Generally, these processes are referred to as transportation, the movement of sediment during erosion, via wind, ice, or water.
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Processes caused by gravity that move sediment downhill include mass wasting events such as landslides, rockfalls, and slumps. Gravity pulls the sediment downslope, overcoming the strength of the materials holding it in place. These processes can be triggered by factors such as heavy rainfall, earthquakes, or human activities.
Mass wasting includes several processes caused by gravity that move sediment downhill, such as landslides, mudslides, rockfalls, and creep. These processes are driven by the force of gravity acting on slopes and can be triggered by factors like heavy rainfall, earthquakes, or human activities.
Mass movements caused by gravity are known as gravity-driven movements and include landslides, rockfalls, and debris flows. Glaciers cause mass movements through glacial erosion, where ice movement transports sediment downhill, leading to processes like rockslides and moraine collapses.
Agents of erosion caused in part by the force of gravity include mass wasting processes such as landslides, rockfalls, and slumps. Gravity acts as a driving force for these processes by pulling loose material downhill.
Erosion caused by gravity, also known as gravitational erosion, occurs when the force of gravity pulls materials downslope, causing them to be transported and eroded. Examples include rockfalls, landslides, and creep. Over time, these processes can shape landscapes and contribute to the movement of sediment and soil.
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.