A river that writes its own history
The Yeşilırmak, or "Green River," flows through a narrow valley in northern Turkey, but its path is anything but straight. This river is an example of a meandering system, a dynamic process where the channel snakes across its floodplain in a series of looping bends. The geomorphology is driven by simple physics: water on the outer edge of a bend flows faster, eroding the bank, while slower water on the inner edge deposits sediment. This constant erosion and deposition cause the meanders to migrate sideways and downstream over time.
In extreme cases, the neck of a meander loop becomes so narrow that the river cuts a new, shorter channel during a high-flow event. This leaves the old, curved channel abandoned, forming a crescent-shaped body of water known as an oxbow lake. The Yeşilırmak River basin is a landscape with these fluvial scars, a record of its movement. The river itself stretches for approximately 519 kilometers, draining an area of over 38,000 square kilometers before reaching the Black Sea. The silts carried and deposited by the river and its tributaries have formed the fertile Çarşamba Plain at its delta.