Age of the Vistula River overbank deposits in Toruń

• Autorzy: Szmańda J. B. , Oczkowski H. L. , Przegiętka K. R.
• Języki publikacji: EN

Abstrakty

EN

The paper presents luminescence dates of the overbank deposits accumulated on the Bazarowa Holm in Toruń. From these results we conclude that the flood deposits accumulation was started in this part of the Vistula river valley between 1000 and 2000 years ago. Deforestation and following increase of the floods. events intensity, which occurred in early Middle Ages, may be the possible reasons for the aggradation phase on the flood plane.

Słowa kluczowe

EN

luminescence dating; overbank deposits; fluvial procceses; flood plane

• Wydawca: De Gruyter
• Czasopismo: Geochronometria
• Rocznik: 2004
• Tom: Vol. 23
• Strony: 35--38
• Opis fizyczny: Bibliogr. 9 poz., rys., tab.

Twórcy

autor

Szmańda J. B.

• Institute of Geography, Nicolaus Copernicus University, Fredry 6/8, 87-100 Toruń, Poland

autor

Oczkowski H. L.

• Institute of Physics, Nicolaus Copernicus University, Grudziądzka 5/7, 87-100 Toruń, Poland

autor

Przegiętka K. R.

• Institute of Physics, Nicolaus Copernicus University, Grudziądzka 5/7, 87-100 Toruń, Poland

Bibliografia

• 1. Chruścińska A., Lankauf K.R., Luc M., Oczkowski H.L., Przegiętka K.R. and Szmańda J.B., 2004: Evolution of St. Laurent Mountain near Chełmno based on luminescence dating. Geochronometria (this volume).
• 2. Kalicki T., 1996: Overbank deposits as indicators of the change in discharges and supply of sediments in the upper Vistula valley. In: Starkel L. and Kalicki T., eds., Ewolution of Vistula river valley during the last 15,000 years 6, Geographical Studies Special Issue 9: 43-61.
• 3. Myślińska E., Hoffman E., and Kulesza-Wiewióra K., 1982: Zróżnicowanie geologiczne mad w wybranych odcinkach doliny Wisły, (Geological differentiation of mada in selected fragments of the Lower Vistula valley). Przegląd Geologiczny 9: 474-479 (in Polish).
• 4. Oczkowski H.L. and Przegiętka K.R., 1998: TL Dating of Young Aeolian Deposits from Kępa Kujawska. Radiation Measurements 29: 435-439.
• 5. Oczkowski H.L., Przegiętka K.R., Lankauf K.R. and Szmańda J.B., 2000: Gamma spectrometry in thermoluminescence dating. Geochronometria 18: 57-66.
• 6. Tomczak A., 1971: Kępa Bazarowa na Wiśle w Toruniu w świetle badań geomorfologicznych oraz archiwalnych materiałów kartograficznych (Kępa Bazarowa in Toruń, in the light of geomorphological research and archival cartographical materials). Studia Societatis Scientiarum Torunensis 7 (6): 1-111. (in Polish).
• 7. Tomczak A., 1982: The evolution of the Vistula river valley between Toruń and Solec Kujawski during the Late Glacial and Holocene. In: Starkel L., ed., Evolution of the Vistula river valley during the last 15 000 years. Geographical Studies Special Issue1: 108-129.
• 8. Tomczak A., 1987: Evolution of the Vistula valley in the Toruń Basin in the Late Glacial and Holocene, In: Starkel L. ed., Evolution of the Vistula river valley during the last 15 000 years. Geographical Studies Special Issue 4: 207-232.
• 9. Wallinga J., 2002: Detection of OSL age overestimation using singlealiquot techniques. Geochronometria 21: 17-26.