Rock Identifier
Granite Boulder (Felsic Intrusive Igneous Rock) — igneous
igneous

Granite Boulder

Felsic Intrusive Igneous Rock

Hardness of 6 on the Mohs scale, predominantly pinkish-grey to tan in color due to potassium feldspar and quartz, dull to sub-vitreous luster, phaneritic (coarse-grained) crystal structure with visible interlocking mineral grains, specific gravity around 2.65 to 2.75.

Identified More igneous
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Physical properties

Hardness of 6 on the Mohs scale, predominantly pinkish-grey to tan in color due to potassium feldspar and quartz, dull to sub-vitreous luster, phaneritic (coarse-grained) crystal structure with visible interlocking mineral grains, specific gravity around 2.65 to 2.75.

Formation & geological history

Formed from the slow cooling and crystallization of magma rich in silica and alkali metals far beneath the Earth's surface, typically over millions of years.

Uses & applications

Widely used in construction, architectural building facades, monuments, countertops, paving stones, and as landscape boulders.

Geological facts

Granite makes up a major part of continental crusts and is one of the toughest natural building materials known to humanity, capable of withstanding severe weathering.

Field identification & locations

Identified by the distinct visible crystals of quartz, feldspar, and micas (such as biotite). Common worldwide in continental shields and mountain roots.