PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Palaeoslopes of Weichselian sand-bed braided rivers in the Toruń Basin (Poland): results of a palaeohydraulic analysis

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Palaeoslopes of Weichselian sand-bed braided rivers have been reconstructed for two stages of fluvial development in the Toruń Basin. (1) The palaeoslope of the ‘fossil’ fluvial succession (buried under Weichselian tills) was calculated on the basis of the median grain size and the Shields parameter. The hydraulic gradient thus found is comparable with the hydraulic gradient of the present-day river. (2) The second developmental stage of the Toruń Basin (as a apart of the Noteć-Warta ice-marginal valley) took place after deglaciation. The slopes of river terraces are a few times lower than those calculated on the basis of the Shields parameter. The palaeoslope of the then river was estimated on the basis of a constant interdependency between the braidplain width, the channel geometry and the grain size. The river gradient that was thus calculated is similar to the measured terrace slope. Palaeoslope estimates in valleys similar to those in the Toruń Basin should consider the width of the braidplain.
Czasopismo
Rocznik
Strony
227--238
Opis fizyczny
Bibliogr. 45 poz.
Twórcy
  • Institute of Geography, Nicolas Copernicus University, ul. Gagarina 9, 87-100 Toruń
Bibliografia
  • Ashley, G.M., 1978. Bedforms in the Pitt River, British Columbia. [In:] A.D. Miall (Ed.): Fluvial sedimentology. Canadian Society of Petroleum Geology, Calgary, 88-104.
  • Cant, D.J., 1978. Bedforms and bar types in the South Saskatchewan River. Journal of Sedimentary Petrology 48, 1321-1330.
  • Cant, D.J. & Walker, R.G., 1978. Fluvial processes and facies sequences in the sandy braided South Saskatchewan River, Canada. Sedimentology 25, 625-648.
  • Dade, W.B., 2000. Grain size, sediment transport and alluvial channel pattern. Geomorphology 35, 119-126.
  • Dade, W.B. & Friend, P.F., 1998. Grain size, sediment-transport regime and channel slope in alluvial rivers. Journal of Geology 106, 661-675.
  • Frings, R.M., 2008. Downstream fining in large sand-bed rivers. Earth-Science Reviews 87, 39-60.
  • Galon, R., 1961. Morphology of the Noteć-Warta (or Toruń-Eberswalde) ice marginal streamway. Prace Geograficzne IGiPZ PAN 29, 129 pp.
  • Henderson, F.M., 1961. Stability of alluvial channels. Journal of the Hydraulics Division 87, 109-138.
  • Julien, P.Y. & Raslan, Y., 1998. Upper-regime plane bed. Journal of Hydraulic Engineering 124, 1086-1096.
  • Julien, P.Y. & Wargadalam, J., 1995. Alluvial channel geometry: theory and applications. Journal of Hydraulic Engineering 121, 312-325.
  • Komar, P.D., 1987. Selective grain entrainment by a current from a bed of mixed sizes: a reanalysis. Journal of Sedimentary Petrology 57, 203-211.
  • Leclair, S.Z. & Bridge, J.S., 2001. Quantitative interpretation of sedimentary structures formed by river dunes. Journal of Sedimentary Research 71, 713-716.
  • Lee, J.S. & Julien, P.Y., 2006. Downstream hydraulic geometry of alluvial channels. Journal of Hydraulic Engineering 132, 1347-1352.
  • Leopold, L.B., Wolman, M.G. & Miller J.P., 1964. Fluvial processes in geomorphology. W. H. Freeman and Company, San Francisco and London, 522 pp.
  • Mackin, J.H., 1948. Concept of the graded river. Geological Society of America Bulletin 59, 463-512.
  • Maizels, J.K., 1983. Palaeovelocity and palaeodischarge determination for coarse gravel deposits. [In:] K.J. Gregory (Ed.): Background to palaeohydrology. John Wiley & Sons, New York, 101-139.
  • Miall, A.D., 1985. Architectural-element analysis: a new method of facies analysis applied to fluvial deposits. Earth-Science Reviews 22, 261-308.
  • Mohrig, D., Heller, P.L., Paola, C. & Lyons, W.J., 2000. Interpreting avulsion from ancient alluvial sequences: Guadalope-Matarranya system (northern Spain) and Wasatch Formation (western Colorado). Geological Society of America Bulletin 112, 1787-1803.
  • Mojski, J.E., 1980. Budowa geologiczna i tendencje roz-rozwoju doliny Wisły [Geological structure and development tendency of the Vistula valley]. Przegląd Geologiczny 6, 332-334.
  • Mojski, J.E., 1995. An outline of the evolution of the Southern Baltic area at the end of the last glaciation and the beginning of Holocene. Biuletyn Peryglacjalny 34, 167-176.
  • Niewiarowski, W. & Tomczak, A., 1969. Morfologia i rozwój rzeźby obszaru miasta Torunia i jego okolic [Morphology and relief development of the town area and vicinity of Toruń]. Zeszyty Naukowe UMK, Geografia 6, 39-89.
  • Niewiarowski, W. & Weckwerth, P., 2006. Geneza i rozwój rzeźby terenu [Genesis and relief development]. [In:] L. Andrzejewski, P. Weckwerth & S. Burak (Eds): Toruń i jego okolice, monografia przyrodnicza [Toruń and its surroundings, natural monograph]. UMK, Toruń, 65-98.
