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210 Pb dating of young holocene sediments in High-mountains lakes of the Tatra Mountains

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Topmost sediments in two oligotrophic lakes of the High Tatra Mountains were studied in terms of sedimentological characteristics and 210 Pb dating. An alpine lake sediments are important source of information on geomorphic process activity in glacial catchments. Two different sediment transfer models are represented. In Morskie Oko lake basin majority of extreme, short lasting geomorphic events triggered on the surrounding slopes are registred in lake sediments (minerogenic laminae), while in Zelene Pleso lake only an effect of pro-longed flooding periods are to be seen. The sedimentation rates in both lakes are similar.
Wydawca
Czasopismo
Rocznik
Tom
Strony
73--77
Opis fizyczny
Bibliogr. 10 poz., rys.
Twórcy
autor
  • Department of Geomorphology and Hydrology, Institute of Geography and Spatial Organisation, Polish Academy of Sciences, św. Jana 22, 31-018 Cracow, Poland
autor
  • The Henryk Niewodniczański Institute of Nuclear Physics, Radzikowskiego 152, 31-342 Cracow, Poland
autor
  • Faculty of Physics and Nuclear Techniques, University of Mining and Metallurgy, Mickiewicza 30, 30-059 Cracow, Poland
Bibliografia
  • 1. Baumgart-Kotarba M., Kotarba A. and Wachniew P., 1993: Young Holocene lacustrine sediments of the Morskie Oko Lake in the High Tatra and their dating by use 210Pb and 14C radioisotopes. Dokumentacja Geograficzna IG i PZ PAN, Z Badañ FizycznoGeograficznych w Tatrach 4-5: 45-61 (in Polish).
  • 2. Flynn W. W., 1968: The determination of low-levels of polonium-210 in environmental materials. Analytica Chemica Acta 43: 221-227.
  • 3. Caine N., 1974: The geomorphic processes of the alpine environment. In: Arctic and Alpine Environments. London: 721- 741.
  • 4. Goldberg E. D., 1963: Radioactive dating. IAEA Symp.: 121-131.
  • 5. Kotarba A., 1995: Rapid mass wasting over the last 500 years in the High Tatra Mountains. Questiones Geographicae, Special Issue 4: 177-183.
  • 6. Larsen E., and Magnerud J., 1981: Erosion rate of a Younger Dryas cirque glacier at Kråkenes, Western Norway. Annals of Glaciology 2: 153-158.
  • 7. Oldfield F. and Appleby P. G., 1984: Empirical testing of 210Pb dating models for lake sediments. In: Haworth E. Y. and Lund J. W. G., eds., Lake sediments and Environmental History. Leic. Univ. Press, Leicester: 93-124.
  • 8. Owens P. and Slaymaker O., 1993: Lacustrine Sediment Budget in the Coast Mountains of British Columbia, Canada. In: McManus J. and Duck R..W.,eds., Geomorphology and Sedimentology of Lakes and Reservoirs. J.Wiley & Sons Ltd: 105-123.
  • 9. Preiss N., Melieres M. A. and Pourchet M., 1996: A compilation of data on lead 210 concentration in surface air and fluxes at the air-surface and water-sediment interfaces. Journal of Geophysical Research 101: 28,874-28,862.
  • 10. Wolman M. G. and Miller J. P., 1960: Magnitude and forces in geomorphic processes. Journal of Geology. 68: 54-74.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BAT3-0007-0018
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