Keywords
depositional mechanisms
palaeohydraulics
heavy minerals
sandur
Pleistocene
Poland
How to Cite
Abstract
During the Pleistocene the Scandinavian ice sheet drained huge quantities of sediment-laden meltwaters. These meltwaters supplied ice-marginal valleys that formed parallel to the front of the ice sheet. Not without significance was the supply of ice-marginal valleys from extraglacial rivers in the south. Moreover, periglacial conditions during and after sedimentation in ice-marginal valleys, the morphology of valley bedrocks, and erosion of older sediments played important roles in the depositional scenarios, and in the mineralogical composition of the sediments. The mechanisms that controlled the supply and deposition in ice-marginal valleys were analysed on the basis of a Pleistocene ice-marginal valley that was supplied by northern and southern source areas in the immediate vicinity. Investigations were conducted in one of the largest ice-marginal valleys of the Polish-German lowlands, i.e., the Toruń-Eberswalde ice-marginal valley, in sandurs (Drawa and Gwda) supplied sediments and waters from the north into this valley, and on extraglacial river terraces (pre-Noteć and pre-Warta rivers), formed simultaneously with the sandurs and ice-marginal valley (Pomeranian phase of Weichselian glaciation) supplied sediments and waters from the south into this valley. A much debated question is how similar, or different, depositional processes and sediments were that contributed to the formation of the Toruń-Eberswalde ice-marginal valley, and whether or not it is possible to differentiate mostly rapidly aggraded sandur sediments from ice-marginal valley sediments. Another question addresses the contribution of extraglacial feeding of the Toruń-Eberswalde ice-marginal valley. These matters were addressed by a wide range of analyses: sediment texture and structure, architectural elements of sediments, frequency of sedimentary successions, heavy-mineral analysis (both transparent and opaque heavy minerals), analysis of rounding and frosting of quartz grains, and palaeohydrological calculations. Additionally, a statistical analysis was used. The specific depositional conditions of distribution of sediments in ice-marginal valley allow to distinguish new environment of ice-marginal valley braided river. The spectrum of depositional conditions in the Toruń-Eberswalde ice-marginal valley and their specific palaeohydraulic parameters allow to distinguish three coexisting zones in the ice-marginal valley braided-river system: (1) deep gravel-bed braided channel zone with extensive scours, (2) deep sand-bed braided channel zone with transverse bars, and (3) marginal sand-bed and gravel-bed braided channel zone with diamicton and breccia deposition, which were characterised in detail. Some of the results have been published previously, which is why they are discussed in the present paper within the context of new data
References
Antczak, B., 1985. Rhythmites on the lower terraces of the Warta River (Poland) and their paleohydrologic implications. Quaestiones Geographicae 1, 31-43.
Antczak, B., 1986. Transformacja układu koryta i zanik bifurkacji Warty w Pradolinie Warszawsko-Berlińskiej i południowej części przełomu poznańskiego podczas późnego vistulianu [Transformation of the channel pattern and the disappearance of Warta bifurcation in Warsaw-Berlin pradolina and the southern part of the Poznań during the late Vistulian]. AMU Press, Geografia 35, 111 pp.
Antczak-Górka, B., 2005. Głazy rzeźbione przez wiatr jako wskaźniki różnowiekowych stref peryglacjalnych ostatniego zlodowacenia w Polsce Zachodniej [Wind-polished stones as indicators of last-glaciation periglacial zones of various ages in western Poland]. AMU Press, Poznań, 209 pp.
Ashley, G.M., 1975. Rhythmic sedimentation in glacial Lake Hitchcock, Massachusetts Connecticut. [In:] A.V. Jopling, B.V. McDonald (Eds): Glaciofluvial and Glaciolacustrine Sedimentation. Society of Economic Paleontologists and Mineralogists Special Paper 23, 304-320.
Ashworth, P. & Ferguson, R.I., 1986. Interrelationships of channel processes, changes and sediments in a proglacial braided river. Geografiska Annaler 68A, 361-371.
Bagnold, R.A., 1966. An approach to the sediment transport problem from general physics. [In:] C.R., Thorne, R.C., MacArthur & J.B., Bradley (Eds): The Physics of Sediment Transport by Wind and Water. American Society of Civil Engineers, New York, 231-291.
