Rock Identifier
Basalt (potential Glacial Erratic) (Extrusive Mafic Volcanic Rock (Basalt)) — igneous
igneous

Basalt (potential Glacial Erratic)

Extrusive Mafic Volcanic Rock (Basalt)

Hardness: 6 (Mohs); Color: Dark gray to black; Luster: Dull to sub-metallic; Texture: Fine-grained/Aphanitic; Specific Gravity: 2.8–3.0.

Hardness
6 (Mohs)
Color
Dark gray to black
Luster
Dull to sub-metallic
Identified More igneous

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Physical properties

Hardness: 6 (Mohs); Color: Dark gray to black; Luster: Dull to sub-metallic; Texture: Fine-grained/Aphanitic; Specific Gravity: 2.8–3.0.

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at the surface. While the local bedrock of Northern KY/Cincinnati is sedimentary (Ordovician limestone), igneous rocks found here are typically glacial erratics transported by ice sheets from the Canadian Shield during the Pleistocene.

Uses & applications

Commonly used as crushed stone for road base, concrete aggregate, and railroad ballast. Exceptionally durable for construction.

Geological facts

Basalt is the most common rock type in the Earth's crust and makes up most of the ocean floor. It is also common on the Moon and Mars.

Field identification & locations

Identify by its dark color, heavy weight (density), and lack of visible crystals. Its presence in a sedimentary region like Northern Kentucky indicates glacial transport.