Abstract
AbstractLandslides are ranked third after earthquakes and floods in terms of material loss of life and damage to loose formations. This sliding phenomenon is prevalent in the Mila basin, particularly the northeastern part of Oued El-Kebir and Rhumel. It is established that landslides are caused by the spatiotemporal conjunction of several factors. These factors may be quasi-static variables such as geology, geomorphology and geotechnical characteristics of the site, or dynamic variables such as precipitation, earthquakes and anthropogenic activities. The present work is a hydrological and geotechnical geological study aiming to propose effective solutions and to determine areas with high potential for instability.KeywordsMila BasinLandslidesProposed solutions
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