Baker, V.R., 1973. Paleohydrology and sedimentology of Lake Missoula flooding in eastern Washington. Geological Society of America, Special Paper 144, 73 pp.
Baker, V.R. & Costa, J.E., 1987. Flood Power. [In:] L. Mayer & D. Nash (Eds): Catastrophic Flooding, 1-21. Biddles, Guildford.
Bartczak, E., 2006. Objaśnienia do Szczegółowej Mapy Geologicznej w skali 1:50 000. Arkusz Piła [Explanations to the Detailed Geological Map of Poland 1:50 000, sheet Piła]. PGI Press, Warsaw.
Bjørnsson, H., 1998. Hydrological characteristics of the drainage system beneath a surging glacier. Nature 395, 771-774.
Blažauskas, N., Jurgaitis, A. & Šinkũnas, P., 2007. Patterns of Late Pleistocene proglacial fluvial sedimentation in the SE Lithuanian Plain. Sedimentary Geology 193, 193-201.
Boothroyd, J.C. & Ashley, G.M., 1975. Processes, bar morphology and sedimentary structures on braided outwash fans, northeastern Gulf of Alaska. [In:] A.V. Jopling & B.C. McDonald (Eds): Glaciofluvial and Glaciolacustrine Sedimentation. Society of Economic Paleontologists and Mineralogists Special Publication 23, 193-222.
Börner, A., 2007. Das Eberswalder Urstromtal - Untersuchung zur pleistozänen Landschaftsgenese zwischen Niederem Oderbruch und Werbellinseerinne (Nordost-Brandenburg) [The Eberswalde ice-marginal valley - investigation of the Pleistocene genesis of the landscape between Nieder Oderbruch and the tunnel valley of the Werbellinesee (Northeast Brandenburg)]. Schriftenreihe für Geowissenschaften 17, 118 pp.
Brandes, Ch., Winsemann, J., Roskosch, J., Meinsen, J., Tanner, D.C., Frechen, M., Steffen, H. & Wu, P., 2012. Activity along the Osning Thrust in Central Europe during the Lateglacial: ice-sheet and lithosphere interactions. Quaternary Science Reviews 38, 49-62.
Bridge, J.S., 2003. Rivers and Floodplains - Forms, Processes and Sedimentary Record. Blackwell, Bodmin, 491 pp.
Bridge, J.S. & Diemer, J.A., 2003. Quantitative interpretation of an evolving ancient river system. Sedimentology 30, 599-623.
Brodzikowski, K. & Van Loon, A.J., 1980. Sedimentary deformations in Saalian glaciolimnic deposits near Włostów (Żary area, western Poland). Geologie en Mijnbouw 59, 251-272.
Brodzikowski, K. & Van Loon, A.J., 1991. Glacigenic sediments. Developments in Sedimentology 49, Elsevier, Amsterdam, 674 pp.
Cant, D.J. & Walker, R.G., 1976. Development of a braided-fluvial facies model for the Devonian Battery Point Sandstone, Quebec. Canadian Journal of Earth Sciences 13, 102-119.
Carling, P.A., 1996. Morphology, sedimentology and palaeohydraulic significance of large gravel dunes: Altai Mountains, Siberia. Sedimentology 43, 647-664.
Church, M. & Gilbert, R., 1975. Proglacial fluvial and lacustrine sediments. [In:] A.V. Jopling & B. McDonald (Eds): Glaciofluvial and glaciolacustrine sedimentation. Society of Economic Paleontologists and Mineralogists Special Publication 23, 22-100.
Costard, F., Dupeyrat, L., Gautier, E. & Carey-Gailhardis, E., 2003. Fluvial thermal erosion investigations along a rapidly eroding river banks: application to the Lena river (central Siberia). Earth Surface Processes and Landforms 28, 1349-1359.
Fraser, J.Z., 1982. Derivation of a summary facies sequence based on Markov chain analysis of the Caledon outwash: a Pleistocene braided glacial fluvial deposit. [In:] R. Davidson-Arnott (Ed.): Research in Glacial, Glacio-fluvial, and Glacio-lacustrine Systems, Geo Books, Norwich, 175-202.
