Stibnite
Stibnite
Socialist Union of Popular Forces
Stibnite [image] General Category Mineral Chemical formula Antimony Sulfide (Sb2S3) Identification Colour Steel gray to dull gray. Black iridiscent Tarnish may be present. Crystal habit Massive, radiationg and elongated crystals. Massive and granular. Crystal system Orthorhombic Cleavage Perfect Fracture Small-scale subconchoidal Mohs Scale hardness 2 Luster Splendent on fresh crystals surfaces, otherwise metallic Refractive index Opaque Pleochroism N/A Streak Similar to colour Specific gravity 4.56 - 4.62 Fusibility ? Solubility Souluble in Hydrochloric acid Major varieties Metastibnite Earthy, reddish deposits
Stibnite is the most important source for the rare Metal Antimony. It is soluble in Hydrochloric acid, and is tarnished by potassium hydroxide solution.
Small deposits of Stibnite are common, large ones are rare. It occurs in Canada, Mexico, Peru, Japan, China, Germany, Romania, Italy, France, England, Algeria, and Kalimantan, Borneo. In the United States it is found in Arkansas, Idaho, Nevada, California, and Alaska.
Spectacular, large iridescent stibnite crystals are found in Japan.