Özet:

The area of research covers the Özalp district and its surroundings connected to the Van province in the east of Turkey. Saha is also within the closed pool of Lake Van and is neighboring to Iran. The aim of this study is to explain the geomorphological characteristics of the area that has not previously been studied from a geographical point of view. In the study, land observations and works, satellite images and photographs, were taken advantage of a variety of maps. In acquiring the geomorphological characteristics of the area today, geological characteristics are in the forefront. In addition, different geomorphological elements are identified in the field where fluvial processes are effective. These are the mountainous and mountainous areas that equal to the high surface of stretching, the back and the mountains, the valleys, the accumulation coins, the throats and the oval field. In the field, from paleozoos to today, there are stones of various ages, which have been greatly influenced by tectonism. The main flow of the field is the D-B axis stretching Özalp Tea. There are many side arms involved in the K-G directions. This area is compatible with the main stream and lies in the D-B axis. At certain times, due to the rain and snow eruptions, water strikes may occur due to the flow of the main coal through the side arms. This is a morphological way of spreading the forms of the forms. It is a place where the weather is severe. But in recent years the climate change that has affected the world can be said that the drying of surface/subterranean water resources as a quality in the field of research sometimes appears in the form of sudden water attacks, changing both the morphological structure and threatening the existing settlements on morphology. Therefore, it is recommended not to establish settlements in the mouth areas, especially in the nearby areas of the Özalp Tea and in the main parts of the mouth where the side arms are connected to the main coal.

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