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Understanding Waterfalls and Gorges in Geography
May 12, 2025
Waterfalls and Gorges - Edexcel GCSE Geography
Key Terms
Waterfall
Hard Rock
: Example - Winstone
Soft Rock
: Example - Limestone
Erosion Types
:
Hydraulic Action
Abrasion
Solution
Plunge Pool
Overhang
Unsupported Rock Fall
Gorge
Waterfalls
Basic Structure
Occur in the course of a river
Consist of two layers of rock:
Hard rock on top
Soft rock on bottom
Diagram Guidelines
Use a pencil for diagrams
Avoid using a ruler; real-life rock faces aren't straight
Process
Erosion of Soft Rock
:
Soft rock erodes faster than hard rock through solution, hydraulic action, and abrasion.
Sediment from erosion is washed downstream, creating a plunge pool.
Water, debris, and rock swirl in the plunge pool, increasing its size through abrasion.
Formation of Overhang
:
As the plunge pool enlarges, the overhang becomes unsupported.
Rock fall occurs when overhang collapses, a type of mass movement.
Collapsed hard rock contributes to upstream retreat of the waterfall.
Cycle repeats: the area of rock fall becomes the gorge.
Gorge Formation
:
The gorge forms between valley walls following the retreat of the waterfall.
Eroded hard rock is carried downstream as larger particles.
Named Example: High Force (River Tees)
Location: Teesdale, County Durham
Hard Rock: Winstone
Soft Rock: Limestone
Limestone eroded away by solution, resulting in waterfall dynamics.
Exam Tips
Be prepared to apply knowledge to diagrams or pictures.
Identify soft rock, hard rock, and main waterfall in images.
Note conditions like high rainfall contributing to additional water flow.
Annotate diagrams thoroughly to demonstrate understanding.
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