In the upper course: The valley is V-shaped due to there being lateral erosion and gravity is the predominant force and the water wants to reach the base level (sea level). There is more transportation by suspension, traction and saltation but not solution. Erosion is primarily hydraulic action and solution. Finally, there are interlocking spurs in the upper course which wind round the rocks (but are no meanders)
In the Middle Course: The valley becomes wider as lateral erosion takes over, due to the fact that the river is closer to the base level. Meanders begin to occur as there is faster flow on the outside so more erosion but slower velocity on the inside causing deposition.
In the lower course: The river is at it's deepest here and most wide, which much larger meanders. The valley has a greater velocity as there is less friction. Most transportation is in the form of solution
I think its a river!
A mountain stream, or a river flowing lower down in the valley.
the river running through rock wear it down into deep valley with the steep sides what is it called
Rhône River valley
Narrow valley.
it is the valley that the St Lawrance river flows down.
Yes, a valley typically has steep sides that slope down to a flat bottom where a river or stream may flow. The steep sides are usually a result of the erosion caused by the flowing water over time.
Mainly it becomes polluted and it loses a large amount of its water through evaporation in the desert.
Because the river is small at the top and big lower down. Just sometimes you get a river that is big at the top and smaller at the bottom, which is why you should never say "always".
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.
Because there strong enough
meander