V-Shaped Valleys and Interlocking Spurs
Ever wondered why mountain valleys look like giant "V" cuts in the landscape? It's all down to how rivers behave when they're young and energetic in their upper course.
Rivers flowing through steep, high land are packed with potential energy, but here's the catch - they lose 90% of this energy to friction! With only 10% left for actual erosion work, these rivers focus all their power on cutting straight down through the rock. This process is called vertical erosion.
As the river cuts downwards, weathering slowly breaks down the valley sides. Gravity and rainfall then transport this weathered material towards the river channel, making the sides even steeper. The result? Those distinctive V-shaped valleys with their narrow, steep-sided profiles that you see in upland areas.
Quick Tip: Remember that low discharge in the upper course means the river can only erode downwards, not sideways - that's why you get that sharp "V" shape!



