[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.]Search in Google Scholar
[Cant, D.J., 1978. Bedforms and bar types in the South Saskatchewan River. Journal of Sedimentary Petrology 48, 1321-1330.10.1306/212F7676-2B24-11D7-8648000102C1865D]Search in Google Scholar
[Cant, D.J. & Walker, R.G., 1978. Fluvial processes and facies sequences in the sandy braided South Saskatchewan River, Canada. Sedimentology 25, 625-648.10.1111/j.1365-3091.1978.tb00323.x]Search in Google Scholar
[Dade, W.B., 2000. Grain size, sediment transport and alluvial channel pattern. Geomorphology 35, 119-126.10.1016/S0169-555X(00)00030-1]Search in Google Scholar
[Dade, W.B. & Friend, P.F., 1998. Grain size, sediment-transport regime and channel slope in alluvial rivers. Journal of Geology 106, 661-675.10.1086/516052]Search in Google Scholar
[Frings, R.M., 2008. Downstream fining in large sand-bed rivers. Earth-Science Reviews 87, 39-60.10.1016/j.earscirev.2007.10.001]Search in Google Scholar
[Galon, R., 1961. Morphology of the Noteć-Warta (or Toruń-Eberswalde) ice marginal streamway. Prace Geograficzne IGiPZ PAN 29, 129 pp.]Search in Google Scholar
[Henderson, F.M., 1961. Stability of alluvial channels. Journal of the Hydraulics Division 87, 109-138.10.1061/JYCEAJ.0000653]Search in Google Scholar
[Julien, P.Y. & Raslan, Y., 1998. Upper-regime plane bed. Journal of Hydraulic Engineering 124, 1086-1096.10.1061/(ASCE)0733-9429(1998)124:11(1086)]Search in Google Scholar
[Julien, P.Y. & Wargadalam, J., 1995. Alluvial channel geometry: theory and applications. Journal of Hydraulic Engineering 121, 312-325.10.1061/(ASCE)0733-9429(1995)121:4(312)]Search in Google Scholar
[Komar, P.D., 1987. Selective grain entrainment by a current from a bed of mixed sizes: a reanalysis. Journal of Sedimentary Petrology 57, 203-211.10.1306/212F8AE4-2B24-11D7-8648000102C1865D]Search in Google Scholar
[Leclair, S.Z. & Bridge, J.S., 2001. Quantitative interpretation of sedimentary structures formed by river dunes. Journal of Sedimentary Research 71, 713-716.10.1306/2DC40962-0E47-11D7-8643000102C1865D]Search in Google Scholar
[Lee, J.S. & Julien, P.Y., 2006. Downstream hydraulic geometry of alluvial channels. Journal of Hydraulic Engineering 132, 1347-1352.10.1061/(ASCE)0733-9429(2006)132:12(1347)]Search in Google Scholar
[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.]Search in Google Scholar
[Mackin, J.H., 1948. Concept of the graded river. Geological Society of America Bulletin 59, 463-512.10.1130/0016-7606(1948)59[463:COTGR]2.0.CO;2]Search in Google Scholar
[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.]Search in Google Scholar
[Miall, A.D., 1985. Architectural-element analysis: a new method of facies analysis applied to fluvial deposits. Earth-Science Reviews 22, 261-308.10.1016/0012-8252(85)90001-7]Search in Google Scholar
[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, 1787-1803.10.1130/0016-7606(2000)112<1787:IAPFAA>2.0.CO;2]Search in Google Scholar
[Mojski, J.E., 1980. Budowa geologiczna i tendencje rozwoju doliny Wisły [Geological structure and development tendency of the Vistula valley]. Przegląd Geologiczny 6, 332-334.]Search in Google Scholar
[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.]Search in Google Scholar
[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.]Search in Google Scholar
[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.]Search in Google Scholar
[Paola, C., 2000. Quantitative models of filling. Sedimentology 47, 121-178.10.1046/j.1365-3091.2000.00006.x]Search in Google Scholar
[Paola, C. & Borgman, L., 1991. Reconstructing random topography from preserved stratification. Sedimentology 38, 553-565.10.1111/j.1365-3091.1991.tb01008.x]Search in Google Scholar
[Paola, C., Heller, P.L. & Angevine, C.L., 1992. The largescale dynamics of grain-size variation in alluvial basins, 1: Theory. Basin Research 4, 73-90.10.1111/j.1365-2117.1992.tb00145.x]Search in Google Scholar
[Paola, C. & Mohrig, D., 1996. Palaeohydraulics revisited: palaeoslope estimation in coarse-grained braided rivers. Basin Research 8, 243-254.10.1046/j.1365-2117.1996.00253.x]Search in Google Scholar
[Parker, G., 1976. On the cause and characteristic scales of meandering and braiding. Journal of Fluid Mechanics 76, 457-480.10.1017/S0022112076000748]Search in Google Scholar
[Prent, M. & Hickin, E.J., 2001. Annual regime of bedforms, roughness and flow-resistance, Lillooet River, British Columbia. Geomorphology 41, 369-390.10.1016/S0169-555X(01)00068-X]Search in Google Scholar
[Sauderson, H.C. & Jopling, A.V., 1980. Palaeohydraulics of a tabular, cross-stratified sand in the Brampton Esker, Ontario. Sedimentary Geology 25, 169-188.10.1016/0037-0738(80)90039-1]Search in Google Scholar
[Schumm, S.A., 1977. The fluvial system. John Wiley & Sons, New York, 338 pp.]Search in Google Scholar
[Simons, D.B. & Richardson, E.V., 1962. Resistance to flow in alluvial channels. Transactions of the American Society of Civil Engineers 127, 927-954.10.1061/TACEAT.0008468]Search in Google Scholar
[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.]Search in Google Scholar
[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.]Search in Google Scholar
[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.]Search in Google Scholar
[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.]Search in Google Scholar
[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.]Search in Google Scholar
[Weckwerth, P., 2010. Evolution of the Toruń Basin in the Late Weichselian. Landform Analysis 14, 57-84.]Search in Google Scholar
[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, 397-412.10.2478/s13386-011-0038-1]Search in Google Scholar
[Williams, G.P., 1971. Flood deposits of the sand-bed ephemeral streams of central Australia. Sedimentology 17, 1-40.10.1111/j.1365-3091.1971.tb01128.x]Search in Google Scholar
[Williams, G.P., 1983. Paleohydrological methods and some examples from Swedish fluvial environments. I. Cobble and boulder deposits. Geografiska Annaler 65A, 227-243.10.1080/04353676.1983.11880088]Search in Google Scholar
[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.]Search in Google Scholar
[Zieliński, T., 1992. Proglacial valley facies of the Silesian Upland - genetic factors and their sedimentological effects. Geologia Sudetica 26, 83-118.]Search in Google Scholar
[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.]Search in Google Scholar
[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.]Search in Google Scholar
[Zieliński, T. & Van Loon, A.J., 2003. Pleistocene sandur deposits represent braidplains, not alluvial fans. Boreas 32, 590-611.10.1080/03009480310004170]Search in Google Scholar