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Areic Basin, Endorheic Basin and Exorheic Basin

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Diference:

In of a lake or basin|lang=en terms the difference between exorheic and endorheic is that
exorheic is (of a lake or basin) externally drained; having one or more outlets while endorheic is (of
a lake or basin) internally drained; having no outlet.

As adjectives the difference between exorheic and endorheic is that exorheic is (of a lake or basin)
externally drained; having one or more outlets while endorheic is (of a lake or basin) internally
drained; having no outlet.

Areic basin

Finally, the arreic basins are those hydrographic basins whose waters do not flow into seas or
lakes, as they end up evaporating or infiltrating into the ground until they disappear. Generally,
these basins occur in areas where the climates are arid or desert, an example is the basin located
in the Qattara depression, located in the Libyan desert.

Exorheic basin

An exorheic basin is an "open" system of water circulation on the earth's surface, whose main
collecting and draining rivers flow into the sea, i.e. outside the territory. There are seven exorheic
basins in the world, corresponding to the seven major oceanic water masses and two of the
largest seas.

Areic basins are watersheds that do not flow into any body of water, neither into the sea nor into
lakes, as their waters evaporate into the atmosphere or seep into the ground before reaching a
drainage network.

They are less common than exorheic and endorheic basins. Examples include the streams and
watercourses of the central Patagonian plateau, or many streams and runoffs of the Sahara and
other desert areas.

Endorheic basin
An endorheic basin (from Greek ἔνδον, éndon, "within" and Greek ῥεῖν rheîn, "to flow") is a closed
drainage basin that retains water and does not allow its outflow to other external bodies of water,
such as rivers or oceans, but converges into lakes or marshes, permanent or seasonal, which are
balanced by evaporation. These basins may also be called closed or terminal basins or internal
drainage systems.

Normally, water that has accumulated in a drainage basin eventually exits through rivers or
streams at the Earth's surface or by subway diffusion through permeable rocks, eventually ending
up in the oceans. However, in an endorheic basin, the rain (or other precipitation) that falls in it
does not flow out, but can only leave the drainage system by evaporation and seepage. The
bottom of such a basin is usually occupied by a salt lake or a saline.

Endorheic regions, unlike exorheic regions, which drain into the ocean following geologically
defined patterns, are closed hydrological systems. Their surface waters drain to terminal inland
locations, where the water evaporates or seeps into the ground, with no access to discharge into
the sea. Endorheic water bodies include some of the world's largest lakes, such as the Aral Sea and
the Caspian Sea, the world's largest body of saline water isolated from the ocean.

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