| Bertrandite | |
| Category: | Sorosilicate |
| Formula: | Be4Si2O7(OH)2 |
| Imasymbol: | Btd[1] |
| Strunz: | 9.BD.05 |
| System: | Orthorhombic |
| Class: | Pyramidal (mm2) H-M symbol: (mm2) |
| Symmetry: | Ccm21 |
| Unit Cell: | a = 8.7135(4) Å, b = 15.268(1) Å, c = 4.5683(3) Å; Z = 4 |
| Color: | Colorless to pale yellow |
| Habit: | Thin tabular, prismatic to needle-like crystals commonly in radial clusters |
| Twinning: | Common on or forming heart- or V-shaped twins |
| Cleavage: | Perfect on ; distinct on, and |
| Mohs: | 6–7 |
| Luster: | Vitreous, pearly on cleavage surfaces |
| Diaphaneity: | Transparent |
| Gravity: | 2.59–2.60 |
| Opticalprop: | Biaxial (−) |
| Refractive: | nα = 1.591 nβ = 1.605 nγ = 1.614 |
| Birefringence: | δ = 0.023 |
| 2V: | Measured: 73° to 81° |
| References: | [2] [3] [4] |
Bertrandite is a beryllium sorosilicate hydroxide mineral with composition: Be4Si2O7(OH)2. Bertrandite is a colorless to pale yellow orthorhombic mineral with a hardness of 6–7.
It is commonly found in beryllium rich pegmatites and is in part an alteration of beryl. Bertrandite often occurs as a pseudomorphic replacement of beryl. Associated minerals include beryl, phenakite, herderite, tourmaline, muscovite, fluorite and quartz.[2]
It, with beryl, are ores of beryllium.
It was discovered near Nantes, France in 1883 and named after French mineralogist, Emile Bertrand (1844–1909).[2] [3] [4]
One of the world's largest deposits of bertrandite is Spor Mountain, Thomas Range, Utah which is currently the source of most of the world's beryllium production.[5] [6]