  • Paola, C., 2000. Quantitative models of filling. Sedimentology 47, 121-178.
  • Paola, C. & Borgman, L., 1991. Reconstructing random topography from preserved stratification. Sedimentology 38, 553-565.
  • Paola, C., Heller, P.L. & Angevine, C.L., 1992. The largescale dynamics of grain-size variation in alluvial basins, 1: Theory. Basin Research 4, 73-90.
  • Paola, C. & Mohrig, D., 1996. Palaeohydraulics revisited: palaeoslope estimation in coarse-grained braided rivers. Basin Research 8, 243-254.
  • Parker, G., 1976. On the cause and characteristic scales of meandering and braiding. Journal of Fluid Mechanics 76, 457-480.
  • Prent, M. & Hickin, E.J., 2001. Annual regime of bedforms, roughness and flow-resistance, Lillooet River, British Columbia. Geomorphology 41, 369-390.
  • Sauderson, H.C. & Jopling, A.V., 1980. Palaeohydraulics of a tabular, cross-stratified sand in the Brampton Esker, Ontario. Sedimentary Geology 25, 169-188.
  • Schumm, S.A., 1977. The fluvial system. John Wiley & Sons, New York, 338 pp.
  • Simons, D.B. & Richardson, E.V., 1962. Resistance to flow in alluvial channels. Transactions of the American Society of Civil Engineers 127, 927-954.
  • Starkel, L., 2001. Historia doliny Wisły od ostatniego zlodowacenia do dziś [Evolution of the Vistula river valley since the last glaciation till present]. Monografie 2, Polish Academy of Sciences, Warszawa, 263 pp.
  • Weckwerth, P, 2007. Późnovistuliański rozwój sieci rzecznej w rejonie Kotliny Toruńskiej na tle struktur starszego podłoża [Development of rivers network in the Late Vistulian period in the Toruń Basin region on the background of older bottom tectonic structures]. Słupskie Prace Geograficzne 4, 143-156.
  • Weckwerth, P., 2004. Morfogeneza wybranych obszarów Kotliny Toruńskiej a problem jej roli w układzie hydrograficznym podczas górnego plenivistulianu [Morphogenesis of some areas in the Toruń Basin and their role in the hydrographic network during the late Plenivistulian]. Ph.D. thesis Toruń University, 168 pp.
  • Weckwerth, P., 2006. Problem bifurkacji Wisły pod Fordonem (Bydgoszcz) na tle ewolucji Kotliny Toruńskiej pod koniec plenivistulianu [The problem of bifurcation flow of the Vistula River at Fordon (Bydgoszcz) on the background of the Toruń Basin evolution in the end of Plenivistulian]. Przegląd Geograficzny 78, 47-68.
  • Weckwerth, P., 2009. Środowisko depozycji fluwialnej w stadiale głównym zlodowacenia Wisły - stanowisko Nowe Dąbie, południowo-zachodnia część Kotliny Toruńskiej [Fluvial depositional environment of the Main Stadial of the Weichselian Glaciation - Nowe Dąbie pit, SW part of Toruń Basin]. [In:] M. Pisarska-Jamroży & Z. Babiński (Eds): Plejstoceńskie środowiska sedymentacyjne Pojezierza Pomorskiego [Pleistocene sedimentary environments of the Pomeranian Lake District]. Wydawnictwo UKW, Bydgoszcz, 90-99.
  • Weckwerth, P., 2010. Evolution of the Toruń Basin in the Late Weichselian. Landform Analysis 14, 57-84.
  • Weckwerth, P., Przegiętka, K., Chruścińska, A., Woronko, B. & Oczkowski, H.L., 2011. Age and sedimentological features of fluvial series in the Toruń Basin and the Drwęca Valley (Poland). Geochronometria 38, 397-412.
  • Williams, G.P., 1971. Flood deposits of the sand-bed ephemeral streams of central Australia. Sedimentology 17, 1-40.
  • Williams, G.P., 1983. Paleohydrological methods and some examples from Swedish fluvial environments. I. Cobble and boulder deposits. Geografiska Annaler 65A, 227-243.
  • Wysota, W., 2002. Stratygrafia i środowiska sedymentacji zlodowacenia Wisły w południowej części dolnego Powiśla [Stratigraphy and sedimentary environments of the Weichselian glaciation in the southern part of the Lower Vistula region]. Nicolas Copernicus University, Toruń, 144 pp.
  • Zieliński, T., 1992. Proglacial valley facies of the Silesian Upland - genetic factors and their sedimentological effects. Geologia Sudetica 26, 83-118.
  • Zieliński, T., 1993. Sandry Polski północno-wschodniej - osady i warunki sedymentacji [Outwash plains of NE Poland - sediments and depositional processes]. Silesian University, Katowice, 96 pp.
  • Zieliński, T, 1998. Litofacjalna identyfikacja osadów rzecznych [Lithofacial identification of alluvial sediments]. [In:] E. Mycielska-Dowgiałło (Ed.): Struktury sedymentacyjne i postsedymentacyjne w osadach czwartorzędowych i ich wartość interpretacyjna [Sedimentary and postsedimentary structures in Quaternary sediments and their value for interpretation]. Warsaw University Press, Warszawa, 195-257.
  • Zieliński, T. & Van Loon, A.J., 2003. Pleistocene sandur deposits represent braidplains, not alluvial fans. Boreas 32, 590-611.
Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-deb2cace-5b4a-479c-988d-10167bd3f1b0
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.