Goethite-coated eluvial (?) and fresh-looking (alluvial ?) Pt-Fe nuggets from Joubdo stream, Birbir River are very variable in external morphology from rounded, flattened to very irregular with sharp projections. Scanning electron microscopy has revealed crystalline details of the Pt-Fe alloys at magnifications not reported previously. The most common Pt-Fe alloy is Pt₃Fe, probably isoferroplatinum, but tulameenite and tetraferroplatinum are also present. A combined electron probe and quantitative optical study has documented an extensive suite of primary inclusions in Pt-Fe alloy matrix : osmium, irarsite, erlichmanite, genkinite (second world occurrence), hollingworthite, laurite, stibiopalladinite, cuprian gold, bornite, chalcopyrite, cubanite, chromite, magnetite, diopside (?), ferroaugite (?), forsterite (?), rhodian « pentlandite » (?), unnamed RhSbS (Raicevic and Cabri, 1976), and unnamed Rh₂S₃ (Begizov et al., 1975). In addition, unnamed minerals reported for the first time include : Pt(Rh, Ir)CuS₄, Rh(Te, Bi)₂, and unidentified anisotropic Fe — Rh — Ni and Fe — Ni — Ir — Rh sulphides. Genkinite and osmium are the only platinum-group minerals exhibiting alteration to secondary minerals, the latter to an unidentified iridium-rich alteration product.