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

Amygdaloidal Basalt

Basalt with secondary mineral infilling

Hardness: 5-6 (matrix); Color: Dark grey to dull green with white/buff spots; Luster: Dull to earthy; Structure: Vesicular/Amygdaloidal; Specific Gravity: 2.8-3.0

Hardness
5-6 (matrix)
Color
Dark grey to dull green with white/buff spots
Luster
Dull to earthy
Identified More igneous

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 5-6 (matrix); Color: Dark grey to dull green with white/buff spots; Luster: Dull to earthy; Structure: Vesicular/Amygdaloidal; Specific Gravity: 2.8-3.0

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava. The 'spots' are amyg dules, which formed when gas bubbles (vesicles) in the cooling lava were later filled with secondary minerals like quartz, calcite, or zeolites through groundwater infiltration.

Uses & applications

Primarily used as crushed stone for aggregate in construction, road base, and concrete. Interesting specimens are used for educational purposes and geological collecting.

Geological facts

Amygdaloidal textures are common in ancient volcanic flows, such as those found in the Lake Superior region of North America, where these pockets can sometimes contain native copper or semi-precious gemstones.

Field identification & locations

Identify by the dark, fine-grained volcanic matrix containing rounded, light-colored mineral 'pockets.' Commonly found in volcanic terrains and glacial till in volcanic regions.