The third and final season of excavation on Pod Hradem Cave (Moravian Karst) reached bedrock at a maximum depth of 3.5 metres, although the bedrock in this part of the cave represents a very steeply sloping wall rather than the cave floor. Radiocarbon dates indicate that the basal layers in this part of the cave were deposited during the late Middle Palaeolithic period. The finding of amber and shell in layer 11 represents a curious discovery, but there is a possibility that these objects represent an intrusion from a different archaeological context., Ladislav Nejman, Lukáš Kučera, Petr Škrdla, Lenka Lisá, Šárka Hladilová, Miroslav Králík, Rachel Wood, Miriam Nývltová Fišáková, Duncan Wright, Marjorie E. Sullivan, Philip Hughes., 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
Ořechov IV is a recently investigated Bohunician site located in southern Moravia, but outside the Brno Basin where most of the other known Bohunician sites are located. It appears to belong to the pure Bohunician industry with no bifacial technology detected. It was probably discovered in the 1930s and due to later errors in reporting its exact location, it was ‘saved’ from prospecting by amateur archaeologists for several decades. We have re-located this site in 2010 and have conducted numerous pedestrian surveys and subsurface testing. We have collected a total of 3214 artifacts (most of them recorded by GPS) and a small amount of ochre. Two-thirds of the artifacts were manufactured on Stránská Skála chert. The second most common raw material used was Krumlovský Les chert followed by very small numbers of other raw materials including erratic flint, a long-distance import. Up to 20 % of the artifacts were damaged by frost action and agricultural activities. Numerous Levallois points and evidence for bidirectional flaking support the Bohunician classification. Test pitting has confirmed the presence of undisturbed sediments with cultural material including 4 structured hearths. Results of radiocarbon dating of some of these hearths are consistent with Bohunician antiquity. Only one lithic artifact in association with a hearth was found insitu. It is likely that future subsurface testing will yield more artifacts., Petr Škrdla, Tereza Rychtaříková, Ladislav Nejman, Jaroslav Bartík, Alena Hrušková, Jan Krása., and Obsahuje seznam literatury