Rock Identifier
Basalt with Quartz/Calcite Vein (Basalt (Mafic Volcanic Rock with secondary mineralization)) — igneous
igneous

Basalt with Quartz/Calcite Vein

Basalt (Mafic Volcanic Rock with secondary mineralization)

Hardness: 5-6 (matrix); Color: Dark brown to charcoal gray with a tan/white vein; Luster: Dull/Earthy; Crystal Structure: Aphanitic (fine-grained) matrix with a secondary crystalline vein; Cleavage: None (conchoidal fracture in matrix).

Hardness
5-6 (matrix)
Color
Dark brown to charcoal gray with a tan/white vein
Luster
Dull/Earthy
Identified More igneous

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Physical properties

Hardness: 5-6 (matrix); Color: Dark brown to charcoal gray with a tan/white vein; Luster: Dull/Earthy; Crystal Structure: Aphanitic (fine-grained) matrix with a secondary crystalline vein; Cleavage: None (conchoidal fracture in matrix).

Formation & geological history

Basalt forms from the rapid cooling of magnesium-rich and iron-rich lava at or near the Earth's surface. This specimen features a secondary mineral vein (likely quartz or calcite) deposited by hydrothermal fluids moving through cracks in the rock long after the basalt solidified.

Uses & applications

Basalt is widely used in construction as aggregate for roads, railroad ballast, and in the production of high-strength stone wool insulation. Collectors value specimens with distinct mineral veining for display.

Geological facts

Basalt is the most common rock type in the Earth's crust and makes up most of the ocean floor. The dark color is due to the presence of pyroxene and calcium-rich plagioclase feldspar.

Field identification & locations

Identify in the field by its heavy weight (high specific gravity), dark color, and fine-grained texture. Look for the distinct contrasting 'stripe' of the vein. Common in volcanic regions such as the Pacific Northwest, Hawaii, and Iceland.