The eastern part of the region contains several small endorheic basins.

The surrounding catchment is an endorheic basin with no outlet.

The grey areas are endorheic basins that do not drain to the ocean.

New Mexico has a number of desert endorheic basins including:

Endorheic basins usually end in a saline lake or a salt flat.

Other lakes are found in endorheic basins or along the courses of mature rivers.

Any water within an endorheic basin leaves the system only through evaporation or seepage.

Lake Pátzcuaro lies in an endorheic basin, which does not drain to the sea.

Inside the "V" are a number of endorheic basins.

The endorheic basin of Lake Pátzcuaro lies to the west.

Most of Kazakhstan is endorheic basin (except northern territories).

Discharging to an endorheic basin, the Okavango does not have an outlet to the sea.

Aksai Chin area has number of endorheic basins with many soda lakes.

It is an endorheic basin, which means that the rivers in it do not flow to the sea.

When the outflow is completely prevented, this is called an 'endorheic basin'.

Saline Valley is a closed or endorheic basin.

A geographic sink is a depression within an endorheic basin where water collects with no visible outlet.

Most of the northern valley is an endorheic basin called the Closed Basin.

Both permanent and seasonal endorheic lakes can form in endorheic basins.

See also List of endorheic basins.

Some endorheic basins are essentially stable, climate change having reduced precipitation to the degree that a lake no longer forms.

In addition, due to its location within a series of endorheic basins, none of its rivers lead to the sea.

Since it formed in an endorheic basin lake, Lake Texcoco was brackish.

The Llanos el Salado is a large endorheic basin of central Mexico.

Other intermittent lakes are only the result of above-average precipitation in a closed, or endorheic basin, usually filling dry lake beds.