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1.) Vertical erosion:
rivers discharge is low in the upper course, so the river can only erode downward
2.) weathering:
the valley's sides are slowly broken down through weathering
3.) mass movement:
overtime the weathering of material will be transferred by means of gravity along with rainfall towards the rivers channel , later then steepening the valley's sides.
4.) V shaped valley:
the narrow steep sided valley shape is created due to upland rivers
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