a lake.
The sides are known as the river bank or river banks.
Over time, the water erodes the river's banks and river beds changing it flow pattern
bed
When a river is actively eroding its stream bed, it typically has a steep gradient. This steep gradient increases the water's velocity, enhancing its ability to transport sediment and carve out the channel. As the river flows downhill, the energy is concentrated, allowing for significant erosion of the bed and banks. Such conditions are often found in mountainous or hilly regions where the river's slope is pronounced.
Yes, it is the bed of a stream or river.
a little bed of water flows and the joins a bigger bed of water, where it joins a stream and then another stream to a bigger stream, then a river which joins a bigger river then goes down to a waterfall where it joins a lake.
A channel.
Yes, the statement is true. Sediment in a river can cause abrasion as it moves along the stream bed, wearing down the rocks and sediments it encounters. Conversely, the stream bed also abrades the sediment, further shaping and breaking it down. This mutual abrasion contributes to the overall erosion and shaping of the river landscape.
A wider and shallower river stream bed tends to slow down the river's speed as frictional forces increase with more contact with the bed. This can reduce the river's power to cause erosion. Conversely, a narrower and steeper stream bed can increase the river's speed, which enhances its erosive power by allowing it to carry more sediment and erode the riverbanks more effectively.
A river, creek, stream, lake, sea or ocean.
this is the bed of a stream, river, orther water way.
sediment,bank and bed