Geomorphology of Karst Features of Shiraz City and Arjan Plain and Development Limitations
Karst term is the determiner of a variety of areas or
landforms and unique perspectives that have been formed in result of
the of the ingredients dissolution of rocks constituter by natural
waters. Shiraz area with an area of 5322km2 is located in the simple
folded belt in the southern part of Zagros Mountain of Fars, and is
surrounded with Limestone Mountains (Asmari formation). Shiraz
area is located in Calcareous areas. The infrastructure of this city is
lime and absorbing wells that the city can influence the Limestone
dissolution and those accelerate its rate and increase the cavitation
below the surface. Dasht-e Arjan is a graben, which has been created
as the result of activity of two normal faults in its east and west sides.
It is a complete sample of Karst plains (Polje) which has been created
with the help of tectonic forces (fault) and dissolution process of
water in Asmari limestone formation. It is located 60km. off south
west of Shiraz (on Kazeroon-Shiraz road). In 1971, UNESCO has
recognized this plain as a reserve of biosphere. It is considered as one
of the world’s most beautiful geological phenomena, so that most of
the world’s geologists are interested in visiting this place. The
purpose of this paper is to identify and introduce landscapes of Karst
features shiraz city and Dasht-e Arjan including Karst dissolution
features (Lapiez, Karst springs, dolines, caves, underground caves,
ponors, and Karst valleys), anticlines and synclines, and Arjan Lake.
[1] A. Maleki, D. Shoohani, M. AlaeiTaleghani, “Zooning of Karst development in Kermanshah provine, Modarres seasonal of humanities,” 13th course, issue No.1, spring, pp: 272-295, 2009.
[2] A. Afrasiabian, “Karst, a trustworthy reservoir to supply water resources,” 2007.
[3] A. Afrasiabian, “the significance of research and studies on Karst water resources in Iran,” proceedings of the second international congress on water in Karst formations, Tehran, Kermanshah, 1998.
[4] A. Aghanabati, “Iran’s Geology,” Publication of Geology Organization, 2004.
[5] A. Alizadeh, “Principles of Applied Hydrology,”AstanGhodsRazavi presses, 2009.
[6] A. Behniafar, H. Ghanbarzadeh, A. Farzaneh, “Geomorphic features of Ahmald Karst mass in the northern slopsof Binalood Mountains,” Geography & Development Journal, Issue No.13, pp: 121-130, 2009.
[7] Asmari Consulting Engineers, “Method of choosing qualitative selective water resources in Dasht-e Arjan zone under study,” 2009.
[8] D. Ford, P.Williams, “Karst hydrogeology and geomorphology,” John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester, West Sussex PO19 8SQ, England, 2007.
[9] D. Gillison “caves, processes, development and management,”EdvardArnold. London, 2004.
[10] F. Mahmoudi, “Structural Geomorphology,” Publication of Payam-e Noor University of Iran, pp.: 80-90, 2006.
[11] F.Regional Water Organization, Bushehr water supply project, “water resources explanation; report on the investigation of Kazeroon Karst water resources,” 1983.
[12] F.Regional Water Organization, “Deputy Office of Water Resources Studies, Domestic Lakes of Fars Province,” 1998.
[13] F.Regional Water Organization, “Report on the collection of data from Dasht-e Arjan,” 1968.
[14] Google Earth2014.
[15] H.KarimiVardanjani, “an Introduction to Karst development in the southwest of Iran,” Proceedings of the first national conference on applied researches of Iran’s water resources, pp: 288-298, 2010.
[16] H. Ahmadi “Applied Geomorphology,” First Volume, Tehran University Press, Fifth Edition, 2007.
[17] H. Moghimi, “Karst Hydrology,” Publication of Payam-e Noor University of Iran, 2005.
[18] http://ngdir.ir/.
[19] http://www.zonums.com/gmaps/digipoint. php.
[20] J. H.Makleod, M.Majedi, “map of Kazerun (1:100,000),” Iranian Oil Operating Companies, 1972.
[21] M.Haririan, “Iran’s Geo-morphology,” Publication of Islamic Azad University, pp: 96, 1990.
