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Summary A* level complete notes and all case studies on Coastal Landforms

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These A* Coastal Landscapes notes cover every OCR A-Level Geography specification point and all required case studies, with precise definitions, key processes and the advanced concepts needed for top-band work. They also include high-quality model answers for the 4/8-mark questions, giving you clear structures, exemplar phrasing and the exact detail examiners reward — everything you need to confidently produce A*-level coastal essays.

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Palm
Jumeirah


Saltburn

Fianborough NILE




coasts
Walton
The
Holderness Naze

, Holderness coastline :




East coast of
England ,
Yorkshire

Annual erosion rate of around 2 meters per year-up to 10m in places
↳ one of Europes coding
fastest coastlines


-





1 I
CAUSES Physical Human

the coastline is made Recurved sea
Geology up walls deflects energy,
· -
· -




of a mixture of clays and erratics (loose not absorbs -
this prevents mainland

rocus) . erosion ,
however beach erosionI
-





clay Sits on a seaward
sloping layer of Groynes (Mapleton) placed perpendicular
-
·




Chall :.
being eroded faster than the to coastline to trap sediment as it is moved


chalk .

by longshore drist
.



↳ Boulder eroded in 4
Clay is
being stages Sediment balance of the spurn head Spit
: ·




1 Rainwater has altered the
Saturates
Clay .. unstable been -
Spit could
easily
.




2
. Cliff be breached
is too steep :
Slumps




g-
. This the
3 reduces
angle preventing further

erosion


4 .

Large waves from the North East

the
remove debris as longshore drift
to the South




Marine processes the size of the
·
-




retch , frequency

frequency of longshore drift
↳ a
long fetch from NE winds creates


larger waves+
stronger backwash : erosion t


↳ Holderness is on the track of mid-latitude


depressions that increase the prequency

of destructive waves : Crosion +

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