Rock Identifier
Granite cobblestone paving (Granite, primarily quartz, feldspar, and mica; likely gray granite or granodiorite) — igneous
igneous

Granite cobblestone paving

Granite, primarily quartz, feldspar, and mica; likely gray granite or granodiorite

AI-generated identification · may be incorrect

Medium- to coarse-grained, gray mottled color with dark minerals, vitreous to dull luster, interlocking crystalline texture, Mohs hardness about 6–7, and no prominent cleavage as a whole rock. Individual paving blocks are sawn or split and weathered.

Identified More igneous
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Physical properties

Medium- to coarse-grained, gray mottled color with dark minerals, vitreous to dull luster, interlocking crystalline texture, Mohs hardness about 6–7, and no prominent cleavage as a whole rock. Individual paving blocks are sawn or split and weathered.

Formation & geological history

An intrusive igneous rock crystallized slowly from silica-rich magma deep underground, commonly during Precambrian to Phanerozoic continental magmatism. The visible blocks are quarried, cut, and used as street paving.

Uses & applications

Highly durable for cobblestone streets, curbs, paving, and building stone; attractive pieces may be used decoratively, but these are construction-grade rather than collectible specimens.

Geological facts

Granite resists abrasion and heavy traffic because of its interlocking quartz–feldspar framework. The pale crystals are usually feldspar or quartz, while black grains are commonly biotite or hornblende.

Field identification & locations

Identify it by visible granular crystals, gray speckling, and great resistance to scratching; it differs from basalt by being lighter and visibly crystalline. Common paving granites come from quarries worldwide, including Europe, China, India, and North America.