Rock Identifier
Weathered basalt pebble (Basalt, a fine-grained mafic volcanic rock; likely containing plagioclase, pyroxene, and iron-titanium oxides) — igneous
igneous

Weathered basalt pebble

Basalt, a fine-grained mafic volcanic rock; likely containing plagioclase, pyroxene, and iron-titanium oxides

AI-generated identification · may be incorrect

Hardness about 5–6 Mohs; pale gray to cream weathering rind with dark gray-black patches, dull to faintly earthy luster, and massive fine-grained texture. No obvious cleavage or visible crystals; rounded shape indicates water abrasion.

Identified More igneous
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Physical properties

Hardness about 5–6 Mohs; pale gray to cream weathering rind with dark gray-black patches, dull to faintly earthy luster, and massive fine-grained texture. No obvious cleavage or visible crystals; rounded shape indicates water abrasion.

Formation & geological history

Formed when basaltic lava rapidly cooled at or near Earth’s surface, then weathered and rounded in a river, beach, or glacial environment. Its exact geological age cannot be determined from the image.

Uses & applications

Commonly used as aggregate, road stone, riprap, and landscaping material; this rounded specimen has mainly educational or decorative value rather than gem value.

Geological facts

Basalt is the most abundant volcanic rock on oceanic crust and commonly weathers to brown, red, or cream surfaces. The dark areas may represent fresher basalt, iron-oxide staining, or weathered mafic minerals.

Field identification & locations

Identify by its heavy, fine-grained texture, dark streak or interior, lack of visible quartz, and resistance to scratching by a steel blade. Common worldwide, especially in volcanic regions, streambeds, beaches, and glacial deposits.