Boracite

Boracite describes both a mineral group as well as an individual mineral within that group. The Boracite group is a solid solution series of chloro-borates, with Boracite, Chambersite, and Ericaite, as the main members. Boracite is the magnesium-rich end member, and the most prevalent mineral of this group.

Boracite is known for its equidimensional crystals, which may form in unique habits not seen elsewhere in the mineral kingdom. Up until recently, Boracite crystals were generally isolated small crystals, but a find in the Boulby Mine in England has produced large crystal groups much different then previous discoveries of this mineral. Boracite is named after its membership within the borate group, containing the element boron in its chemical composition.

A classic locality for Boracite crystals, in green and grayish-green equidimensional crystals, is the potash deposits of Bernburg and Stassfurt in Saxony-Anhalt, Germany. Single floater crystals, in dodecahedral or modified cubic form, have come from  from Lüneburger, Niedersachsen (Lower Saxony), Germany. Transparent green Boracite crystals, mostly in tetrahedral form, have come from the Glückauf Mine, Sondershausen, Thuringia, Germany.

A more recent find of Boracite is at the Boulby Mine, Loftus, North Yorkshire, England. This locality has produced sea-green crystals, in large clusters many times larger than all previous finds of this mineral. Another recent and important producer of Boracite is Alto Chapare, Cochabamba Department, Bolivia. Crystals from this mine are in cubic form with poor transparency, and usually in matrix. The color ranges from grayish-green to a less common peachy pink.