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Nilanjan Bhowmick AIR 3, CSIR NET (Earth Science)
Mayank Mishra
Soil Creeping: Soil creeping is a slow downhill movement of soil, typically occurring on gentle slopes over an extended period of time. It is caused by the force of gravity, which pulls soil particles and rocks downslope. Soil creeping can occur due to various factors, including the presence of water or ice, changes in temperature, or the removal of vegetation that holds the soil in place. During soil creeping, the upper layer of soil gradually moves downslope in a series of small steps, with the soil particles at the base of the slope being compacted and compressed. This can cause the soil to become denser and more resistant to further movement. However, over time, the soil will continue to move, resulting in a slow but steady downslope flow. Soil creeping can have significant impacts on the landscape and can cause damage to structures or infrastructure built on or near the affected slope. Understanding the causes and mechanisms of soil creeping is important for mitigating its effects and protecting vulnerable areas from damage.