The word torrent is a term used in geography since it refers to that watercourse that comes from a mountain. The notion of torrent always assumes that this watercourse has a rapid flow precisely because the rivers and streams that are formed from the mountain melt reach the valleys and even the sea with a force and speed greater than that of other watercourses. Water. In other respects, the term torrent can also refer to the bloodstream or other fluids that are in constant motion and that have a certain speed and strength.
The notion of torrent is related to hydrography since we are talking about a water course that takes place in the environment. These water courses or torrents are usually generated from the meltwater that is formed with the melting of the snow from the mountains and it is thus that from the highest place until it reaches its connection with a lake or sea, the torrent acquires great strength. This is due to the force of gravity as well as the constant flow of water that prevents the torrent from losing force or movement.
The torrents, as might be expected, cause strong erosion on those surfaces through which they circulate due to their strength and speed. Thus, it is normal to find that streams or rivers generated by the thaw leave large and deep furrows in the valleys through which they cross. Many of them even erode the mountain, changing its surface.
There are three parts in which a torrent can be divided: the place of accumulation of the water, when it is not yet in motion, the drainage channel where the water acquires more and more speed and the dejection cone, where it ends its path and where all the sediments that the water carried with it are left.
