INVESTIGATING QUATERNARY GLACIAL GEOMORPHOLOGICAL EVIDENCES AT THE NORTHEAST HEIGHTS OF IRAN (CASE STUDY: BINALUD MOUNTAIN RANGES)

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GHORBANI SHOORESTANI ALI; KHOSRAVI OZRA; NOURMOHAMMADI ALIMOHAMMAD

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Journal: QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES Year:2016 | Volume:5 | Issue:1 Page(s): 1-13

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Title

INVESTIGATING QUATERNARY GLACIAL GEOMORPHOLOGICAL EVIDENCES AT THE NORTHEAST HEIGHTS OF IRAN (CASE STUDY: BINALUD MOUNTAIN RANGES)

Author(s)

GHORBANI SHOORESTANI ALI | KHOSRAVI OZRA | NOURMOHAMMADI ALIMOHAMMAD | Issue Writer Certificate

Keywords

BINALOOD HEIGHTSQ1

GLACIER CIRCUSQ2

QUATERNARY GLACIERSQ1

CLIMATE CHANGEQ2

Abstract

Introduction The effects of CLIMATE CHANGE in the Quaternary period, especially in glacial periods of Iran, is less-known and under- studied. Although there have been some studies on some QUATERNARY GLACIERS in Iran such as Alborz, but no study has to date investigated the East and North East regions of Iran in this regard. Binalud altitudes in the Northeast of Iran are amongst the regions which have the potential for the creation of glaciers and glacial conditions due to an altitude of more than 3000 meters and being located in the pathway of cold Siberian currents, especially in the cold periods of the year.Materials and methods The aim of this study is to identify glacial evidence and determine the permanent snow line of the last Quaternary period in Binalud heights. At first, the border area was determined using 1: 50000 topographic maps. In order to create the current isorain and isothermal maps of the region, the temperature and precipitation data of the stations of Mashhad, Nishaboor, Torogh, Akhlamad, Chenaran, Shandiz, Torqabeh, Kang, Golmakan, Arsalan, Ami Abad, Soltan abad and Chakaneh were used. With the help of this data and the digital elevation model of the area and according to the correlation between elements of temperature, rainfall and altitude, the current isorain and isothermal maps were drawn in the Arc GIS software...

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APA: Copy

GHORBANI SHOORESTANI, ALI, KHOSRAVI, OZRA, & NOURMOHAMMADI, ALIMOHAMMAD. (2016). INVESTIGATING QUATERNARY GLACIAL GEOMORPHOLOGICAL EVIDENCES AT THE NORTHEAST HEIGHTS OF IRAN (CASE STUDY: BINALUD MOUNTAIN RANGES). QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES, 5(1 ), 1-13. SID. https://sid.ir/paper/249023/en

Vancouver: Copy

GHORBANI SHOORESTANI ALI, KHOSRAVI OZRA, NOURMOHAMMADI ALIMOHAMMAD. INVESTIGATING QUATERNARY GLACIAL GEOMORPHOLOGICAL EVIDENCES AT THE NORTHEAST HEIGHTS OF IRAN (CASE STUDY: BINALUD MOUNTAIN RANGES). QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES[Internet]. 2016;5(1 ):1-13. Available from: https://sid.ir/paper/249023/en

IEEE: Copy

ALI GHORBANI SHOORESTANI, OZRA KHOSRAVI, and ALIMOHAMMAD NOURMOHAMMADI, “INVESTIGATING QUATERNARY GLACIAL GEOMORPHOLOGICAL EVIDENCES AT THE NORTHEAST HEIGHTS OF IRAN (CASE STUDY: BINALUD MOUNTAIN RANGES),” QUANTITATIVE GEOMORPHOLOGICAL RESEARCHES, vol. 5, no. 1 , pp. 1–13, 2016, [Online]. Available: https://sid.ir/paper/249023/en

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