Rock Identifier
Grey River Pebble (Greywacke / Basalt) (Stream-rounded silicate rock pebble) — sedimentary
sedimentary

Grey River Pebble (Greywacke / Basalt)

Stream-rounded silicate rock pebble

Hardness: 6-7 on Mohs scale. Color: Dark grey with faint white veinings. Luster: Dull to sub-vitreous when dry. Structure: Fine-grained, microcrystalline to clastic matrix. Cleavage: None (conchoidal to uneven fracture).

Hardness
6-7 on Mohs scale
Color
Dark grey with faint white veinings
Luster
Dull to sub-vitreous when dry
Identified More sedimentary
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Physical properties

Hardness: 6-7 on Mohs scale. Color: Dark grey with faint white veinings. Luster: Dull to sub-vitreous when dry. Structure: Fine-grained, microcrystalline to clastic matrix. Cleavage: None (conchoidal to uneven fracture).

Formation & geological history

Formed through the erosion, mechanical weathering, and stream transport of fine-grained sedimentary rock (like greywacke or shale) or fine-grained igneous rock (like basalt). The rounded shape is caused by natural water attrition over time.

Uses & applications

Commonly used in landscaping, river rock gardens, aquarium decor, and aggregate in construction.

Geological facts

Smooth pebbles like this are natural indicators of ancient or present watercourses, such as rivers, streams, and beaches, where water flow naturally grinds sharp rock fragments into smooth oval shapes.

Field identification & locations

Identify in the field by its smooth, water-worn exterior, rounded edges, and uniform fine-grained grey texture with fine calcite or quartz veinlets. Commonly found along riverbanks, gravel bars, and coastal beaches.