Skip to main content

Advertisement

Log in

The Mazafran river (western Sahel of Algiers): superimposition or antecedence?

  • ArabGU2016
  • Published:
Arabian Journal of Geosciences Aims and scope Submit manuscript

Abstract

At the western Sahel of Algiers, the watercourse of the Mazafran river is perpendicular to the Sahel fold, forming a gorge that has developed in a tectono-eustatic context characteristic of the Sahel region. This gorge has formed in a regime of superimposition which involves the evolution of antecedence in relation to the Sahel uplift. This deduction is the result of multiple analyses that are based on a stratigraphic study which characterizes the succession of continental and marine deposits and the analyses of lineament map of tectonic evolution during the Quaternary which is marked by the Sahel folding. In order to correlate the chronology between the fluvial and marine sedimentary dynamics, a geomorphological study of the Mazafran alluvial terraces associated with the paleoshorelines was realized. The obtained results reveal that the development of the Mazafran river gorge is complex.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14

Similar content being viewed by others

References

  • Avouac JP, Peltzer G (1993) Active tectonics in southern Xinjiang, China: analysis of terrace riser and normal fault scarp degradation along the Hotan-Qira fault system. J Geophys Res 98:21 773–21 807

    Article  Google Scholar 

  • Ayme A, Ayme J M, Magne J (1954) Etude des terrains néogènes de la cluse du Mazafran (Sahel d’Alger), Bull. du Serv. de la carte geol.de l’Algérie, pp. 129–150

  • Ayme A (1952) Le Quaternaire littoral des environs d’Alger. Actes du Cong. Panaf. de préhistoire, II session, Alger 1952, pp.243–246

  • Blum MD, Straffin EC (2001) Fluvial responses to external forcing: examples from the French Massif Central, the Texas Coastal Plain (USA), the Sahara of Tunisia, and the lower Mississippi Valley (USA). In: Maddy D, Macklin M, Woodward J (eds) River basin sediment systems: archives of environmental change. Balkema, Rotterdam, pp 195–228

    Google Scholar 

  • Boudiaf A (1996) Etude sismotectonique de la région d’Alger et de la Kabylie. PhD. Dissertation, Univ. Montpellier, 274 p

  • Bowman D, Svoray T, Devora S, Shapira I, Laronne JB (2010) Extreme channel incision and shape evolution in response to a continuous, rapid base-level fall, the Dead Sea, Israel. Geomorphology 114(3):227–237

    Article  Google Scholar 

  • Bridgland DR (2000) River terrace systems in north-west Europe: an archive of environmental change, uplift and early human occupation. Quat Sci Rev 19:1293–1303

    Article  Google Scholar 

  • Bull WB (1991) Geomorphic responses to climatic change. Oxford University Press, New York 321 p

    Google Scholar 

  • Bull WB (1990) Stream-terraces genesis: implications for soil development. Geomorphology 3:351–367

    Article  Google Scholar 

  • Carcaillet J, Mugnier JL, Koci R, Jouanne F (2009) Uplift and active tectonics of southern Albania inferred from incision of alluvial terraces. Quat Res 71(3):465–476

    Article  Google Scholar 

  • Dalloni M (1933) Le Pliocène du sahel oriental et de la Kabylie, B.S.H.N.Afr. Du Nord, t. XXIV, p. 9–18

  • De Lamothe G (1911) Les anciennes lignes de rivage du Sahel d’Alger et d’une partie de la côte Algérienne, Soc. Géol. France, Comp. Rendus, n 3

  • Ficheur E (1910) Carte géologique de Koléa. Algérie, feuille n° 41, B4. C16

  • Ficheur E (1896) Aperçu sommaire sur les terrains néogènes du Sahel d’Alger. B.S.G. F (3eme série), t. XXIV, p. 973–981

  • Finnegan NJ, Sklar LS, Fuller TK (2007) Interplay of sediment supply, river incision, and channel morphology revealed by the transient evolution of an experimental bedrock channel. J Geophys Res 112(F3):F03S11

