Formation of a waterfall Flashcards
Part one - differential erosion
Where waterfalls (found in the upper course of the river) flows over bedrock with varying levels of resistance, the softer rock erodes first (this is known as differential erosion) This creates a step in the river where the rock meets
Part two - erosion
Over time: the erosional processes of hydraulic action, corrasion and solution erode the less resistant rock
The river falls further and so increased hydraulic action at the base forms a plunger pool
Hydraulic action
sheer force of water breaks apart the rocks, and the air bubbles get into the rock and crack it
Corrasion
rock scrapes and wears away the river bed
Solution
minerals and segments are dissolved in the water flow
Part three - collapse of waterfall
The rocks fall into the plunge pool and continue to widen and deepen it through corrosion and attrition (rocks in the plunge pool hit off of each other, eroding the plunge pool further)
The hard rock becomes unsupported as it has been undercut by the softer rock, and collapses due to the lack of support. The waterfall then retreats upstream