Winding rivers flow higher and therefore with more overall flow, pressure and erosion outside their curves due to the formation of a vortex as in a choppy cup of coffee and, as a result, the river further erodes the outer bank. In the inner bend of a river, the level is lower, the secondary flow moves sand and gravel through the river bed, creating shoals and point beams, and air friction and bed disturbances act against a higher proportion of the water column, which is shorter and slows the water to varying degrees.  Rivers are generally described and interpreted by their convolution. The term is also used to describe the actual occurrence and potential tendency of a river to bend or meander along its length.  It is expressed as the ratio of the distance between two distant points of a river that follow the average course of the river to the right distance between these points.  There are three conventional categorizations of rivers or their foothills. Winding rivers have a winding value of more than 1.5. A softening value of less than 1.1 is a “straight” flow. Between these values, a flow is described as sinuous, describing those that are in a state of transition between the two states. Braided rivers do not follow the same convention.  Winding rivers tend to increase softening.  A meander is a natural form of cutting or cutting in a river when a pronounced meander (hook) in a river is broken by a current that connects the two parts closest to the hook to form a new channel, a complete loop.
The steeper slope of the slope causes the current of the river to gradually leave the meander, which silts up with the sediments of the deposit. Cuts are a natural part of developing a winding river. The rivers form meanders when they flow laterally downstream, or even swing.  Some research has been done to show importance. Further studies need to be conducted on how the extent of these floods and their recurrence interval are related to the frequency with which these sliding stop channels form.  Neck barrier channels are generally formed in the same way when a flow over the bank occurs at high tide and the narrow piece of land between a bend is eroded into a meander; This is called quick cutting.  A meander can also be cut by a channel, as there is an excess of sediment upstream due to high erosion rates. This causes a barrier channel to form, as a river may no longer be able to efficiently transport these sediments across the bend, so the river forms a new path for the river.  Meandering cuts can also be formed by humans; The removal of a beaver dam increases the likelihood that winding channels will block the formation of downstream channels.  A barrier channel can be built for navigation, traditionally for watermills and to control the possibility of future flooding in lower stretches away from the tides. These winding cuts straighten a river.
 Many rivers are transformed by man and become less winding.  The meanders reflect the laws of physics. Currents offer a classic case of an open system – mass and energy can flow through and refine its boundaries. For streams that control downspout water flow, the opposing needs to minimize labor and evenly distribute labor or energy lead to trade-offs. The form that the compromise takes is meandering to achieve a dynamic but relatively stable form. When one of these meander cutting processes occurs, there remains an elbow in the river, which in many cases forms a dead arm. A dead arm lake forms after sediment is deposited by the new barrier channel that flows next to it at the entrance to the abandoned bend; This completes the curve of the rest of the river. Oxbow Lakes have proven to be an important habitat for various wildlife species.
Recently, efforts have been made to protect these important waters from harmful practices such as agricultural use.  One of the methods proposed to restore these dead arm lakes was dredging. Dredging removes sediment from the lake floor and increases the depth of the lake. Collins Lake in Scotia, New York, is an example of this method. Oxbow Lakes can be useful for recreational purposes, and in Salix, Iowa, water levels on Browns Lake have been raised for recreational purposes.  The meander is omnipresent; It is difficult to find examples of straight streams of great length, and even then, the deepest part of the canal – the Thalweg – will meander through the straight channel. The sinuous patterns follow a remarkably predictable geometry described by the wavelength, radius of curvature, and width of the channel bank – the height on the shore where water flows over the floodplain at higher currents (see figure below). Regardless of the size of the current, the wavelength is about 11 times the width of the channel and invariably between 10 and 14 times the width. The radius of curvature of the central part of the curvature of the channel is on average about 1/5 of the wavelength. Canals around the world follow this meander geometry so tightly that the shape of a large river resembles that of a small stream.
Without scale, it can be difficult to see what`s what in aerial photographs. Erosion in a stable stream may be minimal from year to year, but as a meander moves outward and becomes more twisted, currents in the outer curves intensify. Finally, the meander can be cut off from the main channel and form a dead arm. Dead arms along the West Branch Ausable River near Lake Placid along River Road are clearly visible on Google`s satellite views; they indicate the former course of the river before the period of exploitation of the Ausable. For more information about user permissions, please see our Terms of Service. If you have any questions about content licensing on this page, please contact email@example.com for more information and to obtain a license. If you have any questions about how to quote something on our website in your project or class presentation, please contact your teacher. He or she will know the preferred format. When you contact them, you need the page title, URL, and when you accessed the resource.
A dead arm lake begins as a curve or meander in a river. A lake is formed when the river finds another, shorter course. The runner becomes a dead arm lake along the river. Dead arms usually form in shallow low-lying plains near the mouth of the river in another body of water. At these levels, rivers often have wide meanders. The meanders that form lakes of dead arms have two sets of curves: one that moves away from the right path of the river and the other that curves back. The angles of the curves closest to each other are called concave benches. Concave banks erode over time. The power of the water flowing from the rivers carries the earth to the sinuous concave banks. The banks opposite the concave banks are called convex banks.
The opposite of erosion occurs here. Silt and sediment form on convex banks. This structure is called a deposit. Erosion and deposits eventually lead to the crucible of a new channel through the small piece of land at the narrow end of the meander. The river makes a shortcut. The Oxbow Lakes are the remains of the river bend. Dead arms are lakes of calm water. This means that no water flows in or out of them.