SHOTORI (ISHTAR) MOUNTAINS, A GEOTOP PHENOMENON IN EASTERN CENTRAL IRAN

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ASGHARI MOGHADAM M.R.; ASGHARI MOGHADAM N.

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Journal: GEOGRAPHY Year:2010 | Volume:4 | Issue:12 Page(s): 79-112

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Title

SHOTORI (ISHTAR) MOUNTAINS, A GEOTOP PHENOMENON IN EASTERN CENTRAL IRAN

Author(s)

ASGHARI MOGHADAM M.R. | ASGHARI MOGHADAM N. | Issue Writer Certificate

Keywords

SHOTORIQ3

TABASQ3

AZMIGHANQ3

RIVER CAPTUREQ2

DETRITAL FANQ2

GEOTOPQ3

Abstract

SHOTORI Mountains located in east of Iran are important from geologic, geomorphologic and physical morphologic perspectives. These mountains formed by Naiband flat consist of geologic formation from Denovian to lower Kertacae, which mostly include lime stone and dolomite.SHOTORI Mountains result from coming up drifting on the TABAS plate through Austrian and Laramian orogenesis. This drift leads to asymmetric eastern and western hillsides, therefore hydrographic drainage lean to western hillside and rainfall flews to the TABAS plate which causes agricultural development in TABAS.Remained climate is observed everywhere in vallies and outside of the mountains (e.g. alluvial trases, alluvial cones, etc). Interesting landscapes observed make SHOTORI Mountains as a “geo top” which can attract tourists and cause economic development.

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تاثیر قرارگیری ارتفاعات و فعالیت گسل ها بر روند تکاملی مخروط افکنه ها، نمونه موردی مخروط افکنه سر در تبس

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APA: Copy

ASGHARI MOGHADAM, M.R., & ASGHARI MOGHADAM, N.. (2010). SHOTORI (ISHTAR) MOUNTAINS, A GEOTOP PHENOMENON IN EASTERN CENTRAL IRAN. GEOGRAPHY, 4(12), 79-112. SID. https://sid.ir/paper/207995/en

Vancouver: Copy

ASGHARI MOGHADAM M.R., ASGHARI MOGHADAM N.. SHOTORI (ISHTAR) MOUNTAINS, A GEOTOP PHENOMENON IN EASTERN CENTRAL IRAN. GEOGRAPHY[Internet]. 2010;4(12):79-112. Available from: https://sid.ir/paper/207995/en

IEEE: Copy

M.R. ASGHARI MOGHADAM, and N. ASGHARI MOGHADAM, “SHOTORI (ISHTAR) MOUNTAINS, A GEOTOP PHENOMENON IN EASTERN CENTRAL IRAN,” GEOGRAPHY, vol. 4, no. 12, pp. 79–112, 2010, [Online]. Available: https://sid.ir/paper/207995/en

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