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
The agents of erosion are: running water, glaciers, waves, and wind. # I would say that wind is the top agent of erosion that is assisted by gravity because gravity pulls down the sediments that the wind is eroding. # Running water is probably the second because gravity is the force that moves rock and other materials downhill, so if running water is moving downhill, gravity helps it. # Finally, glaciers is another agent assisted by gravity because glaciers also move downhill taking down eroded sediment with it.
Freezing does kill the bacteria because it freezes the cell movement. Bacteria has to maintain in movement to stay alive. Also when it freezes, it shatters easily. This kills the bacteria almost immediately.
Wind and water can carry sediments because of their energy and movement. As they flow, they can pick up sediments from the ground and transport them to new locations. When their speed decreases, they drop these sediments, leading to their deposition.
because you have a friend right here
A slump mass movement is typically faster than a creep mass movement. Slump movement involves a more sudden and rapid downslope movement of material, often in a rotational manner, whereas creep movement involves a slower, more gradual flow of material over time.
Your mother because after i finish inside her the pressure builds up and sends her downhill
In the desert, there are few plants, and those plants that do grow have shallow root systems. This lack of plant cover leaves the desert vulnerable to erosion by water because there is very little holding the sediment together. This means that when the sediments become impregnated with water, they are more likely to break away from lower sediments and slide downhill (a landslide). Additionally, this lack of plant material to hold sediments in place enables water to quickly sweep sediments away.
Creep is a slow, continuous mass movement of soil or rock down a slope. It involves a gradual downhill movement of materials due to the force of gravity. It is not considered a rapid mass movement like landslides or debris flows.
Water is colorless because there are no sediments to give the water color. Sea water has color because there are alot of sediments
The overall process is called Solifluction. If you imagine single particle (in the soil) on a gentle slope. When the water in the soil freezes, it expands and forces the particle away from the slope at right angles to the slope. When the ice then thaws gravity will cause the particle to settle back but the movement will be in a downwards direction, not in the direction it first moved. Add this movement together, repeate season after season and the particle gradually moves down slope.
because sediments has sand in it