Friend, P.P. & Moody-Stuart, M., 1972. Sedimentation in the Wood Bay Formation (Devonian) of Spitsbergen: Regional analysis of a late erogenic basin. Norsk Polarinstitutt Skrifter 157, 1-77.
Gadomska, S., 1957. Utwory trzeciorzędowe i czwartorzedowe doliny Noteci w okolicy Krostkowa i Osieka n/Notecią koło Wyrzyska [Tertiary and quaternary sediments of Noteć Valley in the vicinity of Krostków and Osiek near Wyrzysk]. Biuletyn Instytutu Geologicznego 118, 371-393.
Galon, R., 1961. Morphology of the Noteć-Warta (or Toruń-Eberswalde) ice marginal streamway. Prace Geograficzne 29, 7-115. [In Polish; English summary].
Galon, R., 1968. New facts and problems pertaining to the origin of the Noteć-Warta Pradolina and the valleys linked with it. Przegląd Geograficzny 40, 307-315.
Gilbert, R., 1975. Sedimentation in Lillooet Lake, British Columbia. Canadian Journal of Earth Sciences 12, 1697-1711.
Goudie, A.S., 2004. Encyclopedia of Geomorphology. Vol. 1. International Association of Geomorphologists. Taylor and Francis, 1156 pp.
Hampel, A., Hetzel, R., Maniatis, G. & Karow, T., 2009. Three-dimensional numerical modeling of slip rate variations on normal and thrust fault arrays during ice cap growth and melting. Journal of Geophysical Research 114, 8406-8420.
Harbor, D.J., 1998. Dynamics of bedforms in the Lower Mississippi River. Journal of Sedimentary Research 68, 750-762.
Hasholt, B., 1995. Varves in a proglacial Lake, Semilik, South East Greenland. Danish Journal of Geography 95, 92-96.
Jahn, A., 1975. Problems of the Periglacial Zone. PWN Press. Warsaw, 223 pp.
Jaroszewski, W., Marks, L. & Radomski, A., 1985. Słownik geologii dynamicznej [Dictionary of dynamic geology]. Geological Press, Warsaw, 310 pp.
Kasse, C., 1997. Cold-climate aeolian sand-sheet formation in North-Western Europe (c. 14-12.4 ka); a response to permafrost degradation and increased aridity. Permafrost and Periglacial Processes 8, 295-311.
Karczewski, A.,1968. Wpływ recesji lobu Odry na powstanie i rozwój sieci dolinnej Pojezierza Myśliborskiego i Niziny Szczecińskiej [Influence of Odra Lobe recession on the Myślibórz Lakeland and Szczecin Lowland valleys development]. Prace Komisji Geograficzno-Geologicznej PTPN 8, 108 pp.
Kaufmann, G., Wu, P. & Ivins, E.R., 2005. Lateral viscosity variations beneath Antarctica and their implications on regional rebound motions and seismotectonics. Journal of Geodynamics 39, 165-181.
Kehew, A.E., Lord, M.L., Kozlowski, A. & Fisher, T.G., 2009. Proglacial megaflooding along the margins of the Laurentide Ice Sheet. [In:] D.M. Burr, P.A. Caring & V.R. Baker (Eds): Megaflooding on Earth and Mars, 104-127. Cambridge University Press, Cambridge.
Klimek, K., 1972. Współczesne procesy fluwialne i rzeźba równiny Skeidararsandur (Islandia) [Fluvial processes and morphology of the Skeidararsandur (Iceland)]. Prace Geograficzne IGiPZ PAN, 94 pp.
Komar, P.D., 1989. Physical processes of waves and currents and the formation of marine placers. CRC Critical Reviews in Aquatic Sciences 1, 393-423.
Komar, P.D., 2007. The entrainment, transport and sorting of heavy minerals by waves and currents. [In:] M.A. Mange & D.T. Wright (Eds): Heavy Minerals in Use. Developments in Sedimentology 58, 3-48. Elsevier, Amsterdam.
Kondracki, J., 2000. Geografia regionalna Polski [Regional geography of Poland]. PWN Press, Warsaw, 441 pp.
Kozarski, S., 1959. O genezie O genezie chodzieskiej moreny czołowej [On the origin of the Chodzież end moraine]. Badania Fizjograficzne nad Polską Zachodnią 5, 45-72. [In Polish; English summary].
