Rock Identifier
Beryl (Aquamarine) (Beryllium aluminum silicate (Be3Al2Si6O18)) — mineral
mineral

Beryl (Aquamarine)

Beryllium aluminum silicate (Be3Al2Si6O18)

Hardness: 7.5-8 on Mohs scale; Color: pale blue to greenish-blue; Luster: Vitreous to pearly; Crystal structure: Hexagonal; Cleavage: Imperfect basal; Specific gravity: 2.63-2.80.

Hardness
7
Color
pale blue to greenish-blue
Luster
Vitreous to pearly
Identified More mineral

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Physical properties

Hardness: 7.5-8 on Mohs scale; Color: pale blue to greenish-blue; Luster: Vitreous to pearly; Crystal structure: Hexagonal; Cleavage: Imperfect basal; Specific gravity: 2.63-2.80.

Formation & geological history

Commonly formed in granitic pegmatites and hydrothermal veins. Crystals grow in cavities where mineral-rich fluids cool slowly, allowing for large hexagonal shapes.

Uses & applications

Primarily used as a gemstone (jewelry) when transparent; opaque specimens are used as a source of beryllium metal for aerospace and electronics industries.

Geological facts

The blue color in aquamarine is caused by trace amounts of ferrous iron (Fe2+). It is the official state gem of Colorado.

Field identification & locations

Identify in the field by its hexagonal crystal habit, hardness (it will scratch glass and quartz), and specific pale blue-green hue. Commonly found in Brazil, Pakistan, and Madagascar.