Rock Identifier
Granite Boulder (Glacial Erratic) (Granite) — igneous
igneous

Granite Boulder (Glacial Erratic)

Granite

Hardness: 6-7 on Mohs scale. Color: Speckled grey, pink, and white with dark flecks. Luster: Dull to vitreous on fresh surfaces. Texture: Phaneritic (coarse-grained intrusive igneous texture). Density: ~2.65-2.75 g/cm3.

Hardness
6-7 on Mohs scale
Color
Speckled grey, pink, and white with dark flecks
Luster
Dull to vitreous on fresh surfaces
Identified More igneous
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Physical properties

Hardness: 6-7 on Mohs scale. Color: Speckled grey, pink, and white with dark flecks. Luster: Dull to vitreous on fresh surfaces. Texture: Phaneritic (coarse-grained intrusive igneous texture). Density: ~2.65-2.75 g/cm3.

Formation & geological history

Formed from the slow crystallization of magma below Earth's surface (plutonic). This rounded boulder was likely transported and smoothed by glacial activity during the last Ice Age, resulting in a glacial erratic.

Uses & applications

Used widely in landscaping, construction, dimension stone, building foundations, and aggregate material.

Geological facts

Granite makes up a major portion of Earth's continental crust. Rounded landscape boulders like this are often glacial erratics deposited miles away from their original bedrock source.

Field identification & locations

Identified by its interlocking coarse grains of quartz, potassium feldspar, plagioclase feldspar, and biotite mica or hornblende. Commonly found in glaciated regions and mountainous areas worldwide.