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Morphodynamics of small high-mountain wadis in arid zones (on the examples of the tributaries of the upper Dades River, High Atlas Mountains, Morocco)

Treść / Zawartość
Identyfikatory
Warianty tytułu
Konferencja
International Association of Geomorphologists/Association Internationale des Géomorphologues' (IAG/AIG) International Conference on Geomorphology „Geomorphology and Sustainability”(8, 27-31.08.2013, Paris, France)
Języki publikacji
EN
Abstrakty
EN
The paper reports on a study of the impact of morphology and lithology of small catchments on episodic river channel development in the southern High Atlas Mountains in Morocco. A detailed analysis focused on three catchments of small wadis featuring different relief and lithology along the upper, middle and lower course of the Dades River. The fieldwork combined with an analysis of topographic and geological maps and of satellite images concluded that the development of the river valley and channel structures was related to the main stages in the development of the landform in this part of the High Atlas. The channel dynamics were found to be typical of arid mountains, which was particularly apparent within a denudational-and-fluvial zone that reached up to 3,000 m a.s.l. The dominant morphodynamic system of this zone was pluvio-gravitational where episodic heavy rainfall events triggered fast displacement of stone mantle covers down the slopes and into the river channels. An analysis of the deposition zones in the lower channel reaches and on alluvial fans at the confluence of the side valleys and the main valley leads to the conclusion that the main factor, which determines the channel morphology is the impact of debris flows and heavily loaded streams and rivers. The deposited material is then transported outside the mountain zone and deposited within broad river channels. The development of the river channels in the three catchments depends on their order, morphometric property, slope lithology and the amount of material received from the slopes.
Czasopismo
Rocznik
Tom
Strony
9--19
Opis fizyczny
Bibliogr. 20 poz., rys.
Twórcy
  • Department of Geomorphology, Faculty of Geography and Regional Studies, University of Warsaw, Poland
autor
  • Department of Geomorphology, Institute of Geography and Spatial Management, Jagiellonian University, Cracow, Poland
autor
  • Department of Geomorphology, Faculty of Geography and Regional Studies, University of Warsaw, Poland
autor
  • Department of Geomorphology, Faculty of Geography and Regional Studies, University of Warsaw, Poland
  • Department of Geomorphology, Faculty of Geography and Regional Studies, University of Warsaw, Poland
Bibliografia
  • Brzezińska-Wójcik T., Tsermegas I., 2006. Geologiczne uwarunkowania rozwoju rzeźby Atlasu Wysokiego na przykładzie wąwozu Ziz. In: M. Dłużewski, I. Tsermegas (eds.), Geograficzne i geologiczne uwarunkowania rozwoju rzeźby Maroka. Materiały Warsztatów Geomorfologicznych, Maroko, 19.04–4.05.2006. SGP, WGiSR UW: 217–227.
  • Cooke R.U., Warren A., Goudie A.S., 1993. Desert Geomorphology. University College London Press, London.
  • Dainelli P., 2007. Geological Map of Boumalne 1:50 000. Ministere de L’Energie et des Mines, Direction du Developement Minier, S.E.L.C.A. – Florence, Italie.
  • de Jong C., Cappy S., Finckh M., Funk D., 2008. A transdisciplinary analysis of water problems in the mountainous karst areas of Morocco. Engineering Geology 99: 228–238.
  • de Jong C., Machauer R., Leavesely G., Cappy S., Poete P., Schulz O., 2005. Integrated hydrological modelling concepts for a peripheral mountainous semi-arid basin in southern Morocco. In: R. Escadafal, M.L. Paracchini (eds.), Geomatics for Land and Water Management: Achievements and Challenges in the Euromed Context. EC JRC Workshop proceedings: 219–227.
  • Frizon de Lamotte D., Saint Bezar B., Bracène R., Mercier E., 2000. The two main steps of the Atlas building and geodynamics of the western Mediterranean. Tectonics 19: 740–761.http://dx.doi.org/10.1029/2000TC900003
  • Graf W.L., 1988. Fluvial Processes in Dryland Riviers. Springer-Verlag, Berlin.http://dx.doi.org/10.1007/978-3-642-83048-8
  • Kotarba A., 1998. Landscape Ecology, Human Impact and Extreme Erosional Events in the Tatra Mountains. Poland. Ambio 27, 4: 354–357.
  • Kühle M., 1987. Physisch-geographische Merkmale des Hochgebirges: Zur Ökologie von Höhenstufen und Höhengrenzen. In: Hochgebirge. Ergebnisse neuer Forschungen. Forderfurter Beiträge zur Didaktik der Geographie 10, Forderfurt am Main: 15–40.
  • Laouina A., 2006. Zarys morfostrukturalny i geomorfologiczny Maroka. In: M. Dłużewski, I. Tsermegas (eds.), Geograficzne i geologiczne uwarunkowania rozwoju rzeźby Maroka. Materiały Warsztatów Geomorfologicznych, Maroko, 19.04–4.05.2006 r., SGP, WGiSR UW: 9–12.
  • Leopold L.B., Wolman M.G., Miller J.P., 1964. Fluvial Processes in Geomorphology. W.H. Freeman and Company, San Francisco.
  • Milhi A., 1997. Geological Map of Tinerhir 1:100 000. Ministere de L’Energie et des Mines, Direction de la Geologie, S.E.L.C.A. – Florence, Italie.
  • Powell D.M., Brazier R., Parsons A., Wainwright J., Nichols M., 2007. Sediment transfer and storage in dryland headwater streams. Geomorphology 88: 152–166.http://dx.doi.org/10.1016/j.geomorph.2006.11.001
  • Schulz O., Busche H., Benbouziane A., 2008. Decadal Precipitation Variances and Reservoir Inflow in the Semi-Arid Upper Drâa Basin (South-Eastern-Morocco). In: F. Zereini, H. Hötzl (eds.), Climatic changes and water resources in the Middle East and in North Africa. Springer, Berlin, Heidelberg: 165–178.http://dx.doi.org/10.1007/978-3-540-85047-2_13
  • Schulz O., de Jong C., 2004. Snowmelt and sublimation: field experiments and modeling in the High Atlas Mountains of Morocco. Hydrology and Earth System Sciences 8(6): 1076–1089.http://dx.doi.org/10.5194/hess-8-1076-2004
  • Stokes M., Mather A.E., Belfoul A., Farik F., 2008. Active and passive tectonic controls for transverse drainage and river gorge development in a collisional mountain belt (Dades Gorges, High Atlas Mountains, Morocco). Geomorphology 102: 2–20.http://dx.doi.org/10.1016/j.geomorph.2007.06.015
  • Strahler A.N., 1952. Dynamic basis of geomorphology. Bulletin of the Geological Society of America 63: 923–938.http://dx.doi.org/10.1130/0016-7606(1952)63[923:DBOG]2.0.CO;2
  • Thoot S., Nanson G.C., 2004. Forms and processes of two higly contrasting rivers in arid central Australia, and the implications for channel-pattern discrimination and prediction. Geological Society of America Bulletin 116: 802–816.
  • Thornes J.B., 1980. Structural instability and ephemeral channel behaviour. Zeitschrift für Geomorphologie, Supplement 36: 233–244.http://dx.doi.org/10.1130/B25308.1
  • Wysocki C., Sikorski P., 2009. Fitosocjologia stosowana w ochronie i kształtowaniu krajobrazu. Wyd. SGGW, Warszawa: 1–498.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-484f87d5-45a0-4b5b-8b57-3f0367a83001
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