Soil erosion is defined as the detachment, transportation, and deposition of soil particles by forces like water, wind, waves, and gravity. There are three main steps: 1) detachment of soil particles from the main body, 2) transportation by splashing, floating, or rolling, and 3) deposition in another place. Geological erosion refers to natural erosion caused by water, wind, gravity, and glaciers, while accelerated erosion exceeds the normal rate and becomes destructive due to factors like climate, topography, soil characteristics, ground cover, and land use. The Universal Soil Loss Equation is used to estimate soil and water erosion and considers rainfall, soil erodibility, slope length, slope gradient, crop management,