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it is called a current
The movement of water in a river is a non-example of mass wasting. Mass wasting involves the downslope movement of rock and soil due to gravity, while the movement of water in a river is governed by the flow of the water itself.
A mass movement that requires water to be present is a debris flow. This occurs when water mixes with loose debris, such as soil and rocks, creating a fast-moving mixture that flows downhill. Water acts as a lubricant in debris flows, increasing the speed and destructive force of the movement.
The movement of a large mass of sediment or a section of land down a slope is called mass wasting or mass movement. This process can be triggered by factors such as gravity, water saturation, or seismic activity. It can result in landslides, mudslides, or rockfalls.
The mass of water used in the first six minutes depends on the rate of flow of water. If we know the flow rate, we can calculate the mass using the formula: Mass = flow rate x time.
This type of mass movement is called a debris flow. It is a rapid flow of saturated, unconsolidated material (such as soil, rock, and water) down a steep slope. Debris flows can be triggered by heavy rainfall, rapid snowmelt, or earthquakes.
Groundwater flow.
current
current?
Through flow is the horizontal movement of water through the soil zone. Groundwater flow is the movement of water through the bedrock, which is typically an aquifer
When mud is involved in a mass movement it behaves as a liquid, flowing downhill and looking rather like a muddy flood.
The mass movement of surface water is typically referred to as runoff, which is the flow of water over land surfaces towards rivers, lakes, and oceans. This movement can occur due to rainfall, snowmelt, or other forms of precipitation. Runoff plays a crucial role in the water cycle and can contribute to erosion and sediment transport.