The site of Mohelno-Plevovce is situated below the water line of the Mohelno water reservoir (lower part of the Dalešice pumped-storage hydroelectric power plant). The site was repeatedly occupied during the Late Upper Paleolithic. We discovered three areas with in-situ artifacts within intact sediments. While two assemblages excavated so far in Artifact Cluster 3 are characterized by microlithic tools made on carenoidal blanks and utilization of local rocks, both assemblages in Artifact Clusters 1 and 2 differ significantly from Artifact Cluster 3 and represent different techno-complexes. Artifact Clusters 1 and 2 are characterized by prevailing erratic flint supplemented by several artifacts made on radiolarite and obsidian. Technology is characterized by long, narrow and straight blades and bladelets removed from bidirectional cores. The collection of tools is characterized by prevailing backed microblades, in several cases with a straight truncation. In one case the truncations form a rectangle. This techno-complex continuing the Gravettian technological tradition is similar to material from Brno-Štýřice that is currently dated to the large time span covering two millennia between 17 100 and 19 100 calBP., Petr Škrdla, Jaroslav Bartík, Jan Eigner, Tereza Rychtaříková., and Obsahuje seznam literatury
Mohelno-Plevovce was repeatedly occupied during the Late Upper Paleolithic. Two paved stone structures constructed from local stones have been excavated thus far. These structures are characterized by a high density of lithic artifacts within the paved area and a rapidly decreasing density away from the paved area - this is interpreted as a result of the "barrier-effect" of the covered area. The lithic tools are characterized by abundant splintered pieces, steeply retouched end scrapers, and tiny microlithic tools produced on carenoidal blanks. Utilized raw material types indicate good knowledge of local rocks including rock crystal and weathering products of serpentinite, as well as broad raw material networks including erratic flint imported from northern Moravia and Szentgál radiolarite imported from Balaton Lake area., Petr Škrdla, Jaroslav Bartík, Jan Eigner, Tereza Rychtaříková, Pavel Nikolajev, Miriam Nývltová Fišáková, Ladislav nejman, Michaela Polanská, Jan Novák., and Obsahuje bibliografické odkazy