Rock Identifier
Speckled rounded stone, possibly basalt or diorite (Indeterminate mafic/intermediate igneous rock; likely fine-grained basaltic or dioritic material) — igneous
igneous

Speckled rounded stone, possibly basalt or diorite

Indeterminate mafic/intermediate igneous rock; likely fine-grained basaltic or dioritic material

AI-generated identification · may be incorrect

Small, rounded gray-green specimen with abundant dark speckles and a dull to slightly granular luster. Likely hardness about 5.5–7 Mohs, with no visible cleavage; exact texture and density cannot be confirmed from the blurred image.

Identified More igneous
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Physical properties

Small, rounded gray-green specimen with abundant dark speckles and a dull to slightly granular luster. Likely hardness about 5.5–7 Mohs, with no visible cleavage; exact texture and density cannot be confirmed from the blurred image.

Formation & geological history

Likely formed when silica-poor to intermediate magma cooled, probably as basalt or a related intrusive rock. Geological age and exact formation setting are indeterminate without testing.

Uses & applications

Common rock fragments are mainly of educational or decorative interest; basalt and diorite are also used as aggregate, paving stone, and dimension stone.

Geological facts

The dark spotted appearance may reflect pyroxene, amphibole, or biotite crystals in a lighter feldspar-rich groundmass. The object could also be a tumbled or weathered fragment rather than a naturally spherical specimen.

Field identification & locations

Field identification requires a fresh surface, hand lens, streak, magnetism, hardness, and specific-gravity tests; basalt is commonly darker and denser, while diorite is typically coarser and salt-and-pepper patterned. Common globally in volcanic and plutonic terrains.