STILPNOMELANE
Class : Silicates
Subclass : Phyllosilicates
Crystal system : Triclinic
Chemistry : K(Fe,Mg)8(Si,Al)12(O,OH)27
Rarity : Fairly common
Stilpnomelane is a mica that is found mainly in sedimentary iron deposits, associated with magnetite, goethite, hematite and pyrite. It is also known as a common constituent of weakly metamorphic rocks (chlorite schists, epidote schists), more rarely of glaucophane schists and of certain metamorphic metal deposits (Franklin in New Jersey and Nordmark in Sweden for example). Its name comes from the Greek stilpnos (brilliant) and melanos (black), thus evoking its luster and its color. Stilpnomelane occurs in lamellae or scales, in foliated masses, in fibrous, downy or radiate aggregates, not exceeding 1 cm, or in velvety coatings. Its color is reddish brown to black, golden brown or green-black with easy foliated cleavage. When the lamellae are thin, the resemblance to biotite is strong.
Main photo : Stilpnomelane from Les Moulins Mine, Valais, Switzerland © Mischa Crumbach
Stilpnomelane in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 3 to 4
Density : 2.59 to 2.96
Fracture : Micaceous
Streak : White, gray
TP : Translucent
RI : 1.543 to 1.745
Birefringence : 0.033 to 0.111
Optical character : Biaxial -
Pleochroism : Visible
Fluorescence : None
Solubility : Sulfuric acid
Magnetism : NoneRadioactivity : None