العمليات الجيمورفية الداينميكية المؤثرة في تكوين الأشكال الأرضية في محافظة كربلاء

الملخص EN

This research aims to reveal the nature of the operations in the province of Karbala Almorvodaanmikih and variability and its impact in the formation of landforms where there is close correlation between these operations and the nature of the landforms and contrast.

The research found that these processes clear impact in the formation of landforms in the study area and through the work of wind and running water.

The back of the effect of the wind in the process of erosion is clearly in the desert areas dry with sandy soil and represented in the western parts of them.

Also show that landforms resulting from the process of water erosion to Ataud to the current climate but to the climates in the Middle Ages rain in the with little slope, especially in the northern parts of North and East in the study area.

The deep valleys that descend toward Razaza, as well as in the Euphrates River, where there are a number of formats Altaroah that formed by fluvial erosion.

The process appeared underground water erosion in areas of limestone formations in the western and southern parts of the study area.

The process of sedimentation wind are unclear in the study area in order to flush the surface in general and the lack of Altdhars.

Showed deposition process water in the Euphrates River through river islands formed in its course, and the flood plain in the study area are a result of sedimentation of water over long periods either process material movement of crawling and rock falls and landslides are limited operations are concentrated only in areas of cliffs with steep sever