Rock Identifier
Porphyritic Basalt (Porphyritic Basalt with Plagioclase Phenocrysts) — igneous
igneous

Porphyritic Basalt

Porphyritic Basalt with Plagioclase Phenocrysts

Hardness of 6 on the Mohs scale for feldspar phenocrysts, dark grey to black groundmass with contrasting white or light grey rounded phenocrysts, dull to sub-aphanitic luster, aphanitic-porphyritic texture, specific gravity around 2.8-3.0.

Identified More igneous
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Physical properties

Hardness of 6 on the Mohs scale for feldspar phenocrysts, dark grey to black groundmass with contrasting white or light grey rounded phenocrysts, dull to sub-aphanitic luster, aphanitic-porphyritic texture, specific gravity around 2.8-3.0.

Formation & geological history

Formed via a two-stage cooling process where early-formed minerals (phenocrysts) grew slowly in a magma chamber before the remaining magma erupted and cooled rapidly at or near the Earth's surface.

Uses & applications

Used primarily in construction as crushed aggregate, roadstone, and building stone. Unique spotted specimens are also collected by rockhounds and lapidary enthusiasts.

Geological facts

The distinctive spotted appearance has led to common regional nicknames such as 'leopard rock' or 'porcupine rock' depending on the shape and distribution of the crystals.

Field identification & locations

Easily identified in the field by its contrasting large, light-colored crystals embedded in a dark, fine-grained volcanic matrix. Commonly found in ancient and modern volcanic provinces worldwide.