    Article  Google Scholar 

  • Formento-Trigilio ML, Burbank DW, Nicol A, Schulmeister J, Rieser U (2002) River response to an active fold-and-thrust belt in a convergent margin setting, North Island, New Zealand. Geomorphology 49:125–152

    Article  Google Scholar 

  • Gignoux M (1915) L’étage calabrien (Pliocène supérieur marin) sur le versant nord est de l’Apennin entre le Monte Gargano et Plaisance. Extrait du Bulletin de la Société Géologique de France, 4e série, t. XIV, p. 324

  • Glangeaud L, Ayme A, Caire A, Mattauer M, Muraour P (1952) Histoire géologique de la province d’Alger, Publ. XIX C.G.I., Alger, Mono. Reg., 1° Serie, Algérie, 25, 40 Fig., 3 pl.h.t. 142 p

  • Glangeaud L (1932) Etude géologique de la région littorale de la province d’Alger. Thèse Doct. Sci., Paris, Bull. Serv. Carte géol. Alger 2ème Série, Stratig. N°8, 608 p

  • Hancock GS, Anderson RS (2002) Numerical modeling of fluvial strath-terrace formation in response to oscillating climate. Geol Soc Am Bull 114:1131–1142

    Google Scholar 

  • Harbi A, Maouche S, Ayadi A, Benouar D, Panza GF, Benhallou H (2004) Seismicity and tectonic structures in the site of Algiers and its surroundings: a step towards microzonation. Pageoph 161:949–967

    Article  Google Scholar 

  • Karner DB, Marra F (1998) Correlation of fluvio-deltaic aggradational sections with glacial climate history: a revision of the Pleistocene stratigraphy of Rome. Geol Soc Am Bull 110:748–758

    Article  Google Scholar 

  • Lague D (2010) Reduction of long-term bedrock incision efficiency by short-term alluvial cover intermittency. Geophysical Research 115(2):F02011

    Google Scholar 

  • Lavé J, Avouac JP (2001) Fluvial incision and tectonic uplift across the Himalaya of central Nepal. Geophysical Research 106:26561–26591

    Article  Google Scholar 

  • Maouche S, Meghraoui M, Morhange C, Belabbes S, Bouhadad Y, Haddoum H (2011) Active coastal thrusting and folding, and uplift rate of the Sahel Anticline and Zemmouri earthquake area (Tell Atlas, Algeria). J Tectonophys 509(1–2):69–80

    Article  Google Scholar 

  • Meghraoui M (1991) Blind reverse faulting system associated with the Mont Chenoua-Tipaza earthquake of 29 October 1989 (north-central Algeria). Terra Nova 3:84–93

    Article  Google Scholar 

  • Meghraoui M. (1988) Geologie des zones sismiques du nord de l’Algérie. Paleosismologie, Tectonique active et synthesesismo-tectonique, these de Doc. Es. Sci., Univ Paris VI, 356 p

  • Merritts DJ, Vincent KR, Wohl EE (1994) Long river profiles, tectonismandeustasy: a guide to interpreting fluvial terraces. J Geophys Res 99:14031–14050

    Article  Google Scholar 

  • Mizutani T (1998) Laboratory experiment and digital simulation of multiple fill-cut terrace formation. Geomorphology 24:353–361

    Article  Google Scholar 

  • Moshe LB, Haviv I, Enzel Y, Zilberman E, Matmon A (2008) Incision of alluvial channels in response to a continuous base level fall: field characterization, modeling, and validation along the Dead Sea. Geomorphology 93:524–536

    Article  Google Scholar 

  • Pan B, Su H, Hu Z, Hu X, Gao H, Li J, Kirby E (2009) Evaluating the role of climate and tectonics during non-steady incision of the Yellow River: evidence from a 124 Ma terrace record near Lanzhou, China. Quat Sci Rev 28(2009):3281–3290

    Article  Google Scholar 

  • Pan B, Burbank D, Wang Y, Wu G, Li J, Guan Q (2003) A 900 k.y. record of strata terrace formation during glacial-interglacial transitions in northwest China. Geology 31(11):957–960

