
mineral
Pale green rough beryl (possibly aquamarine)
Beryl, Be₃Al₂Si₆O₁₈; aquamarine is blue to blue-green beryl
AI-generated identification · may be incorrectTranslucent pale blue-green, vitreous luster; hexagonal crystal system, Mohs hardness 7.5–8, no obvious cleavage. The photo alone cannot confirm the species or gem quality.
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Physical properties
Translucent pale blue-green, vitreous luster; hexagonal crystal system, Mohs hardness 7.5–8, no obvious cleavage. The photo alone cannot confirm the species or gem quality.
Formation & geological history
Beryl crystallizes in granitic pegmatites and some metamorphic rocks as magma cools; specimens may range from ancient to geologically recent, depending on deposit.
Uses & applications
Gem-quality aquamarine is cut for jewelry; common or fractured beryl is collected as a mineral specimen and can be an important beryllium ore.
Geological facts
Beryl’s color depends on trace elements: iron produces aquamarine’s blue-green hues, while chromium or vanadium can produce emerald.
Field identification & locations
Look for a hexagonal prism, vitreous surface, and hardness sufficient to scratch glass; color and shape in this irregular fragment are not diagnostic. Beryl occurs in pegmatites worldwide, including Brazil, Madagascar, and Pakistan.
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