Landslides within the Western Ghats and Himalayas range substantially because of modifications in soil, climate and environment. Characterized by complex impure geology, the Western Ghats is in particular liable to landslides in the course of the monsoons while heavy rains motive mountain disasters These landslides are generally shallow, occurring within the the gentle, lateritic soil masking the slopes. The dense flora in this area can stabilize and destabilize slopes; However, the roots maintain the soil together, and the load of cool vegetation can cause slope harm. In assessment, the Himalayas are geologically younger and highly energetic, with frequent earthquake instability. Landslides here are normally deeper and larger, exacerbated through steep terrain and uneven snowpack. Moreover, landslides arise at some point of the yr in the Himalayas because of a aggregate of things inclusive of snowfall, rainfall, human activities including deforestation and street production Climate additionally varies; The Himalayas have a enormously variable weather with extraordinary seasonal modifications, at the same time as the Western Ghats have a regular weather with clean seasonal rainfall This difference leads to extraordinary earthquake intensities and impacts. In summary, whilst rainfall-caused shallow landslides due to monsoons and lateritic soils are not unusual in the Western Ghats, deep landslides are extra frequent caused by seismic pastime, fall apart of atmospheric conditions types and slopes inside the Himalayas form and trigger earthquakes function of these provinces.