It is this first curve that causes the forces to build the corresponding second curve. As discussed above, the water flowing on the outside of the first curve has a greater velocity than the water flowing on the inside of the first curve. As the first curve grows, this faster moving outside water enters the straight section of the river at an increasing angle, which directs a greater volume of water at the riverbank opposite the first curve. This greater volume of faster moving water is in essence an original disturbance to a stable, straight river as above, except it occurs on the opposite side. Hence, in this case the opposite bank erodes faster where as sedimentation increases along the inner bank creating a second curve that forms the shape of an S.
Answered by: Jim Aspell, M.S., Gradient Consulting Group
When it rains, if the ground is tilted in any direction, a portion of the water will immediately run off, and a portion will stay in the soil. The part that runs off follows the direction of the highest gradient, that is, the steepest path downhill. The remainder gets absorbed by the soil. This is determined by the soil density and composition. Dry clay, for example, will run off almost all of the water in a hard, fast rain, but in a slow soaking rain will gradually turn into mud. The soil density and composition also affect the percolation of the soil, ie - the rate at which it can absorb water. Returning to our earlier point when water runs across the ground, it erodes the ground it's on. This creates a small depression which is more likely to divert water flow in the future. You can see that this is an accelerating path. Even if the ground is perfectly flat, the soil is probably not uniform all the way across, and will still sink differently, causing a flow.
No matter which mechanism causes the water to flow, gradient or composition or both, once the flow starts, it continues in an accelerating spiral of development, so long as the waterflow is reliable. When you look at the larger pattern of streams and rivers in a country or continent, you can see that they work from smaller to larger, and transport water to the oceans.
Rivers don't form in straight lines, because they always follow the steepest gradient, and they usually follow the softest soils. This process can continue for thousands of years as a river gouges down into the rock, leaving something like the Grand Canyon behind if conditions are right.
Answered by: Frank DiBonaventuro, B.S., Air Force officer, Physics grad, The Citadel
As it slows the stream spreads because of the continuity of flow requirement i.e. that the volume rate of flow from the steeper zone must be maintained at the flat zone.
Further, in spreading, the water along the horizontal perimeter of the flow flows faster than that along the middle path of flow since the former has a greater distance to travel. This hydrodynamic phenomenon is similar to the phenomenon that causes uplift in airplanes in which the air flowing over the upper surface of the plane flows faster than that flowing beneath.
Two factors then come into play:
(i) sediment drops out of the middle path of the stream more readily than out of the perimeter zones causing the build up of an embankment that impedes further flow
(ii) the faster moving perimeter flow scours the channel more than the middle stream flow.
After a flood say therefore, the subsiding waters will find an easier path along the perimeter of flow of retarded flow zones than along their original direction. The water will therefore tend to divide into two downstream channels.
These perimeter paths will never be equally fluent and so the stream of water further chooses the more fluent of the two resulting in a meander.
Meanders therefore develop in rivers flowing through relatively flat areas as opposed to long rivers.
Answered by: Roger Yearwood, B.S., BSc CE, UWI, Trinidad & Tobago
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