Rock Identifier
Raw greenish beryl (probable aquamarine) (Beryl, Be₃Al₂Si₆O₁₈; blue varieties are aquamarine) — mineral
mineral

Raw greenish beryl (probable aquamarine)

Beryl, Be₃Al₂Si₆O₁₈; blue varieties are aquamarine

AI-generated identification · may be incorrect

Pale blue-green, vitreous luster, commonly hexagonal crystals with imperfect cleavage; Mohs hardness 7.5–8 and specific gravity about 2.63–2.80. The small rough crystal appears heavily included or weathered, so exact identification requires testing.

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Physical properties

Pale blue-green, vitreous luster, commonly hexagonal crystals with imperfect cleavage; Mohs hardness 7.5–8 and specific gravity about 2.63–2.80. The small rough crystal appears heavily included or weathered, so exact identification requires testing.

Formation & geological history

Forms mainly in miarolitic cavities of granitic pegmatites during late-stage cooling, typically in Precambrian to younger continental crust. Trace iron produces aquamarine’s blue-green color.

Uses & applications

Transparent aquamarine is cut for jewelry; opaque or fractured material is mainly a collector specimen. Beryl is also an important beryllium ore, though gem-quality pieces are rarely used industrially.

Geological facts

Aquamarine is the March birthstone and can be heat-treated to intensify blue color. Its characteristic hexagonal crystal habit helps distinguish it from quartz and feldspar.

Field identification & locations

Look for a hard, glassy, pale blue-green crystal and a hexagonal cross-section; it should scratch glass but not be scratched by ordinary steel. Common sources include Brazil, Pakistan, Afghanistan, Madagascar, Russia, and the United States.