[22] M.Hemmatizadeh, “Studying geo-tourism capabilities of Karst features in Dasht-e Arjan, Fars province,” the 3rd national scientific student congress of geography, Tehran University, month of June, 2012.
[23] M.Sadeghi, E. RaeisiArdekani, “Investigating the factors effective on drying of Arjan lagoon,” 15th congress of Iran’s Geological Association, pp: 2-7, 2012.
[24] M.Sedaghat, et al. “Geology Map, 1: 100000 of Shoorab,” State Mineral Exploration & Geology Organization, 2004.
[25] M. AlaeiTaleghani, “Iran’s Geomorphology,” second edition, Ghoomes press, pp: 276, 2003.
[26] M. Jamali, “Investigating geo-tourism potentials of Dasht-e Arjan in Fars province,” Proceedings of 30th congress on geology science of Iran’s Mineral Exploration & Geology Organization, Feb. 22, 23, pp: 4-5, 2012.
[27] P. G.Llewellyn, H.Ahdoot, “Geology map of Famur (1:100,000),” Iranian Oil Operating Companies, 1973.
[28] P. Millanovic, “Karst hydrology WRP,” Colorado, U.S.A, 1988.
[29] R.KoshRaftar, “Protectionareas ofkarstandcaves,”RashtPublicationsHaqshenas, 2010.
[30] S.Velayati, F. Khanalizadeh, “Studying the relation of tectonic structures and Karst features,” (case study of Kardeh drainage basin), geography (research and scientific seasonal of Iran’s Geography Association), new course, 9th year, issue No.31, winter, and pp: 171-189, 2012.
[31] Z. Ara Fars Consulting Engineers, “Investigation into the side effect of water taken from the wells around Parishan lagoon,” general office of Fars Environment Protection, 2010.
[1] A. Maleki, D. Shoohani, M. AlaeiTaleghani, “Zooning of Karst development in Kermanshah provine, Modarres seasonal of humanities,” 13th course, issue No.1, spring, pp: 272-295, 2009.
[2] A. Afrasiabian, “Karst, a trustworthy reservoir to supply water resources,” 2007.
[3] A. Afrasiabian, “the significance of research and studies on Karst water resources in Iran,” proceedings of the second international congress on water in Karst formations, Tehran, Kermanshah, 1998.
[4] A. Aghanabati, “Iran’s Geology,” Publication of Geology Organization, 2004.
[5] A. Alizadeh, “Principles of Applied Hydrology,”AstanGhodsRazavi presses, 2009.
[6] A. Behniafar, H. Ghanbarzadeh, A. Farzaneh, “Geomorphic features of Ahmald Karst mass in the northern slopsof Binalood Mountains,” Geography & Development Journal, Issue No.13, pp: 121-130, 2009.
[7] Asmari Consulting Engineers, “Method of choosing qualitative selective water resources in Dasht-e Arjan zone under study,” 2009.
[8] D. Ford, P.Williams, “Karst hydrogeology and geomorphology,” John Wiley & Sons Ltd, The Atrium, Southern Gate, Chichester, West Sussex PO19 8SQ, England, 2007.
[9] D. Gillison “caves, processes, development and management,”EdvardArnold. London, 2004.
[10] F. Mahmoudi, “Structural Geomorphology,” Publication of Payam-e Noor University of Iran, pp.: 80-90, 2006.
[11] F.Regional Water Organization, Bushehr water supply project, “water resources explanation; report on the investigation of Kazeroon Karst water resources,” 1983.
[12] F.Regional Water Organization, “Deputy Office of Water Resources Studies, Domestic Lakes of Fars Province,” 1998.
[13] F.Regional Water Organization, “Report on the collection of data from Dasht-e Arjan,” 1968.
[14] Google Earth2014.
[15] H.KarimiVardanjani, “an Introduction to Karst development in the southwest of Iran,” Proceedings of the first national conference on applied researches of Iran’s water resources, pp: 288-298, 2010.
[16] H. Ahmadi “Applied Geomorphology,” First Volume, Tehran University Press, Fifth Edition, 2007.
