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Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco

In this paper, we will study the sedimentary state of the river Sebou, which extends between the Mesopotamia, Inaouene Valley and Bouchabel Valley, which is an area of about 36 km (Figure 1). We will analyze the sedimentary components at the bottom of the oued and the level of the floodplain through the banks of the latter. This area comes directly after the confluence of Oued Sebou with Oued Inaouene, in the area of Hamria in douar Ben Hadan, as it extends to the western borders of the center of Sidi Daoud, downstream of the bridge of Sebou in douar Oulad Ben Hamou, where the Oued Sebou takes a general direction from southeast to northwest. This course draws free river confluences in the floodplain extending to the bottom of the Sebou Valley, which is surrounded by land dominated by clay hills of different heights, and overlooking the valley with long to medium slopes. In our study, we relied on fieldwork, including field observation, identification of sections to be studied and analyzed, determination of the properties of river sediments, including coarse elements and morphometric analysis of the gravel, and we relied on choreographic work to draw crosses. Sections and we worked on the identification of the types of banks and the nature of its sedimentary components, we studied the volume of coarse sedimentary elements, in addition to the study of fine sedimentary materials, including laboratory analysis of micro-sediment grains, and we worked on the morphoscopic analysis of quartz grains.

Accusative Case, Middle Sebou Valley, Inaouene and Buchable Rivers, Pri- Rif (Morocco)

APA Style

Mohammed Yazami Ztait, Siham Roudani, Fatima-Zahra Ouali Alami, Abdeslam Taleb, Rachid Laaouidi. (2022). Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. American Journal of Mechanics and Applications, 9(4), 35-45. https://doi.org/10.11648/j.ajma.20210904.11

ACS Style

Mohammed Yazami Ztait; Siham Roudani; Fatima-Zahra Ouali Alami; Abdeslam Taleb; Rachid Laaouidi. Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. Am. J. Mech. Appl. 2022, 9(4), 35-45. doi: 10.11648/j.ajma.20210904.11

AMA Style

Mohammed Yazami Ztait, Siham Roudani, Fatima-Zahra Ouali Alami, Abdeslam Taleb, Rachid Laaouidi. Sedimentary State of the Middle Sebou Valley, Between Oued Inaouene and Oued Bouchabel (Pri- Rif) - Morocco. Am J Mech Appl. 2022;9(4):35-45. doi: 10.11648/j.ajma.20210904.11

