Rock Identifier
Basalt (Vesicular or Porphyritic) (Basalt (composed primarily of plagioclase feldspar, pyroxene, and olivine)) — igneous
igneous

Basalt (Vesicular or Porphyritic)

Basalt (composed primarily of plagioclase feldspar, pyroxene, and olivine)

Hardness: 6-7 on Mohs scale; Color: dark grey to black; Luster: dull to sub-metallic; Crystal structure: aphanitic (fine-grained) to porphyritic; Cleavage: none (conchoidal fracture); Specific gravity: 2.8-3.0.

Hardness
6-7 on Mohs scale
Color
dark grey to black
Luster
dull to sub-metallic
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: dark grey to black; Luster: dull to sub-metallic; Crystal structure: aphanitic (fine-grained) to porphyritic; Cleavage: none (conchoidal fracture); Specific gravity: 2.8-3.0.

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at the Earth's surface. It can be found in volcanic regions globally, often representing oceanic crust or continental flood basalts.

Uses & applications

Extensively used in construction as aggregate for roads and railroads, in concrete, and for stone masonry. It is also used in the production of rock wool (insulation) and occasionally used for decorative landscaping.

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 a primary component of the lunar maria on the Moon and much of the surface of Mars.

Field identification & locations

Identify in the field by its dark color, heavy weight (high density), and fine-grained texture. To collectors, specific textures like vesicular (holed) or porphyritic (having larger crystals embedded) are points of interest. Found on beaches near volcanic coastlines or in ancient volcanic fields.