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Stibnite is an antimony sulphide mineral with a hardness of 2. Its crystal system is orthorhombic, and it often forms as long prismatic crystals with longitudinal striations. It also occurs in massive, granular or bladed forms. The color is metallic gray and tarnishes to black. Stibnite is formed from deposits from hot mineral springs or in low-temperature hydrothermal veins. The largest deposits of stibnite are in hunan province in china and other localities producing well-formed crystals include baia Sprie, Romania, and Shikoku Island.