3. This study achieves the goals of
determining…
• The direction in which sand moves along the shoreline
& why.
• How this migration is affected by our influences such as
beach groins, river jetties.
• The causes of current & past major episodes of beach
erosion
• What might be done to solve beach erosion .
5. What Is Beach Erosion?
♦ wearing away of land and the removal of beach
or dune sediments
♦ Takes place by tidal currents, drainage or high
winds
♦ which take the form of long term losses of
sediments and rocks
9. Plum Island Beach Sand
Erodes & Accretes (gathers),
wind …
& water…
at the direction of
the forces exerted
by…
10. Between the high & low tide lines and below
the water, wave action moves sand…
Photo:Photo: Clark Little,Clark Little, Surfer MagazineSurfer Magazine
This is especially true at Plum Island as
it is a wave & tide dominated beach
Small waves move sand along the shore but
ultimately leave it behind upon the beach.
Large waves remove sand from the beach to the near shore
shallows & continue to move it along near shore, but underwater.
11. Above the water, wind moves sand that isn’t
stored by vegetation, roots, debris,
beach fences & dunes…
12. ……along the beach,along the beach,
Erosion occurs when
sand withdrawals
exceed deposits…
…and when the sand
reserves of the barrier
dune system are depleted.
17. HOW DO PORTS AND OUTER HARBORS
CAUSE EROSION?
♦ alteration of sedimentation patterns may
lead to accretion or erosion of a beach
♦ Majority of Ports and Harbors are causing
large scale Coastal Erosion.
EFFECTS OF IT:
♦ Loss of coastal habitats
18. ♦ Loss of freshwater
and food
resources.
♦ Increased
Vulnerability
♦ Socio-economic
loss.
♦ Unsustainable
development
Erosion Hot
Spots
23. ESTUARIES:
♦ An estuary is a partially enclosed coastal
body of brackish water with one or more
rivers or streams flowing into it and with a
free connection to the open sea.
♦ Estuaries form a transition zone between the
river environments and the maritime
environments.
24.
25.
26.
27. IMPACTS OF EROSION:
♦ Property loss
♦ Tourism
♦ Environmental Degradation
♦ Historical Sites
31. DUMPING ROCKS IS NOT A SOLUTION
• Increases erosion and transfers problem down the
coast
32. • Has to continue
forever as rocks
keep sinking
• Requires huge
sum of public
money
33. Does not protect us from big
waves
Mountains have to be
destroyed
This is NOT sustainable!
34.
35.
36. DO U KNOW FROM HOW
MANY YEARS VIZAG IS
FACING EROSION?
37. SINCE 20 YEARS..........
It has become severe in vizag
since aug 2007 after the
construction of the
“gangavaram port”.
38.
39.
40. HARD-EROSION CONTROLS
♦ provide a more permanent
solution than the former
♦ Seawall and groyne serve
as permanent
infrastructure.
♦ The average life span of a
seawall is 50–100 years
and the average for a
groyne is 30–40 years.
41.
42.
43.
44. SOFT-EROSION CONTROLS
♦ refers to temporary options of slowing the effects
of erosion.
♦ Options includes sandbag,creepers and beach
nourishment.
♦ not intended to be long term or permanent
solutions.
♦ One of the most common methods is beach
nourishment projects.
45. GROWTH OF
CREEPERS IN BEACHES
YOU WOULD HAVE
NOTICED THIS IN
VIZAG BEACH IN OUR
CHILDHOOD
46.
47. Beach nourishment
• Companies like DCI are currently appointed in
Vizag and other places
• These projects involve dredging sand and moving
it to the beaches .
48.
49. IN 2003 SAND NOURISHMENT HAS SHOWN POSITIVE RESULTS
Before Nourishment After Nourishment
52. RELOCATION
♦ Under this response, humans move from the coast
and surrender the coast to the natural processes of
sea level rise and erosion.
♦ By removing structures along the oceanfront, the
beach is surrendered to the natural forces of the
ocean.
♦ This would be most effective in reducing the
impacts of erosion on human society.
53.
54. GEO TUBES:
♦ These are cylindrical shaped tubular
structures.
♦ These are filled with sand, collected from
the same place where it is need to be
placed.
♦ These are not so expensive.
History repeats itself.
If we look at yesterday we can understand today.
wearing away of land and the removal of beach or dune sediments by wave action, tidal currents, wave currents, drainage or high winds
A wave approaches shore, draws in receding water from the berm’s slope & wicks sand up into its wave face.
As it crashes to shore, sand is run up the beach & either deposited or withdrawn depending on wave size.
The beach berm is the area where you place your towel or chair when visiting the beach.
It is a sacrificial deposit of sand that resides at the pleasure of wind & water.
Like $ in your check book, sand here ebbs & flows. Deposits & withdrawals are made.
A happy checkbook is in balance…one can’t have too many withdrawals.
The barrier dune is the savings account, the checkbook’s lifeline when it becomes depleted.
Cost of harbor about 20 crores.
Cost of dumping rocks for shore protection – about 20 crores upto date. This cost will keep going up as it is a recurring cost – rocks sink into the soft sand.
Length of seawall at present: 8 km. It is extending northwards every couple of years.
There is a truth in nature. A certainty of how things are.
We deceive ourselves when we incorrectly observe or interpret nature’s ways.