The general term for that process is erosion.
The process that moves particles from areas of high concentration to areas of lower concentration is called diffusion. During diffusion, particles spread out to achieve an equilibrium, where their concentration is uniform throughout the space. This process occurs naturally and does not require energy input. If the movement involves a selectively permeable membrane, it may also be referred to as facilitated diffusion.
Passive transport that moves particles away from areas is called facilitated diffusion. This process uses transport proteins to help molecules or ions pass through the cell membrane, moving from areas of higher concentration to areas of lower concentration without using energy.
Thermal energy moves from areas of higher temperature to areas of lower temperature through a process called heat transfer. This movement occurs until thermal equilibrium is reached, balancing the temperatures between the two areas.
wind
This process is called diffusion. It occurs spontaneously and is driven by the concentration gradient, where molecules move from an area of higher concentration to an area of lower concentration in order to reach equilibrium. Diffusion is a passive process that does not require energy input.
The process that moves minerals into the B horizon is called illuviation. It involves the movement of dissolved minerals from the A horizon or the topsoil downward into the B horizon or subsoil through the percolation of water.
Air moves from areas of high pressure to areas of low pressure (in order to equalise the pressure). When air moves, it is called wind.
Air moves from areas of high pressure to areas of low pressure (in order to equalise the pressure). When air moves, it is called wind.
when water moves from clouds (high ground) to the low ground it is called rain also known as precipitation.
Winds actually move from areas with higher pressure levels to areas with lower pressure levels, horizontally. Winds actually move from areas with higher pressure levels to areas with lower pressure levels, horizontally.
This process is known as onshore flow. As the cool ocean air moves over the warmer land, it cools the land surface, leading to lower temperatures in coastal areas. Onshore flow can bring fog, mist, and lower humidity levels to the affected regions.
Thermal energy always moves from areas of higher temperature to areas of lower temperature. This transfer of heat occurs through various methods such as conduction, convection, and radiation.