[17] H. Moghimi, “Karst Hydrology,” Publication of Payam-e Noor University of Iran, 2005.
[18] http://ngdir.ir/.
[19] http://www.zonums.com/gmaps/digipoint. php.
[20] J. H.Makleod, M.Majedi, “map of Kazerun (1:100,000),” Iranian Oil Operating Companies, 1972.
[21] M.Haririan, “Iran’s Geo-morphology,” Publication of Islamic Azad University, pp: 96, 1990.
[22] M.Hemmatizadeh, “Studying geo-tourism capabilities of Karst features in Dasht-e Arjan, Fars province,” the 3rd national scientific student congress of geography, Tehran University, month of June, 2012.
[23] M.Sadeghi, E. RaeisiArdekani, “Investigating the factors effective on drying of Arjan lagoon,” 15th congress of Iran’s Geological Association, pp: 2-7, 2012.
[24] M.Sedaghat, et al. “Geology Map, 1: 100000 of Shoorab,” State Mineral Exploration & Geology Organization, 2004.
[25] M. AlaeiTaleghani, “Iran’s Geomorphology,” second edition, Ghoomes press, pp: 276, 2003.
[26] M. Jamali, “Investigating geo-tourism potentials of Dasht-e Arjan in Fars province,” Proceedings of 30th congress on geology science of Iran’s Mineral Exploration & Geology Organization, Feb. 22, 23, pp: 4-5, 2012.
[27] P. G.Llewellyn, H.Ahdoot, “Geology map of Famur (1:100,000),” Iranian Oil Operating Companies, 1973.
[28] P. Millanovic, “Karst hydrology WRP,” Colorado, U.S.A, 1988.
[29] R.KoshRaftar, “Protectionareas ofkarstandcaves,”RashtPublicationsHaqshenas, 2010.
[30] S.Velayati, F. Khanalizadeh, “Studying the relation of tectonic structures and Karst features,” (case study of Kardeh drainage basin), geography (research and scientific seasonal of Iran’s Geography Association), new course, 9th year, issue No.31, winter, and pp: 171-189, 2012.
[31] Z. Ara Fars Consulting Engineers, “Investigation into the side effect of water taken from the wells around Parishan lagoon,” general office of Fars Environment Protection, 2010.
@article{"International Journal of Earth, Energy and Environmental Sciences:68898", author = "Meysam Jamali and Ebrahim Moghimi and Zean Alabden Jafarpour", title = "Geomorphology of Karst Features of Shiraz City and Arjan Plain and Development Limitations", abstract = "Karst term is the determiner of a variety of areas or
landforms and unique perspectives that have been formed in result of
the of the ingredients dissolution of rocks constituter by natural
waters. Shiraz area with an area of 5322km2 is located in the simple
folded belt in the southern part of Zagros Mountain of Fars, and is
surrounded with Limestone Mountains (Asmari formation). Shiraz
area is located in Calcareous areas. The infrastructure of this city is
lime and absorbing wells that the city can influence the Limestone
dissolution and those accelerate its rate and increase the cavitation
below the surface. Dasht-e Arjan is a graben, which has been created
as the result of activity of two normal faults in its east and west sides.
It is a complete sample of Karst plains (Polje) which has been created
with the help of tectonic forces (fault) and dissolution process of
water in Asmari limestone formation. It is located 60km. off south
west of Shiraz (on Kazeroon-Shiraz road). In 1971, UNESCO has
recognized this plain as a reserve of biosphere. It is considered as one
of the world’s most beautiful geological phenomena, so that most of
the world’s geologists are interested in visiting this place. The
purpose of this paper is to identify and introduce landscapes of Karst
features shiraz city and Dasht-e Arjan including Karst dissolution
features (Lapiez, Karst springs, dolines, caves, underground caves,
ponors, and Karst valleys), anticlines and synclines, and Arjan Lake.
", keywords = "Dasht-eArjan, Fault, Karst features, Shiraz City,
Zagros.", volume = "9", number = "1", pages = "25-7", }
