falcondoite

Falcondoite, a member of the sepiolite group, was first discovered in the Dominican Republic, near the town of Bonao. The mineral was found in a deposit mined by Falconbridge Dominica, and so was named "falcondoite" after the company. Falcondoite is frequently associated with sepiolite, garnierite, talc, and serpentine, and is commonly nickel-bearing. While the chemical formula for falcondoite can vary, the mineral must contain more nickel than magnesium to be considered its own species. The ideal chemical formula for falcondoite is (Ni,Mg)4Si6O15(OH)2·6H2O.

== Occurrence == Falcondoite occurs in an extensive deposit of laterite near the town of Bonao in the Dominican Republic. This deposit is part of a serpentinized harzburgite massif, which is composed of limonitic and serpentinitic ore. It's found in whitish-green veins of garnierite that is rich in sepiolite material. These veins are often only millimeters to centimeters thick, and can be formed by the infill of tension fractures. Some commonly associated minerals include sepiolite, garnierite, talc, and serpentine. While falcondoite is most closely associated to sepiolite, it's characterized by containing more nickel.