جۆری توێژینهوه : Original Article
نوسهران
1 بەشی جوگرافیا، کۆلێژی پهروهرده، زانکۆی گهرمیان، هەرێمی کوردستان – عێراق
2 بەشی زانسته کۆمهڵایهتیهکان، کۆلێژی پهروهردەی بنەڕەت، زانکۆی گهرمیان، هەرێمی کوردستان – عێراق
وشه بنچینهییهكان
ناونیشانی توێژینهوه English
نوسهران English
This research entitled (gully erosion from BawShaswar basin) (A Study of Climate Geomorphology) is a research related to both climate and geomorphology, because climate is the most important factor The occurrence of external geomorphological processes, and climate species play an important role in the amount of erosion, either directly or indirectly. The aim of this study is to determine the strength & size of the gully erosion and its spatial differences in the BawShaswar basin, using aerial images (landsat Dem 30m) program (10.5Arc Gis), while studying and identifying the factors contributing to the increase Presence of central erosion size. The area of BawShaswar basin is (303.60) km2 In terms of tectonic conditions, it is located in the unstable edge area that is part of the Arabian-African plate, in the zone of pegs, the study concluded that, in general, the basin falls within it More precisely, the minimum area of the reservoir (13.57%) falls within the framework of very little water removal While the maximum area of the watershed (86.43%) falls within the framework of central removal and high removal, because each of the factors (climate, natural vegetation, salinity degree and direction of salinity, geological structure) contribute to Large amount of candy removal in the water tank. Large amounts of removal have affected the soil in terms of soil degradation and the formation of nuclei and soil shrinkage, as well as weakening the soil capacity by washing away the soil and transporting some of its minerals
وشه بنچینهییهكان English
