glaucodot

{{Infobox mineral | name = Glaucodot | category = Sulfide minerals | image = Glaucodot-169959.jpg | caption = Glaucodot from Håkansboda, Lindesberg, Sweden. Size: 3.3 x 2.7 x 2.6 cm. | formula = {{chem2|(Co_{0.75}Fe^{2+}_{0.25}AsS)}} | IMAsymbol = Gl | molweight = 165.15 g/mol | strunz = 2.EB.10c | system = Orthorhombic | class = Prismatic (2/m) (same H-M symbol) | symmetry = P21/c | color = Grayish tin white, Reddish silver white | habit = Massive, prismatic habits with elongated sphenoids, granular masses- Uniformly indistinguishable crystals forming large masses. | twinning = | cleavage = None | fracture = Brittle - Uneven - Very brittle fracture producing uneven fragments. | mohs = 5 | luster = Metallic | refractive = | fluorescence= inert | opticalprop = | birefringence = | pleochroism = | streak = black | gravity = 5.9–6.01, Average = 5.95 | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = Opaque | other = Nonmagnetic, non-radioactive }}

Glaucodot is a cobalt iron arsenic sulfide mineral with formula . The cobalt:iron(II) ratio is typically 3:1 with minor nickel substituting. It forms a series with arsenopyrite . It is an opaque grey to tin-white typically found as massive forms without external crystal form. It crystallizes in the orthorhombic system. The locality at Håkansboda, Sweden has rare twinned dipyramidal crystals (see photo). It is brittle with a Mohs hardness of 5 and a specific gravity of 5.95. It occurs in high temperature hydrothermal deposits with pyrrhotite and chalcopyrite. Glaucodot is classed as a sulfide in the arsenopyrite löllingite group.