Kozarski, S., 1962. Recesja ostatniego lądolodu z północnej części Wysoczyzny Gnieźnieńskiej a kształtowanie się Pradoliny Noteci-Warty [Problem of the recession of the last ice-sheet from the northern part of the Gniezno Plateau and Noteć-Warta ice-marginal valley development]. Prace Komisji Geograficzno-Geologicznej 2, Poznań, 145 pp.
Kozarski, S., 1965. Zagadnienie drogi odpływu wód pradolinnych z zachodniej części Pradoliny Noteci-Warty [The problem of the outflow from the western part of Noteć-Warta Pradolina]. Prace Komisji Geograficzno- Geologicznej 5, 1-87.
Kozarski, S., 1966. Die glazialen Abflußverhältnisse im westlischen Teil des Noteć-Warta Urstromtales. Wissenschaftliche Zeitschrift der Ernst-Moritz-Arndt-Universität Greifswald 15, 63-72.
Kozarski, S., 1986. Skale czasu a rytm zdarzeń zdarzeń geomorfologicznych vistulianu na Niżu Polskim [Time scales and rhythm of geomorphological events during Vistulian in the Polish Lowlands]. Czasopismo Geograficzne 57, 247-270.
Krausse, K., 1996. Windkanter - interessante Geschiebe Norddeutschlands. Geschiebekunde Aktuell 12, 105-110.
Krüger, J., 1997. Development of minor outwash fans at Kötulujökull, Iceland. Quaternary Science Reviews 16, 649-659.
Lewin, J. & Gibbard, P.L., 2010. Quaternary river terraces in England: forms, sediments and processes. Geomorphology 120, 293-311.
Liedtke, H., 1961. Die Talentwicklung im Oderbruch und im unteren Odertal. Die Zeitschrift der Gesellschaft für Erdkunde zu Berlin 92, 259-280.
Lindé, K. & Mycielska-Dowgiałło, E., 1980. Some experimentally produced microtextures on grain surfaces of quartz sand. Geografiska Annaler 62A, 171-184.
Lindner, L., 1992. Czwartorzęd - osady, metody badań, stratygrafia [The Quaternary - deposits, research methods, stratigraphy]. PAE Press, Warsaw, 683 pp.
Liszkowski, J., 1992. Wpływ plejstoceńskich lądolodów na stan, strukturę, kinematykę i dynamikę ziemi [Impact of the Pleistocene ice sheets structure, kinematics and dynamics of the earth]. [In:] Materiały VII Sympozjum Glacitektonicznego [Proceedings of Glacitectonics Symposium], Zielona Góra, 217-253. Liszkowski, J., 1993. The effects of Pleistocene ice-sheet loading-deloading cycles on the bedrocks structure of Poland. Folia Quaternaria 64, 7-23.
Lord, M.L. & Kehew, A.E., 1987. Sedimentology and paleohydrology of glacial-lake outburst deposits in southeastern Saskatchewan and nothwestern North Dakota. Geological Society of America Bulletin 99, 663-673.
Louis, H., 1936. Neuere Forschungen über die Urstromtäler besonders im mittleren Norddeutschland. Comptes Rendus du Congrès international de Géographie, Warsaw 1934, 335-341.
Lowright, R., Williams, E.G. & Dachille, F., 1972. An analysis of factors controlling deviations in hydraulic equivalence in some modern sands. Journal of Sedimentary Petrology 42, 635-645.
Lüthgens, C., Böse, M. & Preusser, F., 2011. Age of the Pomeranian ice-marginal position in northeastern Germany determined by Optically Stimulated Luminescence (OSL) dating of glaciofluvial sediments. Boreas 40, 598-615.
Maas, G., 1904. Zur Entwicklungsgeschichte des sog. Thorn-Eberswalde Haupttales. Zeitschrift der Deutschen Geologischen Gesellschaft 56, 40-49.
Mange, M.A. & Maurer, H.F.W., 1992. Heavy minerals in colour. Chapman and Hall, London, 147 pp.
Maizels, J., 1993. Lithofacies variations within sandur deposits: the role of runoff regime, flow dynamics and sediment supply characteristic. Sedimentary Geology 85, 299-325.
Maizels, J.K., 1995. Sediments and landforms of modern proglacial terrestrial environments. [In:] Menzies, J. (Ed.), Modern Glacial Environments. Butterworth-Heinemann, Oxford, pp. 365- 416.
