Skip to main content
Log in

An introduction to the karst geomorphology of the Bisetun–Taqe Bostan historical region (northeast Kermanshah, Iran) with special emphasis on karst development as a serious threat for the UNESCO World Heritage Site

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

Abstract

The Bisetun–Taqe Bostan crushed carbonate massif (northeast of Kermanshah City) is a historical region that includes several famous monuments. Several types of karst features, the surface kind especially, have been developed in the area because of high rainfall in the area, tectonic crushing and high purity of the rocks. The field survey showed that the major karst features are karren, including rillenkarren, trittkarren, and solution runnels. Some of the monument stones by it have been deteriorating. Cavities and caves, solution dolines, and karstic springs are other observed karstic features in the area. Cavities and caves present mostly at intersections of shear faults or joint sets, which are considered the main location of water seepage throughout the limestone mass. Dolines in the region can be divided into two groups including solution and collapse dolines. The first group involves deep and large dolines without surface deposit cover, whereas the second group includes shallow dolines with smaller sizes covered by soil layers. Dolines are not problematic for the monuments because of their relatively high distance from them. There are a number of karstic springs in the study area; the Bisetun and Taq-e Bostan springs are the most important among them. Both springs discharge at a fault surface in vicinity of the monuments. As a part of the present study, deterioration occurring in the monuments due to the karst development was investigated. Moreover, some physical and chemical preservation methods were proposed to protect the monuments.

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
Fig. 15
Fig. 16
Fig. 17
Fig. 18
Fig. 19
Fig. 20
Fig. 21
Fig. 22

Similar content being viewed by others

References

  • Ahmadi M, Rezaie-Moghadam MH (2009) Assessment of slopes instability base on weights evidence using GIS case study in “Merek” Area Kermanshah, Iran. Geogr Res 24(95):85–108 (in Persian)

    Google Scholar 

  • Berberian M (1995) Master ‘‘Blind’’ thrust faults hidden under the Zagros folds: active basement tectonics and surface morphotectonics. Tectonophysics 241:193–224

    Article  Google Scholar 

  • Bögil A (1976) Die Wichtigsten Karrenformen der Kalkalpen. Paper presented at the confrence Karst Processes and Relevants Landforms, ISU Comission on Karst Denudation, Ljubljana, pp 141–149

  • Bögli A (1980) Karst hydrology and physical speleology. Springer, Berlin, p 291

    Book  Google Scholar 

  • Chorley RJ (1962) Geomorphology and general systems theory. United States Geological Survey Professional Paper, 500-B

  • Del-Prete S, Iovine G, Parise M, Santo A (2010) Origin and distribution of different types of sinkholes in the plain areas of Southern Italy. Geodin Acta 23:113–127

    Article  Google Scholar 

  • Dercourt J, Ricou LE, Vrielynck B (1993) Atlas Tethys Paleoenvironmental maps. Gauthier Villars, Paris, p 307

    Google Scholar 

  • De-Waele J (2008) Evaluating disturbance on Mediterranean Karst Areas: the example of Sardinia (Italy). Environ Geol 58:239–255

    Article  Google Scholar 

  • De-Waele J, Plan L, Audra P (2009) Recent developments in surface and subsurface karst geomorphology: an introduction. Geomorphology 106:1–8

    Article  Google Scholar 

  • De-Waele J, Gutiérrez F, Parise M, Plan L (2011) Geomorphology and natural hazards in karst areas: a review. Geomorphology 134:1–8

    Article  Google Scholar 

  • De-Wever P, Azema J, Fourcade E (1994) Radiolaires et Radiolarites, production primaire, diagenèse et paléogéographie. Bulletin des centres de recherches Exploration-production Elf-Aquitaine 18:1–63

    Google Scholar 

  • Dunham RJ (1962) Classification of carbonate rocks according to depositional texture. In: W. E. Ham (ed.) Classification of carbonate rocks. American Association of Petroleum Geologists, Memoir, pp 108–121

  • Ford DC, Williams PW (1989) Karst geomorphology and hydrology. Academic Division of Unwin Hyman Ltd, London, p 601

    Book  Google Scholar 

  • Ford DC, Williams PW (2007) Karst hydrogeology and geomorphology. Wiley, Chichester

    Book  Google Scholar 

  • Fornòs JJ, Ginès A (eds) (1996) Karren landforms. Universitat de les Illes Balears Press, Palma de Mallorca

    Google Scholar 

  • Ginés A, Knez M, Slabe T, Dreybrodt W (eds) (2009) Karst rock features: karren sculpturing. Založba ZRC, Ljubljana, p 561

    Google Scholar 

  • Iran Meteorological Organization (2013) Report of Kermanshah weather. [Online] available from: http://www.kermanshahmet.ir

  • Jafarbeyglou M, Moghimi E, Safari F (2010) Evaluating morphotectonic karst sinks in Parav–Bistoun mass using DEM. Geogr Environ Plann J 44(4):1–18 (in Persian)

    Google Scholar 

  • Karimi-Bavandpur A, Haji-Hoseini A (1999) Geological map of Kermanshah, 1:100,000. Geological Survey of Iran (GSI)

  • Kermanshah Regional Water Company (2011) Report of hydrogeology studies of the Bisetun Sarab, Iran (in Persian)

