Bertrandite

Sorosilicate mineral


title: "Bertrandite" type: doc version: 1 created: 2026-02-28 author: "Wikipedia contributors" status: active scope: public tags: ["beryllium-minerals", "sorosilicates", "orthorhombic-minerals", "minerals-in-space-group-36"] description: "Sorosilicate mineral" topic_path: "general/beryllium-minerals" source: "https://en.wikipedia.org/wiki/Bertrandite" license: "CC BY-SA 4.0" wikipedia_page_id: 0 wikipedia_revision_id: 0

::summary Sorosilicate mineral ::

::data[format=table title="Infobox mineral"]

FieldValue
nameBertrandite
imageBertrandite-38545.jpg
captionBertrandite from the Golconda pegmatite, Minas Gerais, Brazil
categorySorosilicate
formulaBe4Si2O7(OH)2
IMAsymbolBtd
strunz9.BD.05
systemOrthorhombic
classPyramidal (mm2)
H-M symbol: (mm2)
symmetryCcm21
unit cella = 8.7135(4) Å,
b = 15.268(1) Å,
c = 4.5683(3) Å; Z = 4
colorColorless to pale yellow
habitThin tabular, prismatic to needle-like crystals commonly in radial clusters
twinningCommon on {011} or {021} forming heart- or V-shaped twins
cleavagePerfect on {001}; distinct on {100}, {010} and {110}
mohs6–7
lusterVitreous, pearly on cleavage surfaces
diaphaneityTransparent
gravity2.59–2.60
opticalpropBiaxial (−)
refractivenα = 1.591 nβ = 1.605 nγ = 1.614
birefringenceδ = 0.023
2VMeasured: 73° to 81°
references
::

| name = Bertrandite | image = Bertrandite-38545.jpg | alt = | caption = Bertrandite from the Golconda pegmatite, Minas Gerais, Brazil | category = Sorosilicate | formula = Be4Si2O7(OH)2 | IMAsymbol=Btd | strunz = 9.BD.05 | dana = | 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 {011} or {021} forming heart- or V-shaped twins | cleavage = Perfect on {001}; distinct on {100}, {010} and {110} | fracture = | tenacity = | mohs = 6–7 | luster = Vitreous, pearly on cleavage surfaces | streak = | diaphaneity = Transparent | gravity = 2.59–2.60 | density = | polish = | opticalprop = Biaxial (−) | refractive = nα = 1.591 nβ = 1.605 nγ = 1.614 | birefringence = δ = 0.023 | pleochroism = | 2V = Measured: 73° to 81° | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | references =

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.

It, with beryl, are ores of beryllium.

It was discovered near Nantes, France in 1883 and named after French mineralogist, Emile Bertrand (1844–1909).

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.

References

References

  1. Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
  2. [http://rruff.geo.arizona.edu/doclib/hom/bertrandite.pdf Handbook of Mineralogy]
  3. [http://www.mindat.org/min-642.html Bertrandite on Mindat.org]
  4. [http://webmineral.com/data/Bertrandite.shtml Bertrandite on Webmineral]
  5. (October 2016). "Beryllium—A Critical Mineral Commodity—Resources, Production, and Supply Chain". USGS.
  6. (1968). "Geology of the Spor mountain Beryllium District, Utah, in Ore deposits of the United States, 1933–1967". The American Institute of Mining, Metallurgical, and Petroleum engineers, Inc..

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