Marcinkowski, B., 2007. Wykorzystanie składu mineralnego i morfologii ziaren minerałów ciężkich do określania środowiska sedymentacyjnego [Application of the mineral composition and the morphology of mineral grains to the interpretation of the sedimentary environment]. Przegląd Geologiczny 55, 207.
Marks, L., 2012. Timing of the Late Vistulian (Weichselian) glacial phases in Poland. Quaternary Science Reviews 44, 81-88.
Marren, P.M., 2005. Magnitude and frequency in proglacial rivers: a geomorphological and sedimentological perspective. Earth-Science Reviews 70, 203-251.
Marren, P.M., Russell, A.J. & Knudsen, O., 2002. Discharge magnitude and frequency as a control on proglacial fluvial sedimentary systems. [In:] F.J. Dyer, M.C. Thoms & J.M. Olley (Eds): The Structure, Function and Management Implications of Fluvial Sedimentary Systems, 297-303. IAHS Publication 276.
Miall, A.D., 1977. A review of the braided-river depositional environment. Earth-Science Reviews 13, 1-62.
Miall, A.D., 1978. Lithofacies types and vertical profile models in braided river deposits: a summary. [In:] A.D. Miall (Ed.): Fluvial Sedimentology. Canadian Society of Petroleum Geologists 5, 597-604.
Miall, A.D., 2006. The Geology of Fluvial Deposits: Sedimentary Facies, Basin Analysis and Petroleum Geology. Springer, 582 pp.
Migoń, P., 2006. Geomorfologia [Geomorphology]. PWN Press. Warsaw, 464 pp.
Mizerski, W. & Sylwestrzak, H., 2002. Słownik geologiczny [Geological dictionary]. PWN Press, Warsaw, 80 pp.
Mörner, N.A., 1990. Glacioisostatic and long term crustal movements in Fennoscandia with respect to lithospheric and atmospheric processes and properties. Tectonophysics 176, 13-24.
Muir-Wood, R., 2000. Deglaciation seismotectonics: a principal influence on intraplate seismogenesis at high latitudes? Quaternary Science Reviews 19, 1399-1411.
Murton, J.B., 1996. Near-surface brecciation of chalk, Isle of Thanet, South-East England: a comparison with ice-rich brecciated bedrocks in Canada and Spitsbergen. Permafrost and Periglacial Processes 7, 153-164.
Murton, J.B. & Belshaw, R.K., 2011. A conceptual model of valley incision, planation and terrace formation during cold and arid permafrost conditions of Pleistocene southern England. Quaternary Research 75, 385-394.
Mycielska-Dowgiałło, E., 1993. Estimates of Late Glacial and Holocene aeolian activity in Belgium, Poland and Sweden. Boreas 22, 165-170.
Mycielska-Dowgiałło, E., 2001. Wpływ warunków klimatycznych na cechy strukturalne i tekstualne osadów mineralnych [The influence of climatic conditions on structural and textual features of deposits]. [In:] A. Karczewski & Z. Zwoliński (Eds): Funkcjonowanie geosystemów w zróżnicowanych warunkach morfoklimatycznych - monitoring, ochrona, edukacja [The functioning of geosystems under different morphoclimatic conditions - monitoring, protection, education]. Poznań, 377-394.
Mycielska-Dowgiałło, E. & Woronko, B., 1998. Analiza obtoczenia i zmatowienia powierzchni ziarn kwarcowych frakcji piaszczystej i jej wartość interpretacyjna [Rounding and frosting analysis of quartz sandgrain surfaces and their interpretative significance].
Przegląd Geologiczny 46, 1275-1281. Niewiarowski W., 1969. The relation of the Drwęca valley to the Noteć-Warta (Toruń-Eberswalde) Pradolina and its role in the glacial and lateglacial drainage system. Geographica Polonica 17, 173-188.
Niewiarowski, W., 1983. Postglacjalne ruch pionowe skorupy ziemskiej na Pojezierzu Krajeńskim w świetle badań geomorfologicznych. Przegląd Geograficzny 55, 13-31.
