Case Study of Fluvial Landforms and Processes

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Case Study of Fluvial Landforms and Processes

All rivers aim to reach equilibrium so they are balanced and when they

are in equilibrium from source to mouth a smooth curve is created

called the graded long profile. However, as you can see from the

diagram many rivers such as The Afon Glaslyn, do not acheive

equilibrium and reach their graded long profile:

Long Profile of Afon Glaslyn River with graded long profile

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Rivers become out of equilibrium when there is a change in base (sea)

level. There can either be a positive change (rise) in the sea level

or a negative change (fall) in sea level, resulting to a change in

base level and a new graded long profile. Sea level changes happen

because the Earth is in or out of glacial periods. Therefore sea level

is changed either eustatically- a change in sea level due to a change

in the amount of water locked up in ice sheets, or isostatically- when

the the change in sea level is due to a change in the level of land

caused by growing or retreating ice sheets. The change in base level

affects the long profile of a river and as the river tries to reach

its new graded profile in order to reach equilibrium there are various

processes and landforms found along the river's course. By looking at

The Afon Glaslyn we can see how and why these processes occur and

landforms formed.

The Upper Reaches

0-4km

· Processes

The main process in this section is erosion, in the form of:

attrition, corrasion, hydraulic action and corrosion. Attrition is

when the boulders collide with each other, breaking up into smaller

pieces. Corrasion is when the ,material carried in suspension rubs

against bank of river. Hydraulic action is the rivers force dislodging

particles and finally corrosion is when acids dissolve rock. Erosion

occurs because at this point the river is above its graded profile

(base level decreased) and the lithologhy (made up of hard rock), this

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