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Physical Process

Endorheic Basin Formation

Hydrological and Oceanic Processes

The development of a drainage basin whose water has no outlet to the ocean, instead collecting in an interior lake, marsh or salt flat and leaving the system only through evaporation and infiltration, typically forming in arid regions where a basin is enclosed by surrounding high ground or where regional aridity prevents any stream from carrying enough flow to reach the sea. Endorheic basins, including those draining to the Caspian Sea, the Great Salt Lake and much of Central Asia and the American Great Basin, are often highly sensitive to changes in regional precipitation and upstream water use, since their water balance has no ocean outlet to buffer it.

Facts
Timescale
Timescale (category)
Thousands of Years 1
Process Type
Hydrological 2
Connections

Caused By

Shaped

Source Caspian Sea (Wikipedia)
Sources
1. Endorheic basin (Wikipedia)
Wikipedia infobox 'Lead section' = 'An endorheic basin ( EN-doh-REE-ik; also endoreic basin and endorre...' on 'Endorheic basin'View the Source
2. Endorheic Basin Formation (Wikipedia)
Wikimedia FoundationLead section
Quote, Lead section
An endorheic basin ( EN-doh-REE-ik; also endoreic basin and endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water (such as rivers and oceans). Instead, the water drainage flows into permanent and seasonal lakes and swamps that equilibrate through evaporation.
View the Source
Caspian Sea (Wikipedia)
Wikimedia FoundationShaped: The Caspian Sea, Formation statement for target 296213
Quote, Shaped: The Caspian Sea, Formation statement for target 296213
An endorheic basin, it is situated in both Europe and Asia: east of the Caucasus, west of the broad steppe of Central Asia, south of the fertile plains of Southern Russia in Eastern Europe, and north of the mountainous Iranian Plateau.
View the Source
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