Rock Identifier
Granite Cobble (Granitic intrusive igneous rock (Quartz, Feldspar, Mica)) — igneous
igneous

Granite Cobble

Granitic intrusive igneous rock (Quartz, Feldspar, Mica)

Hardness: 6-7 on Mohs scale. Color: Mottled tan, grey, and black. Luster: Dull/earthy surface when weathered, vitreous on fresh breaks. Structure: Phaneritic (coarse-grained) crystalline texture. Specific gravity: ~2.63-2.75.

Hardness
6-7 on Mohs scale
Color
Mottled tan, grey, and black
Luster
Dull/earthy surface when weathered, vitreous on fresh breaks
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale. Color: Mottled tan, grey, and black. Luster: Dull/earthy surface when weathered, vitreous on fresh breaks. Structure: Phaneritic (coarse-grained) crystalline texture. Specific gravity: ~2.63-2.75.

Formation & geological history

Formed from the slow cooling of silica-rich magma deep underground. This specific specimen has been chemically weathered and physically rounded by water or glacial transport. Age can range from hundreds of millions to billions of years depending on the pluton of origin.

Uses & applications

Used primarily as construction aggregate, road base, and landscape gravel. Polished granite is used for countertops and monuments.

Geological facts

Granite makes up much of the Earth's continental crust. Because it is highly resistant to abrasion and weathering, it often survives as rounded cobbles in riverbeds long after softer rocks have eroded away.

Field identification & locations

Identify in the field by its 'salt and pepper' appearance and hardness (it will scratch glass). Commonly found in glacial till, riverbeds, and mountainous regions. It is one of the most common rocks on the planet.