    Article  Google Scholar 

  • Pazzaglia FJ, Gardner TW, Merritts DJ (1998) Bedrock fluvial incision and longitudinal profile development over geologic time scales determined by fluvial terraces Geophysical Monograph Series. American Geophysical Union, Washington

    Google Scholar 

  • Rockwell TK, Keller EA, Clark MN, Johnson DL (1984) Chronology and rates of faulting of Ventura River terraces, California. GeolSoc Am Bull 95:1466–1474

    Article  Google Scholar 

  • Saoudi N (1989) Pliocène et pléistocène inferieur et moyen du Sahel occidental d’Alger, Entr. Nat. Du Livre, n° 2020/85, 71 fig., 10 photo. h.t

  • Törnqvist TE (1998) Longitudinal profile evolution of the Rhine Meuse system during the last deglaciation: interplay of climate change and glacioeustasy? Terra Nova 10:11–15

    Article  Google Scholar 

  • Valla PG, Van Der Beek PA, Lague D (2010) Fluvial incision into bedrock: insights from morphometric analysis and numerical modeling of gorges incising glacial hanging valleys (Western Alps, France). Geophysical Research 115(F2):F02010

    Article  Google Scholar 

  • Van den Berg MW, Van Hoof T (2001) The Maas terrace sequence at Maastricht, SE Netherlands: evidence for 200 m of late Neogene and Quaternary surface uplift. In D. Maddy, M. Macklin &J. Woodward (eds), River Basin Sediment Systems: Archives of Environmental Change. Balkema, Rotterdam, 45–86

  • Weisrock A (2002) L’incision des vallées : une question de temps. Revue Géographique de l’Est 4:155–161

    Google Scholar 

  • Westaway R, Cordier S, Bridgland D (2009) Étude du soulèvement Pléistocène dans le nord-est de la France et le sud-ouest de l’Allemagne d’après les terrasses du bassin de la Moselle : relation avec les propriétés crustales, Quaternaire, vol. 20/1. 2009

  • Westaway R (2002a) Geomorphological consequences of weak lower continental crust, and its significance for studies of uplift, landscape evolution, and the interpretation of river terrace sequences. Neth J Geosci 81:283–304

    Google Scholar 

  • Westaway R (2002b) Long-term river terrace sequences: evidence for global increases in surface uplift rates in the Late Pliocene and early Middle Pleistocene caused by flow in the lower continental crust induced by surface processes. Neth J Geosci 81:305–328

    Google Scholar 

  • Westaway R, Maddy D, Bridgland D (2002) Flow in the lower continental crust as a mechanism for the Quaternary uplift of south-east England: constraints from the Thames terrace record. Quat Sci Rev 21:559–603

    Article  Google Scholar 

  • Westaway R, Bridgland D, Mishra S (2003) Rheological differences between Archaean and younger crust can determine rates of Quaternary vertical motions revealed by fluvial geomorphology. Terra Nova 15:287–298

    Article  Google Scholar 

  • Yassini I (1973) Nouvelles données stratigraphiques et microfaunistiques sur la limite Pliocène inférieur/Pliocène moyen (Plaisancien-Astien) dans la région d’Alger. Rev. Micropaleonto., 16, n°4

Download references

Acknowledgements

The authors are grateful to the director of Geomorphology and Georisks laboratory (Faculty of Earth Sciences, USTHB, Algeria) for providing the necessary laboratory facilities and other logistic support and discussion for the study and we would like to thank Professor S. Maouche (CRAAG, Algeria) for his help and precious pieces of advice.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Djamal Akziz.

Additional information

This article is part of the Topical Collection on Current Advances in Geology of North Africa

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Akziz, D., Guendouz, M., Guettouche, M.S. et al. The Mazafran river (western Sahel of Algiers): superimposition or antecedence?. Arab J Geosci 11, 121 (2018). https://doi.org/10.1007/s12517-018-3469-7

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12517-018-3469-7

Keywords

Navigation