Roman slag from the archaeological site near Mo{nje (NW Slovenia) was studied with respect to its mineralogical and geochemical characteristics. Samples were analysed with light microscopy, X-ray powder diffraction (XRD), scanning electron microscopy with an energy dispersive spectrometer (SEM-EDS) and Raman microspectroscopy. A chemical investigation was carried out using inductively coupled plasma-atomic emission spectroscopy (ICP-ES) to determine the major elements. The investigated slags are recognized as iron slags, grouped into two main classes according to their chemical and mineralogical compositions. The first group is characterized by high Fe2O3 and low SiO2 contents and the second by high CaO and SiO2 and low Fe2O3 contents. The phase occurrence obviously depends on the chemical composition as the first group mainly consists of fayalite, wüstite and magnetite, and the second one of augite, leucite, hedenbergite, monticellite and kirschsteinite. Keywords: slag, archaeometallurgy, iron slag, Roman slag, archaeological site near Mo{nje (Slovenia) V prispevku je obravnavana rimska`lindra z arheolo{kega najdi{~a Mo{nje (SZ Slovenija), pri kateri smo dolo~ili mineralno in kemijsko sestavo. Vzorci so bili analizirani s svetlobno mikroskopijo, rentgensko pra{kovno difrakcijo, SEM-EDS in ramansko mikrospektroskopijo. Kemijska sestava glavnih elementov je bila dolo~ena z ICP-ES. Preiskana`lindra dokazuje, da izvira iz pridelave`eleza na tem podro~ju. Glede na mineralo{ko in kemijsko sestavo lahko delimo`lindro na dve skupini. Za prvo skupino je zna~ilna visoka vsebnost Fe2O3 in nizka vsebnost SiO2, za drugo pa visoki vsebnosti SiO2 in CaO ter nizka vsebnost Fe2O3. Kemijska sestava vpliva na mineralne faze; tako je za prvo skupino zna~ilen fajalit, wustit in magnetit, za drugo pa avgit, levcit, hedenbergit, monticelit in kirschsteinit.