Rock Identifier
Granite Cobble (Phaneritic Felsic Igneous Rock) — igneous
igneous

Granite Cobble

Phaneritic Felsic Igneous Rock

Hardness: 6-7 Mohs; Color: Pinkish-tan with black and clear specs; Luster: Dull (weathered) to vitreous (on fresh surfaces); Crystal Structure: Phaneritic (visible grains of quartz, feldspar, and mica); Specific Gravity: 2.63-2.75

Hardness
6-7 Mohs
Color
Pinkish-tan with black and clear specs
Luster
Dull (weathered) to vitreous (on fresh surfaces)
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Pinkish-tan with black and clear specs; Luster: Dull (weathered) to vitreous (on fresh surfaces); Crystal Structure: Phaneritic (visible grains of quartz, feldspar, and mica); Specific Gravity: 2.63-2.75

Formation & geological history

Formed through the slow crystallization of magma below Earth's surface. This specific specimen is a water-worn river stone or glacial cobble, rounded by mechanical erosion over thousands of years.

Uses & applications

Used in construction, countertops, monuments, and as decorative landscaping aggregate.

Geological facts

Granite makes up a large portion of the Earth's continental crust. The pink color in this specimen comes from potassium feldspar (orthoclase).

Field identification & locations

Identify in the field by its 'salt and pepper' appearance and hardness (it will scratch glass). This rounded shape indicates it was transported by water or ice far from its original source.