Rock Identifier
Crushed Granite Gravel (Granite (composed primarily of Quartz, Alkali Feldspar, and Plagioclase Feldspar)) — igneous
igneous

Crushed Granite Gravel

Granite (composed primarily of Quartz, Alkali Feldspar, and Plagioclase Feldspar)

Hardness: 6-7 Mohs; Color: Salt and pepper (pink, gray, white, and black); Luster: Dull to vitreous; Crystal Structure: Phaneritic (coarse-grained); Cleavage: Imperfect; Specific Gravity: 2.63-2.75

Hardness
6-7 Mohs
Color
Salt and pepper (pink, gray, white, and black)
Luster
Dull to vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 Mohs; Color: Salt and pepper (pink, gray, white, and black); Luster: Dull to vitreous; Crystal Structure: Phaneritic (coarse-grained); Cleavage: Imperfect; Specific Gravity: 2.63-2.75

Formation & geological history

Formed by the slow cooling of magma deep beneath the Earth's surface (plutonic formation), typically during Orogeny events millions of years ago. These specific specimens are mechanically crushed and screened from larger quarry deposits.

Uses & applications

Extensively used in construction for road base, railway ballast, concrete aggregate, decorative landscaping, and driveways.

Geological facts

Granite is the most common rock type found in the Earth's continental crust. It is so durable that it was used by Ancient Egyptians to build temples and line the insides of the Great Pyramid of Giza.

Field identification & locations

Identify in the field by its speckled 'salt and pepper' appearance and visible interlocking crystals. Common in mountainous regions or shield areas like the Canadian Shield. For collectors, look for versions with high potassium feldspar content for a deep pink/red color.