Mapping of biological corridors
Introduction
A river is a stream of water that flows continuously through a channel, either on the earth's surface or underground, and can be both natural and artificial.
It has a certain flow "Flow (fluid)"), it is rarely constant throughout the year, and it flows into the sea, a lake or another river,[1] in which case it is called a tributary. The final part of a river is its mouth. Sometimes they end up in desert areas where their waters are lost through infiltration and evaporation (see allochthonous river).
Rivers are part of the hydrological cycle. Water generally accumulates in a river from precipitation "Precipitation (meteorology)") across a watershed from surface runoff and other sources such as groundwater recharge, springs, and the release of water stored in natural ice and snow layers. For what belongs to or relates to a river, the adjective "fluvial" is used.[2].
The sum of the water from all the planet's rivers and their reservoirs represents around 0.01% of the total water on earth.[3].
Etymology
This word comes from the Latin «rivus», which means "stream" or "river".[4].
Topography
Contenido
Por lo general los ríos, especialmente los más grandes, se dividen en tres partes principales de acuerdo con su capacidad erosiva y de transporte de sedimentos:.
high course
The upper course of a river is where they are born. It generally coincides with the mountainous areas of a given basin. Here the erosive potential is much greater and the rivers usually form V-shaped valleys as they fit into the relief. When this part of a river is in a dry climate they may sometimes be called ravines "Barranco (geography)"), ramblas "Rambla (geomorphology)") or torrents "Torrente (hydrography)").[5][6].
medium course
Generally, in the middle course of a river, some of the areas or zones where the river erodes and where it deposits part of its sediments tend to alternate, which is mainly due to fluctuations in the slope and the influence they receive with respect to the flow and sediments of their tributaries. Along the middle course, the cross section of the river will usually soften, taking on a sectioned lever shape instead of the V shape that prevails in the upper course.