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River Landforms Caused by Erosion

Waterfalls

Waterfalls

  • When a river flows over hard rock that overlays softer rock, a waterfall can form.
  • The less resistant rock begins to erode by abrasion and hydraulic action.
  • A step or notch forms in the softer rock, creating a river rapid.
  • Over time, the softer rock is eroded more and more, whereas the harder rock is left sticking out.
  • The height of the drop increases as the water pounds the less resistant rock at the base. Eventually a waterfall forms.
Waterfalls and gorges

Waterfalls and gorges

  • The less resistant rock starts to be eroded underneath the hard rock. This process is called undercutting.
  • The overhanging harder rock collapses because it's unsupported.
  • The waterfall now has harder rock to swirl around its base. The resulting abrasion creates a plunge pool.
  • Hydraulic action keeps undercutting behind the waterfall.
  • If the process repeats over a long time, a gorge may form.
Interlocking spurs

Interlocking spurs

  • In the upper courses of rivers, valleys are steep and V-shaped because most of the erosion that happens is in a vertical direction.
  • Because the rivers don't have enough energy to erode sideways, they are restricted to winding around the hills on the valley sides.
  • These interlocking hillsides are the interlocking spurs.

Landforms of Erosion and Deposition

Meanders

Meanders

  • Erosion and deposition in parts of rivers that have deep and shallow sections lead to meanders forming.
  • On the outside of bends, the deep channel means the current is fast.
    • River cliffs form here because the high energy water has more erosional power.
  • On the inside of bends, the shallow channel means the current is slow.
    • Slip-off slopes form here because sediment is deposited by the low-velocity water.
  • Meanders are usually found in the middle course of a river.
Ox-bow lakes

Ox-bow lakes

  • Over time, meanders become larger, until eventually an ox-bow lake forms.
  • Erosion causes the bends to move closer together to create a swan’s neck meander.
  • During a flood, high energy water will breach the meander neck.
  • This makes the river flow in a straighter and faster course.
  • Over time, deposits will fill in the meander bends.
  • The meander becomes cut off from the river, forming an ox-bow lake.
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