Rock Identifier
Dark tumbled stone, likely basalt or black chert (Probable basalt (fine-grained plagioclase–pyroxene rock); chert is an alternative) — igneous
igneous

Dark tumbled stone, likely basalt or black chert

Probable basalt (fine-grained plagioclase–pyroxene rock); chert is an alternative

AI-generated identification · may be incorrect

Dark gray-black, fine-grained, dull to faintly vitreous luster; basalt hardness about 6–6.5 Mohs, chert about 7. No visible crystals or cleavage are resolvable from the image.

Identified More igneous
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Physical properties

Dark gray-black, fine-grained, dull to faintly vitreous luster; basalt hardness about 6–6.5 Mohs, chert about 7. No visible crystals or cleavage are resolvable from the image.

Formation & geological history

If basalt, it formed from rapidly cooled mafic lava, commonly in volcanic flows; if chert, it formed from microcrystalline quartz in sedimentary settings. Exact age and identification require a close-up or testing.

Uses & applications

Basalt is used for aggregate, roadstone, and occasionally landscaping; chert is used as a knappable stone and collectible. This small rounded specimen has little commercial value.

Geological facts

The rounded surface suggests natural abrasion or tumbling, and its scale is only a few centimeters. A streak, hardness test, and examination for vesicles or conchoidal fracture would distinguish the possibilities.

Field identification & locations

Common sources include volcanic regions worldwide for basalt and sedimentary formations worldwide for chert. Basalt is typically heavy and nonporous; chert commonly breaks with sharp, curved conchoidal fractures.