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Elham Ghasidian
New research on the Middle and Upper Paleolithic of the Kermanshah Province: West Central
Zagros Mountains; Iran
During November and December 2010, in line with the Paleolithic investigations in Zagros Mountains of
Iran, a Paleolithic survey, funded by Hugo Obermaier Society for Quaternary Research and Archaeology of
the Stone Age and the Institut für Ur- und Frühgeschichte, Universität Tübingen, was conducted among the
six districts within the Kermanshah Province including Kermanshah, Eslamabad, Dalahoo, Sarpol-e Zahab,
Gilan-e Gharb and Qasr-e Shirin. These areas cover large and various ecological regions from the eastern
hilly lands of the Mesopotamian Plain to the Zagros highlands in the west central Zagros Mountains. This
extensive survey and a test excavation at Kermanshah lead to the high volume of archaeological evidences
on the Paleolithic occupation in this region. This project aims to study the mobility strategies and settlement
dynamics of the hunter gatherers societies during the upper Pleistocene period in Kermanshah Region.
Institut für Ur-und Frühgeschichte und Archäologie des Mittelalters; Abteilung Ältere Urgeschichte und
Quartärökologie Schloss Hohentübingen D-72070 Tübingen.
Marc Händel, Thomas Einwögerer, Roswitha Thomas
Periglacial processes and the formation of the Gravettian nd horizons at Krems-Wachtberg
Most well-known Palaeolithic open-air sites in Austria are located on slopes of terraces, hills, and promon-
tories formed by loess sediments. Slope dynamics and loess sedimentation, together with a number of
other periglacial processes, are responsible both for the conservation and the dislocation and often enough
destruction – of archaeological ndings. In the case of the Gravettian site of Krems-Wachtberg in Eastern
Austria, where eld work has been conducted by the Prehistoric Commission of the Austrian Academy of
Sciences since 2005, the state of preservation ranges from primary deposits including in-situ occupation
surfaces with undisturbed evident features to a great variety of carefully documented secondary deposits.
The disintegration and dislocation of the primary contexts can therefore be modelled and connected to the
determining periglacial processes. Furthermore, this model helps to assess the manifold implications of
grand-scale dislocations of Palaeolithic deposits.
The research was funded by the Austrian Science Fund (FWF): P-17258, P-19347, P21660 and P-23612
(project management: Christine Neugebauer-Maresch).
References:
Einwögerer, T., Händel, M, Neugebauer-Maresch, C., Simon, U., Steier, P., Teschler-Nicola, M., Wild, E.M.
2009:
14
C Dating of the Upper Paleolithic site at Krems-Wachtberg, Austria. Radiocarbon, Vol 51,
Nr 2, p 847-855.
Händel, M., Simon, U., Einwögerer, T., Neugebauer-Maresch, C. 2008: Loess deposits and the conservation of
the archaeological record – The Krems-Wachtberg example. Quaternary International 198, p 46-50.
Händel, M, Simon, U., Einwögerer, T., Neugebauer-Maresch, C. 2009: New excavations at Krems-Wachtberg
approaching a well-preserved Gravettian settlement site in the middle Danube region. Quartär 56,
p 187-196.
Marc Händel, Prähistorische Kommission, Österreichische Akademie der Wissenschaften, Fleischmarkt 22,
A-1010 Wien
Christian Hoyer, Harald Floss
The formation of the gravettian open-air site Azé-Camping de Rizerolles (Saône-et-Loire, France)
The open-air site Azé-Camping de Rizerolles (Saône-et-Loire, France) was excavated under the direction of
Harald Floss, University of Tübingen, between 1998 and 2004. Its lithic assemblage is composed of ap-
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