Ost, H.G., 1932. Morphologischen Studien im Drage- und Küddowgebiet. Abhandlung und Berichte der Naturwissenschaftlichen Abteilung der Grenzmarkischen Gesellschaft zur Erforschung und Pflege 7, 3-68.
Ost, H.G., 1935. Neuere Anschauungen zur Entwicklungsgeschichte eines norddeutschen Urstromtales. Zeitschrift für Gletscherkunde 22, 96-108.
Passchier, S., 2007. The Use of Heavy Minerals in the Reconstruction of Ice-Sheet Drainage Patterns: An Example from the Edge of the East Antarctic Ice Sheet. [In:] M.A. Mange & D.T. Wright (Eds): Heavy minerals in use. Developments in Sedimentology 58, 677-700. Elsevier, Amsterdam. Paterson, W.S.B., 1994. Hydraulics of glaciers. Glaciers sliding. Deformation of subglacial till. Structures and fabric in glaciers and ice sheet. [In:] W.S.B. Paterson (Ed.): The Physics of Glaciers, 103-203. Pergamon Press, Oxford.
Pisarska-Jamroży, M., 2006. Transitional deposits between endmoraine and sandur plain in the Pomeranian glaciomarginal zone of NW Poland: a missing component of ice-contact sedimentary models. Boreas 35, 126-141.
Pisarska-Jamroży, M., 2007. Glacifluwialne facje strumieni przeciążonych zawiesiną na przykładzie plejstoceńskich osadów wschodniej Jutlandii i Pomorza Zachodniego [Glaciofluvial facies of hyperconcentrated flow (Pleistocene of Denmark and Western Pomerania)]. Przegląd Geologiczny 55, 503-510.
Pisarska-Jamroży, M., 2008a. Zonation of glaciomarginal environment inferred from Pleistocene deposits of Myślibórz Lakeland, NW Poland. Geografiska Annaler 90A, 237-249.
Pisarska-Jamroży, M., 2008b. Mechanizmy depozycji w strefie glacimarginalnej zlodowacenia Wisły. Studium sedymentologiczne z Pomorza Zachodniego i Jutlandii [Depositional mechanisms in glaciomarginal zone of the Vistulian glaciation. Sedimentological study of Western Pomerania and Jutland]. Kazimierz Wielki University Press, Bydgoszcz, 163 pp.
Pisarska-Jamroży, M., 2013. Varves and megavarves of the Eberswalde Valley (NE Germany) - a key for the interpretation of glaciolimnic processes. Sedimentary Geology 291, 84-96.
Pisarska-Jamroży, M. & Weckwerth, P., 2013. Soft-sediment deformation structures in a Pleistocene glaciolacustrine delta and their implications for the recognition of subenvironments in delta deposits. Sedimentology 60, 637-665.
Pisarska-Jamroży, M. & Zieliński, T., 2011. Genesis of a till/sand breccia (Pleistocene, Noteć Valley near Atanazyn, central Poland). Sedimentary Geology 236, 109-116.
Pisarska-Jamroży, M. & Zieliński, T., 2012. Specific erosional and depositional processes in a Pleistocene subglacial tunnel in the Wielkopolska region, Poland. Geografiska Annaler 94A, 429-443.
Pisarska-Jamroży, M. & Zieliński, T., 2014. Pleistocene sandur rhythms, cycles and megacycles: Interpretation of depositional scenarios and palaeoenvironmental conditions. Boreas 43, 330-348.
Pisarska-Jamroży, M., Van Loon, A.J., Woronko, B. & Sternal, B., in press a. Heavy-mineral analysis as a tool to trace the source areas of sediments in an ice-marginal valley, with an example from the Pleistocene in northwest Poland. Netherlands Journal of Geosciences. doi: https://www.doi.org/10.1017/njg.2014.37
Pisarska-Jamroży, M., Van Loon, A.J. & Woronko, B., in press b. Sorting of heavy minerals in sediments deposited at a high accumulation rate, with examples from sandurs and an ice-marginal valley in NW Poland. GFF. doi: https://www.doi.org/10.1080/11035897.2015.1009158.
Plink-Björklund, P. & Ronnert, L., 1999. Depositional processes and internal architecture of Late Weichselian ice-margin submarine fan and delta settings, Swedish west coast. Sedimentology 46, 215-234.
