Rock Identifier
Granite with Mafic Inclusions (Granite (Phaneritic igneous rock composed of Quartz, Feldspar, and Mica)) — igneous
igneous

Granite with Mafic Inclusions

Granite (Phaneritic igneous rock composed of Quartz, Feldspar, and Mica)

Hardness: 6-7 (Mohs scale), Color: Light gray matrix with a dark gray/black band, Luster: Dull to pearly, Crystal structure: Phaneritic (visible grains), Cleavage: None for the rock overall, though mineral components may show it.

Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale), Color: Light gray matrix with a dark gray/black band, Luster: Dull to pearly, Crystal structure: Phaneritic (visible grains), Cleavage: None for the rock overall, though mineral components may show it.

Formation & geological history

Formed from the slow underwater cooling of magma beneath the Earth's surface (intrusive). The dark band likely represents a mafic inclusion or a small dike of different mineral composition (like diorite or basaltic melt) that intruded the granite body.

Uses & applications

Used primarily in construction (countertops, tiles, paving), monuments, and as crushed stone for road base. Specimens with unique banding are sometimes kept as geological educational samples.

Geological facts

Granite makes up a large portion of the Earth's continental crust. The dark stripes in granite, like the one seen here, are often called 'xenoliths' if they are chunks of older rock that got stuck in the magma, or 'schlieren' if they are concentrated streaks of dark minerals.

Field identification & locations

Identify by its 'salt and pepper' granular appearance and its extreme hardness; it cannot be scratched by a steel knife. Commonly found in mountain ranges and ancient shields like the Canadian Shield.