Rock Identifier
K-feldspar Granite / Red Granite Fragment (Alkali feldspar granite (Plutonic igneous rock)) — igneous
igneous

K-feldspar Granite / Red Granite Fragment

Alkali feldspar granite (Plutonic igneous rock)

Hardness of 6-7 on the Mohs scale, reddish-pink to orange color due to potassium feldspar, vitreous to dull luster, phaneritic (coarse-grained) crystal structure, specific gravity around 2.65-2.75.

Identified More igneous
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Physical properties

Hardness of 6-7 on the Mohs scale, reddish-pink to orange color due to potassium feldspar, vitreous to dull luster, phaneritic (coarse-grained) crystal structure, specific gravity around 2.65-2.75.

Formation & geological history

Formed from the slow cooling and crystallization of magma rich in silica and potassium deep beneath the Earth's crust, typically during mountain-building events over millions of years.

Uses & applications

Used in construction, as dimension stone for buildings, monuments, countertops, and by rock collectors.

Geological facts

Granite is the most common igneous rock in the Earth's continental crust. The pink coloration in this specific sample comes from orthoclase or microcline feldspar enriched with iron impurities.

Field identification & locations

Can be identified by its prominent pinkish-red mineral grains mixed with translucent quartz and dark biotite mica. Commonly found in glacial drift, riverbeds, and mountainous regions worldwide.