Rock Identifier
Scoria (Vesicular Basalt / Scoria (Mafic silicate rock)) — Igneous
Igneous

Scoria

Vesicular Basalt / Scoria (Mafic silicate rock)

Hardness: 5-6 Mohs. Color: Typically reddish-brown to dark grey/black. Luster: Dull or earthy. Structure: Highly vesicular (honeycombed with gas bubbles). Cleavage: None. Specific gravity: Low (often floats briefly, though denser than pumice).

Hardness
5-6 Mohs
Color
Typically reddish-brown to dark grey/black
Luster
Dull or earthy
Identified More igneous

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Physical properties

Hardness: 5-6 Mohs. Color: Typically reddish-brown to dark grey/black. Luster: Dull or earthy. Structure: Highly vesicular (honeycombed with gas bubbles). Cleavage: None. Specific gravity: Low (often floats briefly, though denser than pumice).

Formation & geological history

Formed from the rapid cooling of basaltic or andesitic lava under high pressure. Gas bubbles are trapped as the lava solidifies near the surface of volcanic vents or on the surface of lava flows during Cenozoic to recent eruptions.

Uses & applications

Used extensively in landscaping and decorative gardens, as lightweight aggregate in drainage systems, for high-temperature insulation in gas grills (lava rocks), and in road construction for traction.

Geological facts

Unlike its cousin pumice, scoria is mafic and usually sinks in water due to its thicker cell walls and higher iron content. It is a primary component of cinder cones, which are formed by explosive fountaining of lava.

Field identification & locations

Identify by its 'Swiss cheese' appearance, rough/abrasive texture, and reddish-brown oxidation. Commonly found in volcanic regions like Iceland, Hawaii, the Canary Islands, and the Western United States. Collectors should look for unique aerodynamic shapes known as spindle bombs.