A bowl-shaped drainage basin (endhoreic or closed basin) collects water but has no outlet to the ocean. Instead of flowing seaward, water accumulates in a terminal lake, playa, or salt flat, where it evaporates. This process leaves behind dissolved minerals—salts, carbonates, borates—creating saline or hypersaline environments like the Dead Sea, Great Salt Lake, Lake Eyre, or the Salar de Uyuni.
Key characteristics:
If an outlet exists (even intermittent), the basin is exorheic and water eventually reaches the ocean. True endorheic basins cover ~18% of Earth's land surface, mostly in arid/semi-arid regions. They are geological traps where water's journey ends in evaporation, not the sea.