Rock Identifier
Porphyritic Basalt (Porphyritic Basalt (Mafic extrusive rock)) — igneous
igneous

Porphyritic Basalt

Porphyritic Basalt (Mafic extrusive rock)

Hardness: 6-7 (Mohs); Color: Dark grey to black groundmass with light-colored white/cream phenocrysts; Luster: Dull to sub-vitreous; Texture: Porphyritic (fine-grained matrix with larger visible crystals); Cleavage: None (conchoidal fracture); Specific Gravity: 2.8-3.0.

Hardness
6-7 (Mohs)
Luster
Dull to sub-vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs); Color: Dark grey to black groundmass with light-colored white/cream phenocrysts; Luster: Dull to sub-vitreous; Texture: Porphyritic (fine-grained matrix with larger visible crystals); Cleavage: None (conchoidal fracture); Specific Gravity: 2.8-3.0.

Formation & geological history

Formed from the cooling of magnesium-rich and iron-rich lava. The large crystals (phenocrysts), typically plagioclase feldspar, formed slowly underground before a volcanic eruption caused the remaining liquid lava to cool quickly on the surface, creating the fine-grained matrix.

Uses & applications

Commonly used in construction as crushed stone for road base, concrete aggregate, and railroad ballast. Select pieces are used as decorative garden stones or for lapidary work like pavers and tiles.

Geological facts

Basalt is the most common rock type on Earth's crust and also makes up most of the ocean floors. Porphyritic textures are significant because they record two distinct stages of cooling in a single volcanic event.

Field identification & locations

Identify in the field by looking for a 'salt and pepper' look where white rectangular crystals are embedded in a dark, dense, heavy rock. Found globally in volcanic fields like the Pacific Northwest (USA), Iceland, and India's Deccan Traps.