Define mature river










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List of rivers by age

The stream drops its sediment load in a deposit called a delta. Meandering stream channels are quite common. A stream has a natural tendency to reach a base level. The dams have also reduced the amount of natural floods along the river and the velocity of the river's flow. In a waterfall, as water continues to fall over the edge, it erodes the bed of the channel at the base of the waterfall. These dissolved substances are the result of the chemical weathering of rock, which alters the internal structure of minerals by removing or adding elements. The amount of sediment a stream moves depends on the velocity of the stream and the size of the sediment particles. As soon as a stream's velocity decreases, it loses the ability to carry all of its load and a portion will be deposited, depending on how much the stream slows down. Alluvium pronounced ah-LOO-vee-em is the general term for sediment deposited by running water. This refers to the point at which the stream reaches the elevation of the large body of water, such a lake or ocean, into which it drains. Mud deposited on the floodplain can make the soil really good for agriculture. Streams and rivers erode, transport sediment, change course, and flood their banks in natural and recurring patterns.

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According to multipass-recovery.com, mature rivers are bodies of water that flow over wider valleys and snake along flat plains. The meandering streams then create larger.

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Description: Water moving at a low velocity can move only small, fine particles such as sand, silt, and clay. A low ridge or mound along a stream bank, formed by deposits left when floodwater slows down on leaving the channel. When water flows down a slope, it tends to gather in small depressions on the surface along the way. It has a wide, well-developed floodplain marked with oxbow lakes. In contrast, a permanent stream is one that has cut its valley deeply enough so that ground-water seeps into it and keeps it flowing between rainfalls. If you bring your eye to within a few inches of the surface, each stone appears to be submerged in glycerin yet still sharply etched, as if held closely under a strong magnifying glass in summer light. Large rocks and other heavy material are deposited first, followed by other material in decreasing size. As the water erodes rock and other material in the depression, it forms a channel. Eventually, the rapids, too, will be eroded away. The low, crescent-shaped deposit of sediment on the inside of a meander. When it enters the ocean, the Amazon discharges about 7,, cubic feet , cubic meters of water per second.
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