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1

THE UPPER PALEOLITHIC SITE AT UJAZD (POLISH CARPATHIANS)

100%
Valde-Nowak P., Lanczont M., Pawlowska M.
Acta Archaeologica Carpathica
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2005
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vol. 40
5-26
EN
The site No. 6 in Ujazd, distr. Jaslo is situated on a narrow and flat, secondary, sub-parallel ridge with a nose protruding towards the Wisloka River valley. In summer 2005 archaeological excavations took place there. The discovered inventory, . Upper Palaeolithic in the character, is not large. Most of artefacts were found in the secondary position. Two pieces only (flakes) were recognised as finds in the loess-like sediments, which could be identified as a rest of cultural level. However, importance of this discovery cannot be ignored. In the whole Polish Carpathians the Upper Palaeolithic sites are extremely rare. According to the TL dating, the Ujazd site could be situated in the settlement horizon direct after LGM represented by Epigravettian sites at Cosautsi, layer V and IV, and Molodova V, layer 14. This assemblage confirm from the one side some elements typical for the Danube Epigravettian, and some implements more characteristic for the Molodova culture from the other.
2

SITE 25 OF THE CEMETERY AT PRUSIEK, GMINA SANOK, PODKARPACKIE VOIVODESHIP. A NOTE ON THE MIGRATION OF THE PRZEWORSK CULTURE POPULATION INTO THE AREA OF THE POLISH CARPATHIAN MOUNTAINS IN THE EARLY ROMAN PERIOD

88%
Madyda-Legutko R., Pohorska-Kleja E., Rodzinska-Nowak J.
Acta Archaeologica Carpathica
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2005
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vol. 40
115-128
EN
The area of the Polish Carpathians has so far produced no sepulchral finds of the Przeworsk culture which could be dated without any doubt to the Roman period. Site 25 in the cemetery at Prusiek, gmina Sanok, is the first discovery of this kind in the area. The four cremation urn graves found there belong to Phase B2/C1 and C1a of the Roman Period. Their inventory shows direct indebtedness to the eastern zone of the Przeworsk culture. In effect, the find in the Prusiek cemetery can be taken as a clear proof of the expansion of the Przeworsk culture bearers in the direction of the Upper Tisa basin.
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