The Atlantic Gulf Stream also meanders, as shown in the Wikipedia image below. Often the thalweg is the last section to freeze, leaving a sinuous thread of coursing water visible.
The wave pattern of a meander shows up in winter as streams ice over. Without scale, it can be difficult to discern which is which in aerial images. Channels throughout the world follow this meander geometry so closely that the form of a large river resembles that of small streams. The radius of curvature of the central portion of the channel’s bend averages about 1/5 of the wavelength. No matter the size of the stream, the wavelength is approximately 11 times the channel width and, invariably, between 10 and 14 times the width. Meander patterns follow a remarkably predictable geometry described by wavelength, radius of curvature, and channel bankfull width – the height on the bank where, at higher flows, water begins to tip onto the floodplain (see figure below). The meander pattern is ubiquitous it’s difficult to find examples of straight streams of great length and, even then, the deepest part of the channel – the thalweg – will meander within the straight channel.
Oxbows along the West Branch Ausable River near Lake Placid, along River Road, are easily visible on Google satellite views they indicate the river's former path prior to the Ausable's logging era. Eventually, the meander may be cut off from the main channel, forming an oxbow lake. Give with confidence today!Įrosion in a stable stream can be minimal from year to year, but as a meander moves outward and becomes more looped, flows intensify on the outer bends. Support our Natural Stream Restoration efforts to recreate stable channels based on the hydrology and hydraulics that shape natural channels. Further downstream, moving out of the bend, the channel straightens, and the channel cross-section becomes more uniform through the riffle. In these pool and bend sections, one side of the channel is significantly deeper. As every angler knows, deep pools form on the outer bends of meanders, with low sloping point bars of accumulated gravel or cobble on the inside bends. This process reinforces the riffle-pool structure of a stream. Meanders are produced when water in the stream channel erodes the sediments of an outer bend of a streambank and deposits this and other sediment on subsequent inner bends downstream.
Remember, streams are transport machines, moving water and sediment from their watersheds relentlessly downslope. Streams meander to maintain equilibrium – a dynamically stable form and function. The geometry of the meander minimizes the amount of work, or energy expended, while using that same energy uniformly. Those bends and turns manage the energy of water, as it moves through and over channel terrain, by increasing resistance and reducing channel gradient. On broad, low-slope plains, streams thread back and forth. In steep topography, channels are straighter, influenced by slope and confined by valleys. They are sinuous, with channels that bend, curve, or loop. When you see a stream from the air, from a plane or a satellite photo, one thing is quickly apparent: streams meander.
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