Linked from

The 40 pages that link to Endorheic basin, each with the reason it gives.

• Caspian SeaNarrower topic: The Caspian’s closed drainage basin explains its isolation and sensitivity to water-balance changes.

• Iranian PlateauNarrower topic: Many plateau basins have no route to the sea, concentrating salts inland.

• Tarim BasinNarrower topic: The Tarim’s rivers terminate within the landlocked basin.

• AltiplanoNarrower topic: Much of the plateau drains into internal lakes, wetlands, and salt flats.

• Great Salt LakeNarrower topic: The lake has no outlet to the sea, so dissolved salts accumulate as water evaporates.

• Great BasinNarrower topic: This drainage pattern defines the Great Basin’s hydrologic boundary.

• Lake Chad BasinNarrower topic: Lake Chad has no outlet to the ocean, so its basin is endorheic.

• Mexican PlateauNarrower topic: Several plateau basins collect water internally rather than draining directly to the sea.

• Salar de AtacamaNarrower topic: Water and dissolved minerals entering the Atacama basin remain trapped, allowing salts to accumulate.

• Lake TurkanaNarrower topic: The lake has no outlet, so dissolved salts accumulate as water evaporates.

• Lake UrmiaNarrower topic: Lake Urmia’s closed basin concentrates dissolved salts as water evaporates.

• Death ValleyNarrower topic: Water and dissolved salts collect in Death Valley rather than draining seaward.

• SistanNarrower topic: Sistan’s rivers end inland, making water levels sensitive to inflow and evaporation.

• Junggar BasinNarrower topic: Much of the Junggar Basin drains inward rather than to the sea.

• Sistan BasinNarrower topic: The Sistan Basin’s lack of an ocean outlet governs where its water accumulates.

• Issyk-KulNarrower topic: Issyk-Kul’s basin traps incoming water, leaving evaporation as its main natural loss.

• Qinghai LakeNarrower topic: Qinghai Lake retains river inflow rather than draining onward to the ocean.

• Tarim RiverNarrower topic: The Tarim’s water is consumed, evaporated, or stored within the basin.

• Okavango RiverNarrower topic: The river ends in an inland basin, where evaporation and infiltration consume most flow.

• Salt flatNarrower topic: Many salt flats occupy endorheic basins where dissolved minerals accumulate without an outlet.

• Turpan DepressionNarrower topic: Water in the Turpan Depression drains internally or evaporates.

• Chott el DjeridNarrower topic: The lake has no outlet to the sea, so incoming water and dissolved salts remain within its basin.

• Lake BalkhashNarrower topic: Evaporation, rather than an outlet to the sea, removes much of the lake’s water.

• Lake MackayNarrower topic: Lake Mackay lies in an inland basin without a river outlet to the ocean.

• NamtsoNarrower topic: Namtso occupies an inland basin where water leaves mainly through evaporation.

• Continental Divide of the AmericasNarrower topic: Closed basins along the divide reveal exceptions to the usual ocean-bound drainage pattern.

• Dry lakeNarrower topic: Many dry lakes occupy closed basins where inflow has nowhere to drain.

• Turan DepressionNarrower topic: The depression’s rivers terminate in inland lakes, wetlands, and desert sinks.