Plant roots bind the soil and regolith together.
vegetation
gravity
its is when something happens on soil
mudslide
mudflows slump creep landslides
One factor that does not commonly trigger mass movement is vegetation cover. In fact, vegetation can help stabilize slopes and reduce the likelihood of mass movement by absorbing water and providing root strength to hold soil in place.
Individuals walking does not usually trigger mass movement. Mass movements are typically triggered by natural events such as heavy rainfall, earthquakes, volcanic eruptions, or human activities like deforestation and construction.
Saturation of surface materials with water, over steepening of slopes, removal of vegetation, and earthquakes. water
Mass movement
Events that do not typically trigger mass movements include minor policy changes, individual scandals, or isolated incidents that do not resonate with a large portion of the population. Movements usually require a broader issue or grievance that affects a significant portion of society to gain momentum.
The removal of vegetation does away with the roots of plants. Roots tend to hold soil together, without them soil becomes more loose and is more easily moved by other forces such as wind and water.Edited answer:The removal of vegetation by fire converts all organic matter into inorganic gases and solid waste, the logging removes the wood from that place, which again amounts reduction in organic mass. Thus, both these process promote organic mass wasting.
The water content of the soil on a hillside is most likely to trigger a mass movement during heavy rainfall or after a period of prolonged precipitation. This increased water saturation can weaken the soil structure, causing it to become unstable and potentially lead to a landslide or mudslide. Factors such as steepness of the slope, soil composition, and vegetation cover also play a role in determining when a mass movement might occur.
Water can trigger mass movements such as landslides by infiltrating into the ground and reducing the friction between soil particles. This can increase the weight of the soil above and make it unstable, leading to the movement of material down a slope. Additionally, water can increase pore water pressure within the soil, further reducing the effective stress and making it easier for material to move.
Mass movement refers to the movement of surface material due to gravity. Other factors that can trigger mass movement are deforestation, saturation of surface materials with water, earthquakes and flash floods.
Gravity is the force behind mass movements like landslides and rockfalls. Other factors that can trigger mass movements include heavy rainfall, earthquakes, volcanic activity, human activities like construction or deforestation, and changes in slope stability due to erosion or weathering.
Mass movements occur when gravity acts on a large amount of material on a slope, causing it to move downhill. Factors such as steepness of the slope, type of material, amount of water content, and vegetation cover can trigger mass movements like landslides, rockfalls, or debris flows. Once the material becomes unstable and the resisting forces are overcome by gravity, a mass movement occurs.
When the soil is fully soaked with water, such as after heavy rains