Rock Identifier
Porphyritic Basalt with Quartz Inclusions (Aphanitic Porphyritic Basalt) — Igneous
Igneous

Porphyritic Basalt with Quartz Inclusions

Aphanitic Porphyritic Basalt

Hardness: 6-7 (Mohs); Color: dark grey to black matrix with white/clear inclusions; Luster: dull to vitreous; Structure: aphanitic (fine-grained) with phenocrysts; Cleavage: none (conchoidal fracture).

Hardness
6-7 (Mohs)
Color
dark grey to black matrix with white/clear inclusions
Luster
dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs); Color: dark grey to black matrix with white/clear inclusions; Luster: dull to vitreous; Structure: aphanitic (fine-grained) with phenocrysts; Cleavage: none (conchoidal fracture).

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at or near the Earth's surface, typically at mid-ocean ridges or hotspots. The large crystals (phenocrysts) formed slowly at depth before eruption.

Uses & applications

Commonly used as crushed stone for aggregate in construction, road base, and railroad ballast. Larger pieces are sometimes used in architectural facing or as decorative garden stones.

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 found extensively on the Moon and Mars.

Field identification & locations

Identified by its heavy weight, dark color, and fine-grained matrix containing visible larger crystals. Found globally in volcanic regions such as Iceland, Hawaii, and the Pacific Northwest.