
mineral
Rough beryl, possibly green beryl or aquamarine
Beryl, Be₃Al₂Si₆O₁₈
AI-generated identification · may be incorrectTranslucent blue-green to yellow-green, vitreous luster, hexagonal crystal structure; Mohs hardness 7.5–8, with indistinct cleavage. The pictured fragment appears naturally fractured; color alone cannot confirm gem quality or variety.
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Physical properties
Translucent blue-green to yellow-green, vitreous luster, hexagonal crystal structure; Mohs hardness 7.5–8, with indistinct cleavage. The pictured fragment appears naturally fractured; color alone cannot confirm gem quality or variety.
Formation & geological history
Beryl crystallizes in granitic pegmatites and some metamorphic rocks as magma cools and concentrates beryllium; specimens can form across many geological ages.
Uses & applications
Gem-quality beryl is cut for jewelry; lower-grade material is collected, and beryl is an important source of beryllium for specialized alloys and technology.
Geological facts
Aquamarine is blue to blue-green beryl, while emerald is chromium- or vanadium-colored beryl; greenish pieces may be called green beryl rather than emerald.
Field identification & locations
Look for glassy translucence and, on intact crystals, a six-sided prismatic shape; common sources include Brazil, Madagascar, Nigeria, and Afghanistan. The image does not show enough crystal form to determine the variety confidently.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous