Skip to main content
Log in

Structural and geomorphological controls of the present-day landslide in the Moulares phosphate mines (western-central Tunisia)

  • Original Paper
  • Published:
Bulletin of Engineering Geology and the Environment Aims and scope Submit manuscript

Abstract

Present-day deformations occurring within both waste dump and bedrock in the Northern Table mine of Moulares, western central Tunisia, show complex landslides of kilometric dimensions. Rock bodies in this mine slide due to the shear stress concentration along a complex sliding surface. As a result of gravity displacement, these rocks display diverse associate structures such as detachment, open fractures, folds, and striated thrust planes. Interaction between predisposition factors (inherited structures, topography, slope, gravity) and triggering factors (artificial vibrations and seismotectonic activity) provided favourable conditions for the sliding. Sloping fractured ground, marly lithology and meteoric water act further to exacerbate the instability in the ground and encourage rock failure. Additionally, the seismic hazard due to the sustained tectonic activity of the Gafsa fault and the vibrations due to explosive detonation can together trigger significant landslide movement.

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. 5a–d
Fig. 6a–f
Fig. 7a–c

Similar content being viewed by others

References

  • Abbott PL (2004) Natural disasters. McGraw-Hill, New York

    Google Scholar 

  • Ahmadi R, Ouali J, Eric Mercier, Mansy JL, Van-Vliet Lanoë B, Launeau P, Rhekhiss F, Rafini S (2006) The geomorphologic responses to hinge migration in the fault-related folds in the Southern Tunisian Atlas. J Struct Geol 28(4):721–728

    Article  Google Scholar 

  • Bahrouni N, Bouaziz S, Soumaya A, Ben Ayed N, Attafi K, Houla Y, El Ghali A, Rebai N (2013) Neotectonic and seismotectonic investigation of seismically active regions in Tunisia: a multidisciplinary approach. J Seismolog 18(2):235

    Article  Google Scholar 

  • Ben Hassen M, Rebai N, Deffontaines B, Turki M-M, Chaabani F (2011) Phosphate mine subsidences deduced from differential interferometry (DInSAR): the Moulares case example (southern Atlas of Tunisia). C R Geosci 343(2011):729–737

    Article  Google Scholar 

  • Boukadi N (1989) Sur le plissement disharmonique et la dispersion des axes de plis dans les couloirs de décrochement: l’exemple du faisceau de Moularès de Tunisie. C R Acad Sci II 309:2105–2110

    Google Scholar 

  • De Blasio FV (2011) Introduction to the physics of landslides: lecture notes on the dynamics of mass wasting. Springer, Amsterdam. doi:10.1007/978-94-007-1122-8

  • Dlala M, Hfaiedh M (1993) Le séisme du 7 novembre 1989 à Metlaoui (Tunisie méridionale): une tectonique active en compression. C R Acad Sci Paris 317(2):1297–1307

    Google Scholar 

  • Galfati I, Beji Sassi A, Zaier A, Bouchardon JL, Bilal E, Jordon JL, Sassi S (2010) Geochemistry and mineralogy of Paleocene Oum El Khecheb phosphorites (Gafsa-Metlaoui) Tunisia. Geochem J 44:189–210

    Article  Google Scholar 

  • Highland LM, Bobrowsky P (2008) The landslide handbook—a guide to understanding landslides, vol 1325. US Geological Survey Circular, Reston

    Google Scholar 

  • Keefer DK (1984) Landslides caused by earthquakes. Geol Soc Am Bull 1984(95):406–421

    Article  Google Scholar 

  • Marzorati S, Luzia L, De Amicisb M (2002) Rock falls induced by earthquakes: a statistical approach. Soil Dyn Earthq Eng 22(2002):565–577

    Article  Google Scholar 

  • Saïd A, Chardon D, Baby P, Ouali J (2011) Active oblique ramp faulting in the Southern Tunisian Atlas. Tectonophysics 499(1–4):178–189

    Article  Google Scholar 

  • Schuster RL, Highland LM (2004) Impact of landslides and innovative landslide-mitigation measures on the natural environment. In: Proceedings of the International Conference on Slope Engineering, 8–10 December 2003, Hong Kong, China

  • Wang D, Cao L-Z, Piao C-D, Xue Y-D, Wang M (2011) Study on high and steep slope stability of surface mine based on RFPA-SRM. J Coal Sci Eng (China) 17:119–123

  • Zaïer A, Beji-Sassi A, Sassi S, Moody RTJ (1998) Basin evolution and deposition during the Early Palaeogene in Tunisia. Petroleum Geology of North Africa. Geol Soc Lond Spec Publ 132:375–393

    Article  Google Scholar 

  • Zargouni F (1985) Tectonique de l’Atlas méridional de Tunisie: évolution géométrique et cinématique des structures en zone de cisaillement. Thesis, Univ. Louis Pasteur, Strasbourg

Download references

Acknowledgments

The authors would like to thank Martin G. Culshaw, Roger Cojean and the anonymous reviewers for their constructive comments and helpful suggestions.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Ferid Dhahri.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Dhahri, F., Benassi, R., Mhamdi, A. et al. Structural and geomorphological controls of the present-day landslide in the Moulares phosphate mines (western-central Tunisia). Bull Eng Geol Environ 75, 1459–1468 (2016). https://doi.org/10.1007/s10064-015-0827-5

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10064-015-0827-5

Keywords

Navigation