A landslide can rush downhill as a huge mass of soil, water, and rock, leaving a bare scar in the hillside. Landslides can be triggered by heavy rainfall, earthquakes, volcanic eruptions, or human activities like deforestation or mining. They can cause significant damage to infrastructure and pose risks to human safety.
This form of erosion is referred to as mass wasting or mass movement. It occurs when gravity pulls loose rock and soil downhill, causing landslides, rockfalls, and slumps.
Creep is the slowest type of mass wasting, where soil and rock move downhill imperceptibly slowly due to gravity. This gradual movement can be observed through the tilting of fences, trees, or other structures over time.
The slow downhill mass movement of rock and soil caused by gravity is called creep. This gradual movement occurs over time, resulting in the slow shifting of materials downslope. Creep is one of the most common types of mass wasting processes.
The downhill mass movement of rocks or soil due to gravity is called a landslide. It can be triggered by factors such as heavy rainfall, earthquakes, or human activities that destabilize the slope. Landslides can cause significant damage to infrastructure and pose a threat to human life.
mudslide
A landslide can rush downhill as a huge mass of soil, water, and rock, leaving a bare scar in the hillside. Landslides can be triggered by heavy rainfall, earthquakes, volcanic eruptions, or human activities like deforestation or mining. They can cause significant damage to infrastructure and pose risks to human safety.
This form of erosion is referred to as mass wasting or mass movement. It occurs when gravity pulls loose rock and soil downhill, causing landslides, rockfalls, and slumps.
This is known as a landslide.
Creep is the slowest type of mass wasting, where soil and rock move downhill imperceptibly slowly due to gravity. This gradual movement can be observed through the tilting of fences, trees, or other structures over time.
The slow downhill mass movement of rock and soil caused by gravity is called creep. This gradual movement occurs over time, resulting in the slow shifting of materials downslope. Creep is one of the most common types of mass wasting processes.
Erosion. More specifically in soils this is likely to be creep or solifluction. These are types of mass wasting.
air and soil if you havy any comment find me at hkedash@yahoo.com
The downhill mass movement of rocks or soil due to gravity is called a landslide. It can be triggered by factors such as heavy rainfall, earthquakes, or human activities that destabilize the slope. Landslides can cause significant damage to infrastructure and pose a threat to human life.
The downhill movement of rock or soil is called erosion. Erosion can be caused by natural processes like water flow, wind, glaciers, and gravity. It can also be accelerated by human activities such as deforestation and construction.
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.
Mass movement (also known as mass wasting) can be any of four types of motions :creep (objects lean downhill over many years)slump (rock and soil slip down a hill in one large mass)slides (landslides : rock and soil slide downhill)flows (mudslides and mudflows: rock and soil mixed with water slides downhill)Under some definitions, there are two other types, which do not involve "flows" of material. They are :topples (rock pivots off a slope)falls (rock separates and falls without flowing)