erosion
Erosion.
Glaciers move very slowly.
sedimentary rock
Sedimentary rock is formed from sediments are piled on top of one another, then compacted and cemented into rocks. Sandstone and limestone are examples of sedimentary rocks.
The mutual forces of gravitational attraction between a glacier and the Earth cause the glacier to slowly 'flow' downhill. Also, if any of the ice should melt underneath the glacier, then the resulting liquid water flows similarly downhill, although faster than the ice does.
The process in which sediments move slowly downhill, is called creep. It is common where freezing and thawing occur. As ice expands in soil, it pushed sediments up. Then as soil thaws, the sediments move farther downslope. Over time, creep can move large amounts of sediment, possibly causing damage to some structures
creep
Erosion.
Erosion. More specifically in soils this is likely to be creep or solifluction. These are types of mass wasting.
Pressure of water and other sediments.
If you put a rock on a hill, the gravity of the ground will slowly make it move downhill.
Erosion
Glaciers move very slowly.
Erosion
try going slowly on it
sediments are transported by ocean rift, streams, river currents, wind (air). they are deposited according to size. The largest sediments are deposited first. The sediments settle into the sand and are carried by the stream. Near the mouth of the stream where the water moves slowly the small sediments settle out. The larger sediments get carried by the river into the sea then the samller sediments. The sea water dissolved minerals and soak the sediments and cement together. This eventually forms sediments.
sedimentary rock