Rock Identifier
Amygdaloidal Basalt (Amygdaloidal Basalt (containing secondary minerals like Quartz, Zeolites, or Calcite)) — igneous
igneous

Amygdaloidal Basalt

Amygdaloidal Basalt (containing secondary minerals like Quartz, Zeolites, or Calcite)

Hardness: 5-7 Mohs; Color: Dark grey to greenish-black groundmass with light-colored circular or almond-shaped inclusions; Luster: Dull (matrix) to vitreous (vesicle fill); Crystal structure: Aphanitic (fine-grained) matrix with amygdules.

Hardness
5-7 Mohs
Luster
Dull (matrix) to vitreous (vesicle fill)
Identified More igneous

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Physical properties

Hardness: 5-7 Mohs; Color: Dark grey to greenish-black groundmass with light-colored circular or almond-shaped inclusions; Luster: Dull (matrix) to vitreous (vesicle fill); Crystal structure: Aphanitic (fine-grained) matrix with amygdules.

Formation & geological history

Formed from the cooling of mafic lava flows. As gas bubbles (vesicles) were trapped in the solidifying rock, they were later filled by secondary minerals precipitating from groundwater. Most common in ancient volcanic provinces (spanning from Precambrian to Cenozoic).

Uses & applications

Used primarily as decorative garden stones or aquarium decor. Exceptionally well-preserved specimens can be used for lapidary work (cabochons). Historically, when containing native copper (as in Michigan), used for metal extraction.

Geological facts

The name comes from the Greek word 'amygdala', meaning almond, referring to the shape of the mineral-filled gas bubbles. These rocks often trace the ancient migration path of hydrothermal fluids through volcanic fields.

Field identification & locations

Identify in the field by looking for a dark, heavy volcanic base pitted with lighter, rounded mineral 'spots' that don't look like standard crystals. Found commonly in Lake Superior (Michigan/Ontario), Iceland, and the Deccan Traps in India.