Rock Identifier
Asphalt (Bituminous pavement) (Bituminous concrete / Asphalt) — Sedimentary (Anthropogenic)
Sedimentary (Anthropogenic)

Asphalt (Bituminous pavement)

Bituminous concrete / Asphalt

Hardness: 1-2 Mohs (can vary with temperature); Color: Charcoal-grey to black; Luster: Dull to matte; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.3 - 2.5

Hardness
1-2 Mohs (can vary with temperature)
Color
Charcoal-grey to black
Luster
Dull to matte
Identified More sedimentary (anthropogenic)

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Physical properties

Hardness: 1-2 Mohs (can vary with temperature); Color: Charcoal-grey to black; Luster: Dull to matte; Crystal structure: Amorphous; Cleavage: None; Specific gravity: 2.3 - 2.5

Formation & geological history

Formed by the refinement of crude oil (bitumen) mixed with aggregate (crushed stone, gravel, and sand). Though man-made, the core components originate from millions-of-years-old organic sediments.

Uses & applications

Primary material for road construction, parking lots, and roofing shingles. Provides a durable, water-resistant surface for automotive travel.

Geological facts

Asphalt is 100% recyclable and is the most recycled material in America. Naturally occurring asphalt deposits (like the La Brea Tar Pits) have been traps for fossils for thousands of years.

Field identification & locations

Identified in the field by its dark color, granular texture, and distinct petroleum-like smell when hot. Found globally in urban and suburban infrastructures.