Slope stabilization is the process of implementing measures to prevent the failure of slopes or embankments, ensuring their long-term stability. There are two main factors that contribute to slope destabilization: natural and man-induced. Natural factors include slope failure caused by rainfall, seismic events, and weathering over time due to climatic conditions. Excessive rainfall can erode or infiltrate water into the slope, weakening its structure, while seismic events, such as earthquakes, can cause shaking that leads to landslides or slope failure.