Rich bluish-green to pure vivid green; trace chromium and vanadium impart the signature emerald hue.
Chemical formula
Be₃Al₂(SiO₃)₆ + Cr³⁺/V³⁺ (Beryllium Aluminum Silicate with Chromium and/or Vanadium)Soft rose pink, peach, and salmon-pink hues caused by trace manganese; often forms flat tabular hexagonal crystals.
| Mineral Family | Beryl |
|---|---|
| Mineral Species | Beryl |
| Gemological Variety | Morganite |
| Chemical Composition | Be₃Al₂(SiO₃)₆ + Mn²⁺/Mn³⁺ |
| Crystal System | Hexagonal |
| Mohs Hardness | 7.5 – 8.0 Mohs |
| Specific Gravity | 2.71 – 2.90 (elevated by cesium content in pegmatitic beryls) |
| Refractive Index | 1.585 – 1.594 |
Soft rose pink, peach, and salmon-pink hues caused by trace manganese; often forms flat tabular hexagonal crystals.
Forms in lithium- and cesium-enriched granitic pegmatites in Pakistan (Skardu/Shigar), Afghanistan (Nuristan), Brazil, and Madagascar.
Tabular pink crystals from the Hindu Kush and Karakoram mountains are prized by crystal collectors for their sharp geometry and association with tourmaline and cleavelandite.
Highly favored for rose-gold engagement rings, cushion-cut pendants, and statement earrings.
Frequently heat-treated at low temperatures or irradiated/annealed to convert yellow/orange modifiers into pure pink. Treatment status is disclosed per specimen.
Wash gently in warm soapy water; store away from sustained intense heat.
Named after financier and mineral collector J.P. Morgan in 1911; associated with warmth, gentleness, and heartfelt connection.
Note: Cultural and birthstone traditions are presented strictly as historical folklore, never as scientifically verified medical or metaphysical effects.
Rich bluish-green to pure vivid green; trace chromium and vanadium impart the signature emerald hue.
Be₃Al₂(SiO₃)₆ + Cr³⁺/V³⁺ (Beryllium Aluminum Silicate with Chromium and/or Vanadium)
Pastel sky blue to deep sea-blue and greenish-blue, colored by trace iron within the hexagonal channel structure.
Be₃Al₂(SiO₃)₆ + Fe²⁺/Fe³⁺
Lemon yellow, golden honey, to greenish-yellow, colored by ferric iron (Fe3+) substituting for aluminum.
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