
Mineral
Beryl (Variety Mix)
Be3Al2(Si6O18)
Hardness: 7.5-8 on Mohs scale. Color: This string showcases a mix of Beryl varieties, including Aquamarine (light blue/green-blue), Morganite (pink/rose), Heliodor (yellow/yellow-green), and common Beryl (white/pale green). Luster: Vitreous to resinous. Crystal Structure: Hexagonal.…
- Hardness
- 7
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 7.5-8 on Mohs scale. Color: This string showcases a mix of Beryl varieties, including Aquamarine (light blue/green-blue), Morganite (pink/rose), Heliodor (yellow/yellow-green), and common Beryl (white/pale green). Luster: Vitreous to resinous. Crystal Structure: Hexagonal. Cleavage: Indistinct on the basal plane. Specific Gravity: 2.65-2.80.
Formation & geological history
Beryl typically forms in igneous and metamorphic rocks. It is most commonly found in granitic pegmatites, but also occurs in mica schists and in hydrothermal veins. The specific color varieties are due to trace impurities: iron for aquamarine and heliodor, manganese for morganite, and chromium/vanadium for emerald (not clearly present here). Formation occurs as magma cools slowly, allowing large crystals to grow, or under high temperature and pressure conditions in metamorphic settings. Geological Age: Varies widely, found in formations from Precambrian to Tertiary periods.
Uses & applications
All gem-quality varieties of Beryl are highly valued as gemstones for jewelry (e.g., Aquamarine, Morganite, Emerald, Heliodor, Goshenite). Due to its hardness, it's suitable for various jewelry settings. Historically, Beryl has been a source of beryllium, a lightweight metal used in aerospace, nuclear reactors, and high-tech ceramics.
Geological facts
Beryl is a single mineral species, but it comes in a breathtaking array of colors, each with its own varietal name. The most famous Beryl variety is emerald, known for its intense green color. Aquamarine gets its name from 'aqua marina', meaning 'water of the sea', reflecting its beautiful blue-green hues. Morganite was named after J.P. Morgan, a prominent banker and gem collector. Goshenite is the colorless variety of beryl.
Field identification & locations
Identify Beryl by its hexagonal crystal structure (though these are tumbled beads, making crystal structure less obvious), relatively high hardness, vitreous luster, and wide range of characteristic pastel colors. It is often found in pegmatite formations, where large crystals can be extracted. Major sources include Brazil, Pakistan, Afghanistan, Russia, Namibia, and the USA. In the field, look for hexagonal prisms in granitic rocks. Collectors value Beryl for its diverse colors and gemological significance. The beads shown are likely tumbled and polished, obscuring natural crystal forms but highlighting the varied colors of the Beryl family.
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