Rock Identifier
Amygdaloidal Basalt (Basalt with secondary mineral infilling) — igneous
igneous

Amygdaloidal Basalt

Basalt with secondary mineral infilling

Hardness: 5-6 (matrix); Color: dark gray to greenish-black; Luster: dull to earthy; Texture: Vesicular (pitted) to amygdaloidal (filled pits); Structure: Fine-grained aphanitic matrix.

Hardness
5-6 (matrix)
Color
dark gray to greenish-black
Luster
dull to earthy
Identified More igneous

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Physical properties

Hardness: 5-6 (matrix); Color: dark gray to greenish-black; Luster: dull to earthy; Texture: Vesicular (pitted) to amygdaloidal (filled pits); Structure: Fine-grained aphanitic matrix.

Formation & geological history

Formed from the rapid cooling of basaltic lava. The holes (vesicles) are created by trapped gas bubbles during eruption. If these holes later fill with minerals like quartz, calcite, or zeolites due to groundwater infiltration, it is called 'amygdaloidal'.

Uses & applications

Common basalt is used in construction as crushed stone for roads and railroads. Polished specimens are used as decorative stones or for educational geological collections.

Geological facts

Many of the world's finest copper and agate specimens are found within the amygdaloidal cavities of ancient basaltic lava flows, such as those in the Lake Superior region.

Field identification & locations

Identify in the field by its dark color, heavy weight (high specific gravity), and the presence of small rounded cavities or white/colored mineral 'spots' (amygdules) within a dense matrix.