Why Do Rivers Flow in Curves?
Rivers flow in curves because water erodes the outer bank while depositing sediment on the inner bank, gradually forming the bends known as meanders.
The Physics Behind the Curves
The process by which rivers form curves is known as meandering and it works through a fascinating self-reinforcing cycle. When a river bends slightly at any point, the water on the outer side starts flowing faster. As the speed increases, that section erodes more soil and sand. On the inner side, the water moves more slowly and deposits the material it was carrying. Over time the outer bank gets carved away while the inner bank builds up. This process makes the curve a little more pronounced with every passing year. Over decades and centuries a river can develop enormous bends. Some rivers curve so dramatically that a loop nearly forms a complete circle, and eventually that loop gets cut off and becomes an isolated body of water. This is called an oxbow lake and examples of them can be found all over the world. So in a sense rivers do not just carry water, they are constantly rebuilding their own beds.
There are other factors that influence how rivers curve as well. Gravity, the composition of the ground, the amount of rainfall and the changing water levels across seasons all play a role. In soft soils rivers develop deeper and more dramatic curves much more quickly, while rocky terrain slows the process down considerably. On flat plains rivers seem to wander almost freely and produce different curve patterns over centuries that are genuinely striking when viewed from above. Studying these patterns from satellite imagery is an experience in itself. Nature does not engineer anything deliberately, yet the results sometimes look more precise than the finest human construction. /