Waves traps air in the
rock joints and is
compressed by oncoming
waves,exerting presssure
on joints,cause joints to
weaken & rocks shatter
Abrasion/Corrasion
Sediments are carried by
waves and are hurled against
the coast.Loosened sediments
knock and scrape against
coastal cliffs.Weakens surface
and breaks down the
coast.Powerful enough to
undercut a cliff.
Attrition
Rocks break down into
smaller pieces & become
smoother and more
rounded over time.
Solution/Corrosion
Sea water react chemically with
water-soluble minerals in coastal
rocks.For exp,limestone are easily
eroded by carbonic acid.Weakens
rocks and rocks will eventually
disintegrate.
Sediment
Transport
Longshore
drift
Beach drift
Resultant
Zig-Zag
movement of the
sediments
Longshore
current
Currents that
flow parallel to
the coast
Sediment
deposition
Low wave energy like
constructive waves
allows the deposition
of sediments.It vary
in type and
size,resulting a
variety of beaches
Coastal landforms
Depositional
coast
Beaches
Form from loose
sand,gravel,pebbles,broken
shells etc.
Fine sand =
gentler
gradient;Coarse
sand = steeper
gradient
Constructive
waves
Spits&tombolos
Longshore Drift > direction of
coastline changes abruptly > LSD
continue to transport sediments
from original direction >
Sediments accumulated appear
above water surface > spit >
continue to extend from mainland
to another island > Tombolo