Science Facts

Why Do Rivers Meander? – River’s Curve

Rivers Meander

Rivers, the gently flow over sloping ground, do begin to curve back and forth. These bending, looping rivers are called meandering rivers. So what causes a river to bend in the first place? All it takes is a little disturbance and a lot of time, which is plenty in nature. River bends are asymmetric due to obstructions. Hence, the speed of flowing water between the banks differs.

Meanders are a feature of old age. As rivers age, they develop more and more exaggerated meanders. Eventually, the meander becomes so exaggerated that the curve is abandoned, and an oxbow lake is formed. And the channel becomes straight again. Humans can only develop these curves when an area is flat, like back east at the Mississippi. And the exaggerated curves as well, which means central Washington used to be flat. But there’s a twist. This place isn’t flat anymore. This is a deep canyon system.

Why do rivers meander?

Meander is a slight bend in the river, and water will continue to flow down the river’s long profile from the upper course to the low cost. As the water flows through the meander, it travels faster on the outside bend creating erosion through abrasion and hydraulic action. This undercuts the riverbank and forms a river cliff, whereas the water travels slower on the inside bend, causing deposition to create a slip-off slope.

The meanders got established when the area was flat. A subtle curve is becoming a more exaggerated curve. Entrenched meanders tell that the land is lifting against the river. The river has been down there for millions of years. And the land has been lifting against the meander against the river. The river’s been cutting, matching an uplift rate of the bedrock. Basalt layer after basalt layer exposing themselves on the way up.

The winding curve in a river is the result of erosional and depositional processes. River water flows around various obstructions such as stones and rocks, which results in different areas of slow and fast-moving water. Deeper parts of the river contain slower areas of water and are filled with fine sediments. These parts are known as pools. Shallower parts of the river contain faster areas of water and larger stones.

These areas are called riffles. The river now swings from side to side, and over time the pools move to opposite sides of the relatively straight channel. As fast-flowing water erodes the outside of the pool and slow-flowing water deposits, various materials inside the pool meanders begin to occur.

Meanders are formed in the middle course of a river. The rivers flow through almost a flat plane in the middle courses. As water flowing under gravity seldom flows straight for any long-distance, a winding course soon develops. The irregularities of the ground force the river to swing in great S-shaped curves forming horseshoe-like loops called meanders.

The course of a river comprises three distinct paths.

  • First is the upper or the mountain course where the river originates. Here the velocity of the water is faster due to the steep gradient. The floor of the valley is narrow, and the valleys are reshaped.
  • Second is the middle of the valley course, where floors are wider, and the sides of the valley are more gently sloping. Here the velocity of the river is slower than the upper stage. Meanders are typical landforms found in this stage of the river.
  • The third part of the river is the lower course which has a gentle slope and almost flat. The river channel is usually at its widest and deepest here. It is because the amount of water flowing within the river is at its greatest. Oxbow lakes are conspicuous features in the lower course of a river apart from the deltas, where the river
    drains inter seas.

The water in a river channel flows faster around the outside bend due to centrifugal force, whereas it is relatively slow on the inside bends. The fast-flowing water on the outside bend erodes the riverbanks, whereas slow-moving water deposits sand and mud on the inside bend. At the site of erosion on the outside bend, a steep river cliff is created. The water piles up on the outside bend due to centrifugal force. A bottom current is set up in a corkscrew motion that deposits the eroded material on the inner bank, forming a slope slip.

In the lower course of a river, a meander becomes very much pronounced. The outside bend gets eroded rapidly, and the meander loop becomes almost a complete circle. Gradually the narrow necks of the loop erode further and intersect each other. Now the river cuts through the intersection to flow in a straight path. As a result, the meander loop is abandoned, and it forms an oxbow lake. The oxbow lake later turns into a swamp, and subsequent floods may silt up the lake. It becomes marshy and eventually dries up.

On the faster side of the river, speedy water carries loose, dirt, and rocks from the riverbed and banks eroding to form a hollow. Water gushes into the newly formed hollow with increased speed and erodes more. As the water begins to run faster through the new opening, it further does the opposite bank. On the slower-moving side, water can’t carry much weight.

Hence, all the dirt moves to the bottom, making the river shallower until it becomes land. While one side of the river is drying up, the new curve causes water running against the outside bank to pick up enough force. It slams into the opposite bank further down the river. It also creates another curve and then another, until eventually a windy, snakelike river.

The meanders tend to grow with time. That’s because water enters a bend and flows on the inside of the bend. It tends to be much slower than the flow on the outside. Imagine, the water coming through the outside has to swing around much more quickly than on the inside. So that is the general relationship about the Reynolds number, which depends on flow speed.

Scientists can’t predict because the bend tends to grow and become larger and larger. The outside of the bend is eroding, and the inside is depositing. The Reynolds number depends both on flow speed and water depth. The highest water depth and the fastest flow speeds are on the outside of the bend carry the highest Reynolds number.


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