Rock Identifier
Granite River Pebble (Granite (composed of Quartz, Feldspar, and Biotite)) — igneous
igneous

Granite River Pebble

Granite (composed of Quartz, Feldspar, and Biotite)

Hardness: 6-7 Mohs; Color: Mottled tan (feldspar), grey (quartz), and black (biotite/hornblende); Luster: Vitreous when wet or polished; Crystal structure: Phaneritic (coarse-grained)

Hardness
6-7 Mohs
Luster
Vitreous when wet or polished
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Mottled tan (feldspar), grey (quartz), and black (biotite/hornblende); Luster: Vitreous when wet or polished; Crystal structure: Phaneritic (coarse-grained)

Formation & geological history

Formed from the slow cooling of silica-rich magma deep underground (plutonic). This specimen appears water-worn, smoothed by transport in a river or coastal environment over thousands of years.

Uses & applications

Used in construction, countertops, monuments, and as decorative landscaping stone. Polished river pebbles are common in home decor and aquariums.

Geological facts

Granite is the primary component of the Earth's continental crust. The specific color of this specimen suggests a high concentration of orthoclase feldspar giving it the yellowish-tan tint.

Field identification & locations

Identify in the field by its speckled 'salt and pepper' appearance and extreme hardness (it will scratch glass). Commonly found in mountainous regions or riverbeds downstream from crystalline basement rocks.