THE MORPHOLOGICAL INFLUENCE OF THE SLOPES IN EVOLUTION OF THE GLACIER CIRCUSES IN OSHTORANKUH

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MOGHIMI E.; YARAHMADI A.M.; SERVATI M.R.; KARDAVANI P.

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Journal: Journal of Spatial Planning Year:2012 | Volume:16 | Issue:3 (75) Page(s): 119-139

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Title

THE MORPHOLOGICAL INFLUENCE OF THE SLOPES IN EVOLUTION OF THE GLACIER CIRCUSES IN OSHTORANKUH

Author(s)

MOGHIMI E. | YARAHMADI A.M. | SERVATI M.R. | KARDAVANI P. | Issue Writer Certificate

Keywords

MORPHOLOGYQ2

GLACIER CIRCUSQ2

GLACIERQ2

OSHTORANKUHQ2

Abstract

The presence of the GLACIER forms in the mountains indicates the function of the GLACIER processes in developing of the earth surface forms. One of them is GLACIER CIRCUS/fa?page=1&sort=1&ftyp=all&fgrp=all&fyrs=all" target="_blank"> GLACIER CIRCUSes.The subject matter of this research is the circuses formation on the slopes of OSHTORANKUH and the differences between the evolution and development degrees influenced by the MORPHOLOGY of the slopes.The raw data were provided by using of the ETM+ images, aerial pictures, geological and topographical maps and field study. Then, was processed in Google Earth, ARC GIS, Auto Cad and Erdas Imaging Software and as results the necessary information were obtained.The analyzing method of this research is correlation and the data was analyzed by using SPSS Software and calculating correlation and regression. It was proved that there is highest correlation with evolution of circuses in the southern slope (18 circuses) which arc related to the directional variables. (The azimuth of the western crest of circuses is-0.71, Talweg azimuth -0.63 and the height of main peak 0.63). While the effective factors in the northern slope (24 circuses) are mainly altitude variables (The average height of the western axle 0.74, the average height of the eastern axle 0.65, the height of the main peak 0.64). The analysis of regression determines “the average height of the western crest” in the northern slopes and “the western crest azimuth of circuses” in thesouthern slopes as the evolution factors. The above relations are because of the influence of the MORPHOLOGY of the slopes.

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APA: Copy

MOGHIMI, E., YARAHMADI, A.M., SERVATI, M.R., & KARDAVANI, P.. (2012). THE MORPHOLOGICAL INFLUENCE OF THE SLOPES IN EVOLUTION OF THE GLACIER CIRCUSES IN OSHTORANKUH. SPATIAL PLANNING (MODARES HUMAN SCIENCES), 16(3 (75)), 119-139. SID. https://sid.ir/paper/171915/en

Vancouver: Copy

MOGHIMI E., YARAHMADI A.M., SERVATI M.R., KARDAVANI P.. THE MORPHOLOGICAL INFLUENCE OF THE SLOPES IN EVOLUTION OF THE GLACIER CIRCUSES IN OSHTORANKUH. SPATIAL PLANNING (MODARES HUMAN SCIENCES)[Internet]. 2012;16(3 (75)):119-139. Available from: https://sid.ir/paper/171915/en

IEEE: Copy

E. MOGHIMI, A.M. YARAHMADI, M.R. SERVATI, and P. KARDAVANI, “THE MORPHOLOGICAL INFLUENCE OF THE SLOPES IN EVOLUTION OF THE GLACIER CIRCUSES IN OSHTORANKUH,” SPATIAL PLANNING (MODARES HUMAN SCIENCES), vol. 16, no. 3 (75), pp. 119–139, 2012, [Online]. Available: https://sid.ir/paper/171915/en

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