Waterfall Formation in Detail
Waterfalls form through fascinating differential erosion processes that you can observe at places like Powerscourt or Niagara Falls. The key is understanding that hard rock (like granite) resists erosion much better than soft rock (like limestone).
When a river flows over alternating bands of hard and soft rock, hydraulic action and abrasion erode the soft rock faster, creating a small fall. The falling water carves a plunge pool at the base through eddying - that swirling action that deepens the pool.
Solution from misty spray gradually weakens the back wall, whilst hydraulic action undercuts the hard rock above. Eventually, the unsupported overhang collapses into the plunge pool. This undercut and collapse process causes headward erosion - the waterfall literally migrates backwards towards the river's source!
As the waterfall retreats, it leaves behind a deep, narrow gorge. Niagara Falls moves backwards about one metre per year through this incredible natural process.
Exam Gold: Remember the sequence - differential erosion → plunge pool formation → undercutting → collapse → headward erosion!