It is often driven by the action of water in promoting liquefaction and pushing a given material beyond its angle of repose, especially in loose soil.
Evidence of it can be seen in material referred to collectively as talus, and examples include lahars and solifluction. It is often driven by the action of water in promoting liquefaction and pushing a given material beyond its angle of repose, especially in loose soil. When upper-layer regolith moves faster than the soil beneath it, creep occurs, which is much slower than processes like slump or rock falls. For 10 points, name this consequence of weathering and important part of erosion, defined as the downhill motion of rock or soil under the influence of gravity.
Evidence of it can be seen in material referred to collectively as talus, and examples include lahars and solifluction.
{mass wasting}