أثر العمليات المورفومناخية على الانحدارات الأرضية في قضاء شقلاوة

الملخص EN

The study concluded that carbonization is a supporting processes in most of the lime rock in Shaqlawa.

Most of the karst shapes and caves in the field of the study were formed by the carbonization process particularly within the milieu of the declivities.

However, most of the melting processes depend on the type of rocks and their geological texture in addition to the gradient and the features of the qualitative water that affect the metals of the rocks.

The results of the melting processes are represented by the small gaps and digs and also by caves and Bogaz, the Karren in separated places in Shaqlawa.

As for the erosion processes, there are72 locations empty of any water streams these locations are located in places in which the gradient is a semi nonexistent.

They are distributed separately in the area of the study while the slight erosion has about 651 water streams places.

Accordingly the area of the slight erosion is(446.49 square k.

m.

) out of the total area.

The level of erosion is between( 6◌-0◌) and there is no intensive erosion I, of about (7◌), in the field of the study.

They are located in separated places in the field of the study especially in the semi plane places, in the southern and west southern parts and also the northern and the west northern parts and some parts in Balessan in the east and the north eastern parts in ShaqlawaMorphoclimatic Process, Geographic Information System(GIS), Remote Sensing(RS)