  • Köppen W (1936) Das geographische system der klimate. In: Köppen and Geiger (Eds) Handbuch der Klimatologie, Gebrüder Borntraeger, Berlin, p 44

  • LaMoreaux PE, Tanner JT (Eds) (2001) Springs and bottled waters of the world: ancient history, source, occurrence, quality and use hardcover

  • Macaluso T, Madonia G, Palmeri A, Sauro U (2002) Atlante dei karren nelle evaporiti della Sicilia. Quaderni del Museo Geologico G.G. Gemmellaro 5:1–143

    Google Scholar 

  • Maghsoudi M, Karimi H, Safari F, Charrahi Z (2010) Study of karst development using recession coefficient, spring death time and chemical and isotope analysis in Parav–Bistoun Massif (Kermanshah province-west of Iran). Phys Geogr Res Q 41(69):51–65 (in Persian)

    Google Scholar 

  • Mahmudi F, Maleki A (2001) Karstic evolution and their recognizing the water tables. Res Geogr 40:93–105 (in Persian)

    Google Scholar 

  • Maleki A, Oveisi M (2010) Effects of karst development on destruction of Bisetun inscription using radar method. Paper presented at the conference proceedings of the first iranian national conference on applied research in water resources, 11–13 May, Kermanshah, Iran

  • Ricou LE, Marcoux J (1980) Organisation générale etrôle structural des radiolarites et ophiolites le long du système alpino-méditerranéen. Bull Soc Geol Fr 1:1–14

    Article  Google Scholar 

  • Ricou LE, Braud J, Brunn JH (1977) Le Zagros. Mém. Hors série Soc. geol, France 8

    Google Scholar 

  • Saedi B, Heidari M, Mohseni H, Momeni AA (2012) The study of durability of the Darius Inscription in the Bisetun area. Paper presented at the conference 31th national symposium congress on geoscience, geological survey of Iran, 30th November–1th December 2012, Tehran, Iran (in Persian)

  • Stocklin J (1968) Structural history and tectonics of Iran: a review. AAPG Bulletin 52:1229–1258

    Google Scholar 

  • Sweeting MM (1973) Karst landforms. Macmillen, London, p 362

  • Sweeting MM (1981) Karst geomorphology. In: Rhodes W. & C. U. Fairbridge (ed.), Benchmark papers in geology, Hutchinson Ross Publishing Company, Stroudsburg

  • Torabi-Kaveh M, Heidari M, Miri M (2012) Karstic features in gypsum of Gachsaran formation (case study; Chamshir Dam reservoir, Iran). Carbonates Evaporites 27:291–297

    Article  Google Scholar 

  • Trudgill ST (1985) Limestone geomorphology. Geomorphology Texts 8. Longman Group Ltd., London

  • UNESCO World Heritage Center (2006) World heritage list, Bisotun. [Online] available from: http://whc.unesco.org/en/list/1222

  • UNESCO World Heritage Center (2007) World heritage list, Taq-e Bostan. [Online] available from: http://whc.unesco.org/en/tentativelists/5182

  • US Patent No: 6296905 (2001) Method for protecting and consolidating calcareous materials

  • Van-Beynen P, Townsend K (2005) A disturbance index for karst environments. Environ Manage 36:101–116

    Article  Google Scholar 

  • Veni G (1999) A geomorphological strategy for conducting environmental impact assessments in karst areas. Geomorphology 31:151–180

    Article  Google Scholar 

  • Veress M (2000) The main types of karren development of limestone surface without soil covering. Karsztfejlődés IV. BDF Természetföldrajzi Tanszék, Szombathely, pp 7–30

  • Veress M (2010) Karst environments–Karren formation in high mountains. Springer, Heidelberg, p 230

    Book  Google Scholar 

  • Vincent PJ (1983) The morphology and morphometry of some arctic Trittkarren. Zeitschrift für Geomorphologie 27:205–222

    Google Scholar 

  • Werner E (1975) Soluation of calcium carbonate and the formation of karren. Cave Geology 1:3–28

    Google Scholar 

  • White WB (1988) Geomorphology and hydrology of Karst Terrains. Oxford University Press, New York

    Google Scholar 

  • Williams PW (Ed.) (1993) Karst Terrains, Environmental changes and human impact: Cremingen-Destedt, Germany. no 25, Catena Supplement, p 268

  • Zhu-Xuewen Z, Waltham T (2005) Tiankengs: definition and description. Cave and Karst Science 32:75–80

    Google Scholar 

Download references

Acknowledgments

This work was supported by the Bu-Ali Sina University. The authors are grateful to Prof. Márton Veress from the University of Western Hungary for the help and suggestions in the interpretation of karstic features.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to M. H. Ghobadi.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Ghobadi, M.H., Torabi-Kaveh, M., Miri, M. et al. An introduction to the karst geomorphology of the Bisetun–Taqe Bostan historical region (northeast Kermanshah, Iran) with special emphasis on karst development as a serious threat for the UNESCO World Heritage Site. Bull Eng Geol Environ 74, 1071–1086 (2015). https://doi.org/10.1007/s10064-014-0662-0

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10064-014-0662-0

Keywords

Navigation