- Boehmite
Boehmite or Böhmite is an
aluminium oxide hydroxide (γ-AlO(OH)) mineral, a component of the aluminium orebauxite . It is dimorphous withdiaspore . It crystallizes in theorthorhombic dipyramidal system and is typically massive in habit. It is white with tints of yellow, green, brown or red due to impurities. It has a vitreous to pearly luster, aMohs hardness of 3 to 3.5 and aspecific gravity of 3.00 to 3.07. It is colorless in thin section, optically biaxial positive with refractive indices of nα = 1.644 - 1.648, nβ = 1.654 - 1.657 and nγ = 1.661 - 1.668.Boehmite occurs in tropical
laterite s and bauxites developed on alumino-silicate bedrock. It also occurs as ahydrothermal alteration product ofcorundum andnepheline .It was first described in 1927 and named for German geologist
Johann Böhm (1857–1938).References
* [http://rruff.geo.arizona.edu/doclib/hom/bohmite.pdf Mineral Data Pub. The University of Arizona]
* [http://webmineral.com/data/Boehmite.shtml Webmineral data]
* [http://www.mindat.org/min-707.html Mindat with location data]
* [http://www.uwgb.edu/DutchS/PETROLGY/LepidocrStruc.HTM Steven Dutch, 2002, Lepidocrocite and Boehmite Structure, University of Wisconsin - Green Bay]
Wikimedia Foundation. 2010.