COASTAL PROCESSES
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Transcript COASTAL PROCESSES
COASTAL
PROCESSES
COASTAL
PROCESSES
COASTAL
EROSION
COASTAL
TRANSPORTATION
COASTAL
DEPOSITION
COASTAL
DEPOSITION
It refers to processes that results in the addition of materials
to the coasts.
COASTAL TRANSPORTATION
This refers to the movement of materials along the coast.
COASTAL
EROSION
This refers to the processes that results in the removal of
materials from the coasts.
COASTAL EROSION
COASTAL EROSIONAL
PROCESSES
HYDRAULIC
ACTION
FACTORS AFFECTING EROSION
WAVE SIZE
ABRASION/
ROCK COMPOSITION/
CORRASION
STRUCTURE
ATTRITION
POSITION OF COAST
SOLUTION/
CORROSION
CLIMATE
COASTAL
EROSIONAL
PROCESSES
HYDRAULIC ACTION I
Waves repeatedly hits against soil and rocks along a coast.
Over time, the repeated wave action loosens these soil and rocks and
sweeps them away.
This process is known as hydraulic action.
HYDRAULIC ACTION II
As the waves pound against the coast, the air within these cracks is
compressed.
When the waves recede, the compressed air suddenly expands.
Over time the repeated compression and expansion widens and
weakens cracks and ultimately breaks the rocks.
ABRASION
Waves carry rock fragments such as pebbles and gravel.
These fragments act as chiselling tools when they are hurled against
the coast, and breaks the rocks.
This process is known as abrasion.
ATTRITION
Rock fragments carried by the waves are thrown against one another.
This gradually break up the rocks into smaller, smoother and
rounded pieces.
This process is known as attrition.
SOLUTION
Soluble minerals in coastal rocks are dissolved in and removed by the
seawater.
For example, calcium carbonate reacts chemically with the carbonic
acid and changes into soluble hydrogen carbonate.
When solution occurs, the rocks are weakened and ultimately
disintegrates.
FACTORS AFFECTING
COASTAL EROSION
WAVE SIZE
The bigger the waves, the more energy they have to erode the coast.
This is because larger waves have more powerful backwash than the
smaller waves that plunges over when breaking.
This erodes the coast faster.
ROCK COMPOSITION I
Soft rocks such as shale and clay will be eroded faster than hard rocks
such as granite and basalt.
This is because, such rocks being weaker are unable to withstand the
force of the strong waves.
ROCK COMPOSITION II
Similarly, rocks with mineral composition that that or chemically
react with water to form new chemicals are more prone to erosion.
This is because, such rocks are gradually weaken under the constant
attack of sea water and break down.
ROCK STRUCTURE
The presence of lines of weaknesses such as joints and bedding
planes will result in a faster rate of erosion.
This is because such weaknesses makes the rocks more susceptible to
the strong force of waves.
POSITION OF COAST
A coast that is exposed to strong prevailing onshore winds will be
more susceptible to erosion.
This is because it is exposed to the full force of wave action while
sheltered coast is protected.
CLIMATE
Strong prevailing onshore winds such as monsoon period will
intensify coastal erosion.
This is because wave action is much more stronger during this period.
HUMAN INTERFERNCE
Coastal defences such as seawalls and breakwaters slows down the
rate of coastal erosion.
COASTAL
TRANSPORT
COASTAL TRANSPORT
One of the ways in which waves transport sediments along a
coast is by longshore drift.
Definition: This refers to the movement of materials along a
coast by the action of waves.
Draw: Longshore Drift
LONGSHORE DRIFT
Waves approach coast at an angle.
Swash carries the materials up the coast at an oblique angle.
Backwash carries the materials perpendicularly down the beach due to gravity.
This results in a zig-zag movement of materials along a coast known as the
longshore drift.
COASTAL
DEPOSITION
WHEN?
SHELTERED COAST:
Deposition occurs when the coast is sheltered from prevailing winds as wave
erosion is minimal in these areas.
GENTLE COASTAL SLOPE:
On a gentle slope, depositional materials are brought by constructive waves as
swash is more powerful than backwash in this area.
WHEN?
EXCESSIVE LOAD
During a storm, large amounts of materials are eroded from the coast. These
materials are deposited when the storm subsidies as the retreating waves are
unable to carry them.
SHALLOW WATERS
When the coastal waters are shallow, the advancing waves break off and leave
eroded materials on the coast and deposition occurs.