It doesnt fack you
fall
Downhill shifting of rocks and soil due to gravity is called mass wasting. It occurs when the force of gravity overcomes the strength of the slope material, causing it to move downwards. Factors such as slope angle, water content, and vegetation cover can influence the occurrence and speed of mass wasting events.
Gravity is the main factor that causes a rockslide. However, water can also contribute by lubricating rock layers and reducing friction, making a slope more prone to sliding. Wind alone typically does not cause rockslides, but it can indirectly impact the stability of a slope by eroding or destabilizing the rocks.
Maybe the slope went slower because of the water went slower
heavy rains combined with loss of vegetation due to wildfires trigger ... Although the term landslide is often used somewhat loosely to mean any fairly rapid ... What Kinds Of Mass Wasting Processes Do We See? ... Such falls can be triggered by freezing of water, the growth of plants
Slope Gradient
Mass wasting or mass movement refers to the movement of rock debris down a slope due to the influence of gravity. The movement is induced by natural factors or by human interferance on hill slope. The movement can be slow or fast.
Factors that affect the stability of a slope include the slope gradient, type of soil or rock, presence of water or groundwater, vegetation cover, weather conditions, and human activities like construction or excavation. Steeper slopes, loose or weak soil, heavy rainfall, and disturbances like deforestation or construction can all increase the risk of slope instability and potential landslides.
The addition of water can decrease the stability of a slope by increasing pore water pressure, reducing the effective stress between soil particles, and decreasing the shear strength of the soil. This can lead to slope failure through processes such as landslides or soil erosion.
Several factors can affect a slope, including the composition and stability of the soil and rock materials, moisture levels, vegetation cover, and human activities such as construction or deforestation. Additionally, weather events like heavy rainfall or earthquakes can trigger landslides or erosion, further impacting slope stability. The angle of the slope itself also plays a crucial role, as steeper slopes are generally more susceptible to failure.
fall
I believe It changes the affect on the earth's surface, for an example: Dry sand grains are bound mainly by friction with one another. Small amounts of water increase the cohesion among sand grains. Saturation reduces friction and causes the sand to flow.
This process is called mass wasting or mass movement. It involves the movement of soil, rock, and debris down a slope under the influence of gravity. Factors such as steepness of the slope, type of material, and presence of water can affect the rate and type of mass wasting that occurs.
The force of gravity causes mass wasting to occur faster.
Erosion can weaken the base of a slope, making it more susceptible to mass wasting events such as landslides or rockfalls. By stripping away supporting material, erosion can increase the likelihood of slope failure. Additionally, erosion can transport material downslope, contributing to the accumulation of debris at the base of the slope and potentially triggering mass wasting.
When the gravitational force acting on a slope exceeds its resisting force, slope failure (mass wasting) occurs. The slope material's strength and cohesion and the amount of internal friction between material help maintain the slope's stability and are known collectively as the slope's shear strength. The steepest angle that a cohesionless slope can maintain without losing its stability is known as its angle of repose. When a slope possesses this angle, its shear strength perfectly counterbalances the force of gravity acting upon it. Mass wasting may occur at a very slow rate, particularly in areas that are very dry or those areas that receive sufficient rainfall such that vegetation has stabilised the surface. It may also occur at very high speed, such as in rock slides or landslides, with disastrous consequences, both immediate and delayed, e.g., resulting from the formation of landslide dams. Factors that change the potential of mass wasting include: change in slope angle; weakening of material by weathering; increased water content; changes in vegetation cover; and overloading.
Gravity, geological age, and slope angel