• Chemistry: Be4Si2O7(OH)2, Beryllium Silicate Hydroxide.
  • Class: Silicates
  • Subclass: Sorosilicates
  • Uses: An ore of beryllium and as mineral specimens.
  • Specimens

Bertrandite was named after Leon Bertrand, a French mineralogist, and is one of the more important ores of beryllium, second only to beryl. Bertrandite is closely tied to the gemstone mineral beryl in many ways besides its use as an ore for the same metal. The two are often associated together as bertrandite is an alteration product of beryl. At times bertrandite is growing on beryl crystals and at other times bertrandite has completely replaced the beryl crystals forming a pseudomorph. A pseudomorph is an atom by atom replacement of one mineral for another; replacing the chemistry and structure with a new mineral, but preserving the outward shape of the original crystal. Pseudomorph mean false shape. Bertrandite is found in beryllium bearing pegmatitic rocks and some hydrothermal veins.


  • Color is colorless, white and pale yellow.
  • Luster is vitreous to pearly.
  • Transparency: Crystals are transparent to translucent.
  • Crystal System is orthorhombic; m m 2.
  • Crystal Habits include tabular to platy crystals and some prismatic forms. Often aggregates formed over crystals of beryl. Twinning is common. Pseudomorphs of bertrandite after beryl are also common.
  • Cleavage good in one direction lengthwise.
  • Fracture is uneven to conchoidal.
  • Hardness is 6-7.
  • Specific Gravity is 3.3-3.5
  • Streak is white to gray.
  • Other Characteristics: Some specimens have fluoresced green under UV light.
  • Associated Minerals are numerous and include of course beryl as well as quartz, albite, orthoclase, fluorapatite, micas, anatase, brookite, pyrite, fresnoite, analcime, calcite and cheralite.
  • Notable Occurrences include the type locality of Petit-Port and Barbin, Nantes, Loire-Atlantique, France aa well as Akca Tau and Kara-Oba, Kazakhstan; Zabytoe, Primorie, Russia; Spor Mountain and the Brush Beryllium Mine, Juab County, Utah; Harding Mine, New Mexico; Texas and Pala District, San Diego County, California, USA; China; Cornwall, England; Mongolia; Norway and Mexico.
  • Best Field Indicators include only one direction of cleavage, crystal habit, color, association with beryl and hardness.
BERTRANDITE specimens:
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BERTRANDITE specimen brr-1
$ 72.00
Dims:0.8x0.7x0.3" (2.0x1.8x0.3 cm)
Wt: 0.2oz. (6g)w/base
Galconda Mine, Govenador Valadares, Minas Gerais, Brazil
This specimen consists of hundreds of tiny intergrown orthorhombic prisms of bertrandite. There is no matrix material with this specimen. Some of the bertrandite crystals are transparent, showing striations and vitreous luster. Near the base of this specimen is one crystal of bertrandite showing a hexagonal shape. I believe that this is a pseudomorph of bertrandite after beryl.
no photo
brr-1 ($ 72.00)
Galconda Mine, Govenador Valadares, Minas Gerais, Brazil
BERTRANDITE specimen brr-2
$ 50.00
Dims:1.4x0.7x0.7" (3.6x1.8x1.8 cm)
Wt: 0.2oz. (7g)
Governador Valadares, Minas Gerais, Brazil
This thumbnail specimen consists of hundreds of tiny intergrown crystals of bertrandite, with no matrix at all. Close examination with a loupe reveals that many of these crystals are hexagonal in shape, leading me to believe that these are in fact pseudomorphs after beryl. Scattered sparsely over the specimen are tiny crystals of pyrite and/or chalcopyrite. There is only the most minor damage to this specimen.
no photo
brr-2 ($ 50.00)
Governador Valadares, Minas Gerais, Brazil


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