Rock Identifier
Aquamarine bead bracelet (Beryl, Be₃Al₂Si₆O₁₈; blue color is typically caused by trace iron) — gemstone
gemstone

Aquamarine bead bracelet

Beryl, Be₃Al₂Si₆O₁₈; blue color is typically caused by trace iron

AI-generated identification · may be incorrect

Pale blue, translucent, vitreous beads, likely polished natural beryl. Aquamarine has Mohs hardness 7.5–8 and a hexagonal crystal structure; the beads’ internal texture and exact identity cannot be confirmed from the image alone.

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Physical properties

Pale blue, translucent, vitreous beads, likely polished natural beryl. Aquamarine has Mohs hardness 7.5–8 and a hexagonal crystal structure; the beads’ internal texture and exact identity cannot be confirmed from the image alone.

Formation & geological history

Beryl forms in pegmatites and some hydrothermal veins; aquamarine-bearing deposits occur in Brazil, Madagascar, Pakistan, and elsewhere. The bracelet’s beads are cut and polished from mined material; the mineral may be millions to billions of years old.

Uses & applications

Aquamarine is used in jewelry and as a collectible gemstone; beryl also has limited industrial use as a beryllium ore.

Geological facts

Aquamarine is the blue-to-blue-green variety of beryl; its name derives from Latin for “water of the sea.”

Field identification & locations

Look for natural inclusions, glassy luster, and hardness, but gem testing is needed to distinguish it from look-alike materials. Beads are commonly drilled and polished, obscuring crystal form.