STIBICONITE
Class : Oxides and hydroxides
Subclass : Oxides
Crystal system : Cubic
Chemistry : Sb3O6(OH)
Rarity : Fairly common
Stibiconite is the most common oxidation mineral of primary antimony minerals, particularly stibnite. It is therefore found in the superficial parts of antimony deposits, very often associated with other secondary antimony minerals, particularly kermesite; it makes up most of the "antimony ochres", a generic term for secondary antimony minerals with a yellowish tint. Its name comes from the Latin stibium (antimony) and the Greek konis (powder), thus emphasizing the often powdery appearance of the mineral and its chemical composition. Stibiconite most commonly occurs in masses and coatings of earthy appearance of yellow to yellowish white color, covering the surface of primary antimony minerals, sometimes completely replacing them (pseudomorph). It is an ancillary ore of antimony.
Main photo : Stibiconite pseudomorph after stibnite from Catorce, San Luis Potosi, Mexico © Connor Williams
Stibiconite in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 5.5 to 7
Density : 3.3 to 5.5
Fracture : Undetermined
Streak : White to yellow
TP : Translucent to transparent
RI : -
Birefringence : 0
Optical character : None
Pleochroism : None
Fluorescence : None
Solubility : Acids
Magnetism : NoneRadioactivity : None