MECHANISM OF GEOMORPHOLOGIC CREATION AND DEVELOPMENT OF GULLY IN THE WINTER-QUARTER OF HAJ MOHAMMAD IN THE NORTHERN SLOPE OF KHOROSLU IN ARDEBIL

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MOGHIMI EBRAHIM; SALAMI NIKZAD

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Paper Information

Journal: GEOGRAPHICAL JOURNAL OF TERRITORY Year:2011 | Volume:8 | Issue:30 Page(s): 49-61

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Title

MECHANISM OF GEOMORPHOLOGIC CREATION AND DEVELOPMENT OF GULLY IN THE WINTER-QUARTER OF HAJ MOHAMMAD IN THE NORTHERN SLOPE OF KHOROSLU IN ARDEBIL

Author(s)

MOGHIMI EBRAHIM | SALAMI NIKZAD | Issue Writer Certificate

Keywords

GULLYQ2

GEOMORPHOLOGYQ2

ORIGINAL ELEMENTSQ2

DEVELOPMENTQ2

KHORUSLUQ2

Abstract

Duo to the status quo and capability of eradication with respect to lithology, pedology and topography, the northern part of Khoroslu region has but an extreme potential of GULLY erosion regarding to mass movements such as slip, slide, etc. for its unstable soil. Because of Soil erosion and degradation in this region a large amount of cultivatable soil is in danger. Nevertheless it is of great significance to study and scrutinize the important factors in creation and DEVELOPMENT of gullies in the region.In evaluating the origin and features of GULLY creation and DEVELOPMENT the role of topographic and morphogenesis elements is regarded. According to examinations on the studied region, slope, height, difference and existing materials have been known as the most important factors in GULLY creation and DEVELOPMENT. In this research 29 active gullies regarding geomorphologic features are selected. Length, depth, width and height of the gullies as well as the height of their slope is determined and the data are analyzed by means of Excel Spss software. The result shows that 0.1% of the changes in gullies is because of changes in length which compared to the height changes is less effective. So the increase in height raises the slope and the congestion of soil then the DEVELOPMENT of gullies is reduced. Finally the long and deep gullies in higher slope areas are less common compared to lower slope.

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References

CHARACTERISTICS AND CONTROLLING FACTORS OF GULLY EROSION (CASE STUDY: LIMITED BETWEEN AHAR-MESHKINSHAHR)

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APA: Copy

MOGHIMI, EBRAHIM, & SALAMI, NIKZAD. (2011). MECHANISM OF GEOMORPHOLOGIC CREATION AND DEVELOPMENT OF GULLY IN THE WINTER-QUARTER OF HAJ MOHAMMAD IN THE NORTHERN SLOPE OF KHOROSLU IN ARDEBIL. GEOGRAPHICAL JOURNAL OF TERRITORY, 8(30), 49-61. SID. https://sid.ir/paper/116372/en

Vancouver: Copy

MOGHIMI EBRAHIM, SALAMI NIKZAD. MECHANISM OF GEOMORPHOLOGIC CREATION AND DEVELOPMENT OF GULLY IN THE WINTER-QUARTER OF HAJ MOHAMMAD IN THE NORTHERN SLOPE OF KHOROSLU IN ARDEBIL. GEOGRAPHICAL JOURNAL OF TERRITORY[Internet]. 2011;8(30):49-61. Available from: https://sid.ir/paper/116372/en

IEEE: Copy

EBRAHIM MOGHIMI, and NIKZAD SALAMI, “MECHANISM OF GEOMORPHOLOGIC CREATION AND DEVELOPMENT OF GULLY IN THE WINTER-QUARTER OF HAJ MOHAMMAD IN THE NORTHERN SLOPE OF KHOROSLU IN ARDEBIL,” GEOGRAPHICAL JOURNAL OF TERRITORY, vol. 8, no. 30, pp. 49–61, 2011, [Online]. Available: https://sid.ir/paper/116372/en

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