igneous
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Physical properties

Dark brown-gray, rounded and smoothly weathered, with a dull-to-subvitreous luster and faint speckling; hardness about 5–6 Mohs, no visible cleavage, and typical specific gravity around 2.8–3.0. The image alone cannot confirm the exact rock type.

Formation & geological history

Formed when mafic lava cooled rapidly at or near Earth’s surface, then was rounded by river, beach, or glacial abrasion. Basalt ranges from Precambrian to modern age and occurs in oceanic crust and volcanic provinces.

Uses & applications

Used as aggregate, road stone, riprap, and decorative landscaping material; attractive polished pieces may be used in simple crafts, but this specimen has little gem value.

Geological facts

Its smooth shape records prolonged abrasion and transport. Brown coloration commonly reflects surface weathering and oxidation of iron-bearing minerals.

Field identification & locations

Look for fine grain, high density, dark color, and weak attraction to a magnet if iron-rich; a fresh broken surface should be gray-black. Common worldwide near volcanic rocks and streambeds.