GEOCHEMICAL PROSPECTING AT MT. PROSARA AND MOTAJICA, NORTHERN BOSNIA: EXAMINING POTENTIAL SITES OF BRONZE AGE PLACER TIN ORE MINING
To test the hypothesis that these sites may be tin-bearing, geochemical prospecting was conducted on coarse sediments from streams flowing from the major drainages of these mountains. Cassiterite (SnO2) is hard (Mohs hardness 6-7), dense (6.9 g/cm³), and stable under surface conditions, and so accumulates as placer deposits. Accordingly, sediments were collected from sand/gravel bars, sieved, sluiced, and panned on site to prepare a rough heavy mineral separate. The heavy mineral fraction of each sample was then further concentrated in the lab using sodium polytungstate heavy liquid (2.94 g/ml). The mineral magnetite was magnetically extracted and the heavy sediments were sorted according to grain size fractions: very coarse sand (>850μ), coarse sand (850-420μ), and fine sediments (<420μ). The chemical composition of these heavy mineral separates were analyzed using an Olympus Innov-X X-ray fluorescence (XRF) hand apparatus with a tin detection limit of approximately 150 ppm.
The XRF analysis indicated high concentrations (> 1%) of elements common to heavy mineral sands (Fe, Ti, Mn, Ca, and K). However, no tin was identified. Thus, it is highly unlikely that northern Bosnia supplied tin ore for bronze production in prehistory. Further separation, such as magnetic susceptibility, and an SEM-EDS analysis is underway to verify the absence of tin in the samples and to further characterize the heavy mineral assemblages in the major streams of Prosara and Motajica.