Geomorphological processes are considered one of the most important mean that have a significant role in the emergence and change of topography, and based on the reason for their emergence; these processes can be divided into some sorts of processes such as morpho tectonic, morpho climatic, morpho kinetic. In this study, we focus on morpho climatic processes that have a major role in the change of terrain and the emergence of new topography in the Bemo region. This is done with the help of all branches of the weathering process (mechanical weathering, chemical weathering, biological weathering), and erosion factors in all its branches (raindrop erosion, running water erosion, wind erosion), with the exception of sedimentation factors (aquatic and aerobic precipitation). To show the impact of climatic Morpho processes on the development of landforms in the Bemo region, which is the main objective of the study, the study was divided into an introduction and three main axes, and for this analytical methods were used. In conclusion, the results of weathering and erosion processes in the study area were presented, and based on the results, the study included some suggestions.
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