Rock Identifier
Porphyritic Basalt (with Amygdales) (Amygdaloidal Porphyritic Basalt) — igneous
igneous

Porphyritic Basalt (with Amygdales)

Amygdaloidal Porphyritic Basalt

Hardness: 5-6 (Mohs); Color: Dark brown to reddish-purple groundmass with white/clear mineral inclusions; Luster: Dull to sub-vitreous; Structure: Aphanitic (fine-grained) matrix with visible phenocrysts/vesicle fillings; Specific Gravity: 2.8–3.0

Hardness
5-6 (Mohs)
Luster
Dull to sub-vitreous
Identified More igneous

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Physical properties

Hardness: 5-6 (Mohs); Color: Dark brown to reddish-purple groundmass with white/clear mineral inclusions; Luster: Dull to sub-vitreous; Structure: Aphanitic (fine-grained) matrix with visible phenocrysts/vesicle fillings; Specific Gravity: 2.8–3.0

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at or near the Earth's surface. The 'holes' (vesicles) were formed by gas bubbles trapping in cooling lava, which later filled with secondary minerals like quartz, calcite, or zeolites through hydrothermal activity.

Uses & applications

Commonly used as crushed stone for aggregate in construction, road base, and railroad ballast. Decorative specimens are used in landscaping or small-scale geology collections.

Geological facts

The reddish-purple hue suggests high iron content that has undergone oxidation (weathering). These rocks often record the volatile content of ancient volcanic eruptions through their gas-bubble patterns.

Field identification & locations

Identify in the field by looking for a dense, dark, fine-grained rock containing distinct small white or translucent 'spots' that don't look like regular rounded pebbles (as in conglomerate) but rather secondary mineral growths. Frequently found in volcanic fields like the Deccan Traps or the Lake Superior region.