A second occurrence of the Cu–Pb–Bi sulfosalt larosite, ideally (Cu,Ag)21PbBiS13, is described from Cu–Ag vein mineralization associated with an amphibolite dyke at Tinnsjå, southern Norway. The host assemblage consists of bornite – chalcocite – magnetite – wittichenite (± chalcopyrite, digenite, stromeyerite) and closely resembles that from the type locality Larosite crystals present an acicular morphology (<100 μm in length, <10 μm in width). An electron-microprobe analysis gives the mean empirical formula Cu20.47Ag3.68Fe0.22Pb1.01Bi1.06S15.00 calculated on the basis of 15 S atoms.