Rock Identifier
Granitic Pegmatite (Granite (with coarse-grained Quartz, Feldspar, and Mica components)) — igneous
igneous

Granitic Pegmatite

Granite (with coarse-grained Quartz, Feldspar, and Mica components)

Hardness: 6-7 (Mohs scale); Color: Mottled white, gray, and pink/tan with dark flecks; Luster: Vitreous to pearly; Crystal structure: Phaneritic (large, visible crystals); Cleavage: Perfect in feldspar and mica inclusions; Specific gravity: 2.6-2.7

Hardness
6-7 (Mohs scale)
Color
Mottled white, gray, and pink/tan with dark flecks
Luster
Vitreous to pearly
Identified More igneous

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Physical properties

Hardness: 6-7 (Mohs scale); Color: Mottled white, gray, and pink/tan with dark flecks; Luster: Vitreous to pearly; Crystal structure: Phaneritic (large, visible crystals); Cleavage: Perfect in feldspar and mica inclusions; Specific gravity: 2.6-2.7

Formation & geological history

Formed from the slow cooling of magma deep within the Earth's crust, allowing large crystals to grow. Typically found in Plutonic environments and ancient continental shields.

Uses & applications

Used in construction as crushed stone, architectural facades, and countertops. Also a source of industrial minerals like quartz and mica.

Geological facts

Pegmatites are known for containing the largest crystals of any rock type on Earth. This specimen shows a mix of milky quartz and alkaline feldspar.

Field identification & locations

Identify in the field by its coarse, 'salt and pepper' crystalline texture and extreme hardness (cannot be scratched by a steel knife). Commonly found in mountain ranges and glacial till.