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1. A. Dridri & B. Fedan, Origine et distribution des argiles des formations superficielles du moyen Sebou (Maroc). Université Sidi Mohammed Ben Abdellah, FSD Géologie, Fès, Université Mohammed V. Agdal, ISDG, Maroc. Bulletin de l’institut scientifique. Rabat. 2001. N° 23. Pp. 55 – 65 (2001).
2. A. E. Mohamed and al, Comparison of the MUSLE Model and Two Years of Solid Transport Measurement, in the Bouregreg Basin, and Impact on the Sedimentation in the Sidi Mohamed Ben Abdellah Reservoir, Morocco. Water. Pp. 1-27, (2020).
3. C. Castanet, and al, Approche géographique, sédimentologie et géomorphologique intégrée pour la caractérisation des dynamiques fluviales de la Loire survenue durant les derniers 25000 ans (Val d’Orléans, Loiret). Univ Paris 1 Panthéon-Sorbonne, France. Univ Pierre et Marie Curie, Paris, France. BRGM, 2 Av. Cedex. France. 6ème colloque Géofcan. Bondy, France. Pp. 99-102 (2007).
4. E. F. Maryem and al, Hydrogeochemical assessment of mine water discharges from mining activity. Case of the Haut Beht mine (central Morocco). AIMS Environmental Science, 8 (1). Pp. 60-85, (2021).
5. F. Andrea and C. C. H. Jean, The International Sedimentary Geosciences Congress (ISGC) 2021 – An Opportunity to Shape the Futu re of Sedimentary Geosciences, Some of the authors of this public ation are also w orking on these r elated projects: Post-avulsion Channel Ev olution: Niger Delta Continental Slope and Geolog y, Philosophy, and Society. Pp. 1-5, (2020).
6. F. Andrea and M. H. Angela, Sustainability without Geology? A Shortsighted Approach. À publication by the society for sedimentary geology. VOLUME 19, NO. 2. Pp. 1-4, (2021).
7. C. Hervé, Paléo-environnements. Armand colin, 267 p, (2009).
8. H. Mohammed and al, Moroccan Groundwater Resources and Evolution with Global Climate Changes. Geosciences. Pp 1-26, (2020).
9. J. Deferne & N. Engel, Des débris de l’érosion aux roches sédimentaires. Extrait de « Le monde fascinant des roches ». 16p (2010).
10. J. L. Peiry, Le Transport sédimentaire sur l’Allier ET la problématique des captures de gravières. Univ Blaise Pascal. Séminaire technique. 21p (2011).
11. J. P. Larue, La dynamique des cours d’eau dans les zones de confluence au cours du Quaternaire. In: Norois. N°118. Pp. 227-244 (1983).
12. K. Aziza and al, Evaluation of the environmental and human health risk related to metallic contamination in agricultural soils in the Mediterranean semi-arid area (Saiss plain, Morocco). Environmental Earth Sciences. Pp 1-22, (2020).
13. L. Champagnac, Dynamique des formations superficielles et analyse morphologique du Val de Ruz. Univ de Neuchâtel. Institut de géographie et de géologie. 149p (2005).
14. M. Abderrahim and F. Ali, Cartographie des zones vulnérables à l’érosion hydrique en amont du barrage Allal El Fassi (Moyen Atlas-Maroc). Editions universitaires européennes. 109 p, (2019).
15. M. Chapuis, Mobilité des sédiments fluviaux grossiers dans les systèmes fortement anthropisés: éléments pour la gestion de la basse vallée de la Durance. Thèse en géographie. Univ Aix Marseille. CEREGE, France. 223p (2012).
16. M. G. Wolman, A method of sampling coarse bed material. American Geophysical Union. Transactions, 35: Pp. 951-956 (1954).
17. R. Tony, Dynamiques hydro-sédimentaires en petite Camargue à l’Holocène. Thèse de doctorat en géographie. Univ Montpellier III-Paul Valery, Art et Lettre, Langue et Sciences Humaines et Sociales. 309p (2006).
18. S. Maria and al, Effects of the construction of dams on the water and sediment fluxes of the Moulouya and the Sebou Rivers, Morocco. Reg Environ Change. Pp 5-12, (2002).
19. S. Sanja, and al, Geochemical Fractionation and Risk Assessment of Potentially Toxic Elements in Sediments from Kupa River, Croatia. Review of Water 2020, 12, 2024; doi: 10.3390/w12072024. Pp. 1-16 (2020).
20. T. Ali and al, Naissance et evolution du reseau hydrographique et terrasses fluviatiles dans les bassins du sebou et de l’inaouene (sillon sud-rifain central): état des connaissances. Actes RQM7, Agadir. Pp 186-205, (2013).
21. V. Bacchi, Etude expérimentale de la dynamique sédimentaire d’un système à forte pente soumis à des conditions hydrauliques faibles. Thèse de doctorat. Univ de Grenoble, École Doctorale Terre Univers Environnement. Paris. 209 p (2011).
22. W. Guanping and al, Sedimentary Evolution Characteris tics of Fine-Graine d Lithofac ies under the High-Resolut ion Isochronous Shelf Syste m: Insights from the Wufeng-Longm axi Shales in the Sichuan Basin. GeoScienceWorld Lithosphere. Pp. 1-20, (2021).
23. W. Peijia, and al, Morphological changes in the lower Lancang River due to extensive human activities. Review PeerJ. Jul 23; 8: e9471. doi: 10.7717/peerj.9471. eCollection. Pp. 1-21 (2020).
24. X. Devleeschouwer, Cours de sédimentologie (GEOL-F-204), Processus d’érosion mécanique. Univ Libre de Bruxelles. Univ d’Europe. 110p (2009).