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HarD roCk Soft r ock HarD roCk HarD roCk Waterfall retreats Steep-sided gorge develops as waterfall retreats A plunge pool develops Ridges of hard rock creates an uneven slope. This creates rapids Waterfalls are one of the most spectacular landforms found in the upper valley and are created by erosion processes. A waterfall occurs where a band of hard rock (such as granite) overlies a softer rock (such as sandstone). Erosion processes such as hydraulic action (the force of the water) and abrasion (where the river rubs stones that are being transported against the bed of a river, thereby breaking it down) dominate. The softer rock is eroded quicker than the harder rock and gradually washes away downstream. This creates a plunge pool where water is swilled around and any rocks or debris swept will be swirled around and rub against the bed and banks of the plunge pool (called corrasion), deepening it further. Over time, the softer rock is eroded further creating an overhang of hard rock. This overhang is unstable and its weight is unsupported. Eventually, this hard rock collapses and the waterfall moves back upstream. This creates gorges, which are steep sided rivver valleys. This process will repeat continually, with the location of the waterfall moving back upstream. Overhang

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Page 1: Soft rock HarD roCk - nstgroup.co.uk Library/PDFs/Other Documents... · Soft rock HarD roCk HarD roCk Waterfall retreats Steep-sided gorge develops as waterfall retreats A plunge

HarD roCk

Soft rockHarD roCkHarD roCk

Waterfall retreats

Steep-sided gorgedevelops as

waterfall retreatsA plunge pool

develops

Ridges of hard rock creates an uneven slope. This

creates rapids

Waterfalls are one of the most spectacular landforms found in the upper valley and are created by erosion processes.

A waterfall occurs where a band of hard rock (such as granite) overlies a softer rock (such as sandstone). Erosion processes such as hydraulic action (the force of the water) and abrasion (where the river rubs stones that are being transported against the bed of a river, thereby breaking it down) dominate.

The softer rock is eroded quicker than the harder rock and gradually washes away downstream. This creates a plunge pool where water is swilled around and any rocks or debris swept will be swirled around and rub against the bed and banks of the plunge pool (called corrasion), deepening it further.

Over time, the softer rock is eroded further creating an overhang of hard rock. This overhang is unstable and its weight is unsupported.

Eventually, this hard rock collapses and the waterfall moves back upstream. This creates gorges, which are steep sided rivver valleys. This process will repeat continually, with the location of the waterfall moving back upstream.

Overhang