Racinowski, R. & Rzechowski, J., 1969. Minerały ciężkie w glinach zwałowych Polski środkowej [Heavy minerals in the tills of middle Poland]. Geological Quarterly 13, 479-490.
Randriamazaoro, R., Dupeyrat, L., Costard, F. & Gailhardis, E.C., 2007. Fluvial thermal erosion: heat balance integral method. Earth Surface Processes and Landforms 32, 1828-1840.
Russell, A.J., 2005. Catastrophic floods. [In:] C.S. Richard, L.R.M. Cocks & I.R. Plimer (Eds): Encyclopedia of Geology, Elsevier, Amsterdam, 628-641.
Russell, A.J. & Marren, P.M., 1999. Proglacial fluvial sedimentary sequences in Greenland and Iceland: a case study from active proglacial environments subject to jökulhlaups. Skeiðararsandur, Iceland. Global and Planetary Change 28, 203-226.
Saunderson, H.C. & Jopling, A.V., 1980. Palaeohydraulics of a tabular cross-stratified sand in the Brampton esker, Ontario. Sedimentary Geology 25, 169-188.
Schlaak, N., 1993. Studie zur Landschaftsgenese im Raum Nordbarnim und Eberswalder Urstromtal. Berliner Geographische Arbeiten 76, 119 pp.
Siegenthaler, Ch. & Huggenberger, P., 1993. Pleistocene Rhine gravel: deposits of a braided river system with dominant pool preservation. [In:] J.L. Best & C.S. Bristow (Eds): Braided Rivers. Geological Society Special Publication 75, 147-162.
Snorrason, Á., Jónsson, P., Sigurdsson, O., Pálsson, S., Árnason, S., Víikingsson, S. & Kaldal, I., 2002. November 1996 jökulhlaup on Skeiðararsandur outwash plain, Iceland. International Association of Sedimentologists, Special Publication 32, 55-65.
Soons, J.M.,1964. Ice-marginal Drainage Channels in the Rakaia Valley. New Zealander Geographer 20, 153-164.
Stankowski, W., 1963a. Deflation relief of the western part of the Warta-Noteć Interfluve. INQUA, Report of the 6th International Congress on Quaternary, Warsaw, 337-339.
Stankowski, W., 1963b. Rzeźba eoliczna Polski Północno-Zachodniej na podstawie wybranych obszarów [Aeolian relief of NW Poland on the base of selected sites]. Prace Komisji Geograficzno-Geologicznej 4, 147 pp.
Steidtmann, J.R., 1982. Size-density sorting of sand-size spheres during deposition from bedload transport and implications concerning hydraulic equivalence. Sedimentology 29, 877-883.
Szupryczyński, J., 1958. Rzeźba i budowa geologiczna Dębowej Góry. Studia Societatis Scientiarium Torunensis 3, 1-13. Tomczak, A., 1987. Evolution of the Vistula valley in the Toruń Basin in the Late Glacial and Holocene. [In:] L. Starkel (Ed.): Evolution of the Vistula river valley during the last 15 000 years, 207-232. Geographical Studies, Special Issue 4, Toruń.
Toucanne, S., Zaragosi, S., Bourillet, J.F., Cremer, M., Eynaud, F., Turon, J.L., Fontanier, C, Van Vliet Lanoë, B. & Gibbard, P.L., 2009a. Timing of massive ‘Fleuve Ukraine. Quaternary International. doi: https://www.doi.org/10.1016/j. quaint.2014.08.013.
Zieliński, T., 1993. Sandry Polski północno-wschodniej - osady i warunki sedymentacji. [Sandurs of NE Poland - sediments and depositional conditions]. Silesian University Press, Katowice, 96 pp. [In Polish; English summary].
Zieliński, T., 2007. The Pleistocene climate-controlled fluvial sedimentary record in the Belchatow mine (central Poland). Sedimentary Geology 193, 203-209.
Zieliński, T., 2014. Sedymentologia. Osady rzek i jezior [Sedimentology. Deposits of rivers and lakes]. Adam Mickiewicz University Press, Poznań, 594 pp.
Zieliński, T. & Pisarska-Jamroży, M., 2012. Jakie cechy litologiczne warto kodować, a jakie nie? [Which features of deposits should be included in a code and which not?]. Przegląd Geologiczny 60, 387-397.
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