Formation of a v-shaped valley Flashcards
1) Rivers begin high up in the mountains, TMT
they flow quickly downhill as vertical erosion.
2) The river cuts a deep notch down into the landscape TIDT
abrasion, hydraulic action, solution + attrition.
2) Abrasion - is where pebbles grind along the river bank / + bed by the movement of water TMT
it is like a sandpaper effect.
2) Hydraulic action - this is the sheer power of the water as it smashes against the river banks. Air becomes trapped in cracks TMT
it causes ‘‘mini explosions’’ causing parts of the river bank to break away.
3) As the river erodes downwards, the sides of the valley are exposed to freeze-thaw action, TMT
the rocks are loosened. Some of which will fall into the river + steepen the valley’s sides.
4) Gradually, mass movement of the materials, slides down the valley slope, giving a distinctive v-shape. TMT
this material is gradually transported away by the river when there is enough energy.
5) The rocks which have fallen into the river help with abrasion TMT
further erosion is caused.
6) As the river flows through the valley, it is forced to swing from side to side around more resistant rock (spurs) TMT
this creates interlocking spurs.