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FREE SAMPLE: OCR A Level Geography Coastal Landscapes Summary - 1a (Coastal landscapes can be viewed as systems) £0.00

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FREE SAMPLE: OCR A Level Geography Coastal Landscapes Summary - 1a (Coastal landscapes can be viewed as systems)

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Summary of part 1a from Chapter 1 (Coastal Landscapes) of Michael Raw's OCR A Level Geography textbook which is linked to this document

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  • Chapter 1, 1a (coastal landscapes can be viewed as systems)
  • August 4, 2022
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  • 2021/2022
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System feedback in coastal landscapes

Equilibrium = the rate at which sediment is being added to the beach is equal to
the rate at which sediment is being removed from the beach, inputs and outputs
1.1 . How can coastal landscapes be viewedareas systems?
equal
 1a. Coastal landscapes can be viewed as systems
Dynamic equilibrium = when equilibrium is disturbed and the system undergoes
Components of open systems self-regulation and changes its form in order to restore equilibrium, a state of
balance between continuing processes, this is an example of negative feedback
System = set of interrelated objects comprising components (stores) and
processes (links) that are connected together to form a working unit Negative feedback = an automatic response to change in a system that restores
equilibrium
Open system = energy and matter can be transferred from neighbouring
systems as an input as well as to neighbouring systems as an output e.g. Sediment cells
input of fluvial sediment from a river, as it deposits its load at the mouth
when available energy decreases Closed system = a system with inputs
and outputs of energy, but without
A coastal landscape system has: any movement of materials across
system boundaries, e.g. sediment cell
- Inputs
 kinetic energy from wind and waves Sediment cell = stretch of coastline
 thermal energy from the heat of the Sun and its associated nearshore area
 potential energy from position of material on slopes; material within the movement of coarse
sediment, sand and shingle is largely
from marine deposition, weathering and mass movement from
self-contained
cliffs
 90% = fluvial deposition  Sediment doesn’t usually move
- Outputs between cells, however the
 marine & wind erosion from beaches & rock surfaces; evaporation dissolved material doesn’t require
- Throughputs much energy so may move to the
next cell via suspension
 stores, including beach and nearshore (shallow waters) sediment
accumulations
 flows (transfers), movement of sediment along a beach by LSD  11 large sediment cells across the coast of England & Wales
 Boundaries are determined by the topography and shape of coastline
 Large physical features e.g. Lands End, act as huge natural barriers that
prevent the transfer of sediment to adjacent cells
 It’s unlikely that they are completely closed because of: variations in
wind direction & presence of tidal currents
 There are many sub-cells existing within major cells

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