It can be called a landslide.
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A landslide can rush downhill as a huge mass of soil, rocks, and other debris due to the force of gravity overcoming the stability of the slope. Landslides can be triggered by heavy rainfall, earthquakes, volcanic eruptions, or human activities that weaken the slope's integrity.
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.