extended abstracts - Geomorphic Processes and Geoarchaeology

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Geomorphic processes and geoarchaeology deposition is evidenced by lower accumulation terraces formed in the last centuries e.g. in the outlet of the Wisłoka river in the Carpathian margin [22] as well as in the Dniester valley in Kružyky site, where at the bottom of the 5-meter terrace oak trunk processed by man, dated at 400 ± 35 BP (1440-1620 cal AD) [15] were found. Progress of economic activity coincided with the beginning of the Little Ice Age. Increasing number of sites in river valleys indicates sequential occurrence of enhanced flood accumulation connected exclusively with human impact (e.g. Roman Period), phases conditioned exclusively by increase in precipitation in the periods of economical recession (5-6 th centuries) as well as phases of coincidence of both these factors (e.g. 11 century and Little Ice Age) [8, 23]. References 1. Wasylikowa K., Starkel L., Niedziałkowska E., Skiba S., Stworzewicz E. 1985. Environmental changes in the Vistula valley at Pleszów caused by Neolithic man. Przegląd Archeologiczny, Vol. 33, P. 19-55. 2. Starkel L., Czopek S., Madeja J., Budek A., Harmata K. 2002, Ewolucja środowiska a osadnictwo prehistoryczne na przedpolu brzegu Karpat w rejonie Sędziszowa i Rzeszowa. Materiały i Sprawozdania Rzeszowskiego Ośrodka Archeologicznego, Vol. 23, P. 5-30. 3. Kalicki, T. 1996. Phases of increased river activity during the last 3500 years. Geographical Studies, part VI, Special Issue No. 9, P. 94-101. 4. Starkel, L., Kalicki T., Krapiec, M., Soja, R., Gębica, P., Czyżowska, E. 1996. Hydrological changes of valley floors in the upper Vistula basin during Late Vistulian and Holocene. Geographical Studies, part VI, Special Issue No 9, P. 158 5. Kalicki, T., Krąpiec, M. 1991. Black oaks and Subatlantic alluvia of the Vistula in Branice-Stryjów near Cracow. Geographical Studies, part IV, Special Issue No. 6, P. 39-61. 6. Gębica, P., Krąpiec, M. 2009. Young Holocene alluvia and dendrochronology of subfossil trunks in the San river valley. Studia Geomorphologica Carpatho-Balcanica, Vol. 43, P. 63-75. 7. Krąpiec M. 1996. Dendrochronology of black oaks from river valleys in Southern Poland. Geographical Studies, part VI, Special Issue No. 9, P. 61-78. 8. Starkel, L. 2005. Role of climatic and anthropogenic factors accelerating soil erosion and fluvial activity in Central Europe. Studia Quaternaria, Vol. 22, P. 27-33. 9. Starkel, L., Krąpiec M. 1995. Profile of the alluvia with black oaks in Kędzierz on the Wisłoka river. Geographical Studies, part V, Special Issue No. 8, P. 101-110. 10. Starkel, L., Gębica, P., Budek, A., Krapiec, M., Jacyšyn, A., Kalinovyč, N. 2009. Evolution of the lower section of the Strvjaž river valley during the Holocene (piedmont of the Eastern Carpathians). Studia Geomorphologica Carpatho-Balcanica, Vol. 43, P. 5-37. 11. Havliček, P. 1991. The Morava River Basin during the last 15000 years. In: Starkel L., Gregory K.J. and Baker V. (Eds.), Temperate Palaeohydrology. P. 319-341. 12. Starkel, ed. 1981. The evolution of the Wisłoka valley near Dębica during the Late Glacial and Holocene. Folia Quaternaria, Vol. 53, 91 p. 13. Gębica, P. 2011. Stratigraphy of alluvial fills and phases of the Holocene floods in the lower Wisłok river valley, SE Poland. Geographia Polonica, Vol. 84, Special 265
Geomorphic processes and geoarchaeology Issue, part 1, P. 39-60. 14. Harmata, K., Kalinovyč, N. 2006. Phases of settlement in the pollen diagram. In: Harmata K., Machnik J. and Starkel L. (Eds.), Environment and man at the Carpathian foreland in the Upper Dnister catchment from Neolithic to Early Medieval period. Polska Akademia Umiejętności. Prace Komisji Prehistorii Karpat, Vol. 13, P. 70-77. 15. Gębica, P., Starkel, L., Jacyszyn, A., Krąpiec, M. (In print). Medieval accumulation in the Upper Dniester River Valley: the role of human impact and climate change in the Carpathian Foreland. Quaternary International. 16. Niedziałkowska, E., Gilot, E., Pazdur, M., Szczepanek, K. 1985. The evolution of the Upper Vistula valley in the region of Drogomyśl in the Upper Vistulian and Holocene. Folia Quaternaria, Vol. 56, P. 101-132. 17. Dotterweich, M. 2008. The history of soil erosion and fluvial deposits in small catchments of central Europe: Deciphering the long-term interaction between humans and the environment – A review. Geomorphology, Vol. 101, P. 192-208. 18. Alexandrowicz, S.W., Alexandrowicz, W.P., Krąpiec, M. 2005. Holocene terrace of the Velyky Lukavets River in Starunia: sediments and dendrochronology. In: Kotarba M. (Ed.). Polish and Ukrainian geological studies (2004-2005) at Starunia – the area of discoveries of wooly rhinoceroses. P. 95-102. 19. Chiriloaei, F., Radoane, M., Persoiu, I., Popa, I. 2011. Reconstruction of the fluvial activity in the last 3000 years for the Moldova River (Romania). Abstracts volume «Climate change in the Carpathian-Balkan Region during Late Pleistocene and Holocene». PAGES. University of Suceava, P. 35. 20. Starkel, L. 2001. Historia doliny Wisły od ostatniego zlodowacenia do dziś. In: (Sum. Evolution of the Vistula river valley since the Last Glaciation till present). Monografie 2. Instytut Geografii i Przestrzennego Zagospodarowania PAN, 263 p. 21. Kukulak, J. 2004. Zapis skutków osadnictwa i gospodarki rolnej w osadach rzeki górskiej (na przykładzie aluwiów dorzecza górnego Sanu w Bieszczadach Wysokich. In: (Sum: Record of human settlement and agriculture in mountain river sediments (based on the example of alluvia of Upper San catchment in Bieszczady Wysokie). Prace Monograficzne 381. 125 p. 22. Klimek, K. 1974. The structure and mode of sedimentation of the floodplain deposits in the Wisłoka valley (South Poland). Studia Geomorphologica Carpatho- Balcanica, Vol. 8, P. 137-151. 23. Starkel, L., Soja R., Michczyńska, D. 2006. Past hydrological events reflected in Holocene history of Polish rivers. Catena, Vol. 66, Is. 1-2, P. 24-33. LATE GLACIAL PALEOSOLS (MIS 2) OF THE GEOARCHEOLOGICAL MONUMENT «DIVNOGOR’E 9» Sycheva S.A. 1 , Bessudnov A.N. 2 1 Institute of Geograhpy, RAS, Moscow, Russia, sychevasa@mail.ru 2 Lipetsk Pedagogical University, Lipetsk, Russia, noo-archeolog@freemail.ru Soils of the late glacial period are locally distributed on the territory of the East- European Plain and are more often described around archeological monuments. Stratigraphic position, genesis and evolution of these soils are still not well known. 266
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