Underground spring in the context of "Lake Akşehir"

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⭐ Core Definition: Underground spring

A spring is a natural exit point at which groundwater emerges from an aquifer and flows across the ground surface as surface water. It is a component of the hydrosphere, as well as a part of the water cycle. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall.

Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. A spring produced by the emergence of geothermally heated groundwater is known as a hot spring. The yield of spring water varies widely from a volumetric flow rate of nearly zero to more than 14,000 litres per second (490 cu ft/s) for the biggest springs.

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👉 Underground spring in the context of Lake Akşehir

Lake Akşehir (Turkish: Akşehir Gölü) is a tectonic freshwater endorheic lake in Afyonkarahisar and Konya provinces, in the southwestern part of Turkey. It carries the same name as the town of Akşehir south of the lake.

The lake is fed by the Eber Channel, five larger streams from the Sultan Mountains, and many smaller streams. The lake's salinity increases towards the middle and northern parts due to underground spring waters. The lake is used for irrigation.

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