Coral reefs i (english)-converted

A detailed description of Coral reefs involving its definition, conditions of growth, distribution and types. Beneficial for U.G. & P.G. students

1. Dr. MeenakshiPrasad
Assistant Professor
P.G. Department of
Geography
M.U, BodhGaya

2. Contents :
•Definition of Coral
Reef
•Distribution of Coral
Reefs
•Conditions for
Growth of Coral
Reefs
•Types of Coral Reefs
Source : googleimages

3. DEFINITION
•Coral reefs are masses of limestone & dolomite
accumulated by lime secreting organisms known
as coral polyps which are a kind of sea anemone
which can be of various colours.
•It has a ridge like shape with a broad base & a
tapering top which gets flattened by the action of
sea waves
•Live coral polyps are found at its top
•They are located close to the coast & separated
by it by a lagoon

4. DISTRIBUTION
•Coral reefs are found along the eastern margins of the
continents between 30
0
N & 30
0
S latitudes leaving the
equatorial latitudes, i.e. area lying between 5
0
N to 5
0
S
latitudes.
•They develop on the continental shelves or sub-marine
platforms at suitable depths

5. •Some old coral reefs are found up to 37
0
latitudes
which is explained by climatic change & continental
drift
There are two major areas of coral reefs in the world:
•Caribbean sea
•India ocean & Western Pacific ocean
Contd……
Source : googleimages

6. CONDITIONS FOR GROWTH
•Temperature –Ideal temperature for the growth
of coral polyps is 20
0
C, but under specific
conditions they can also develop between the
temperature of 18
0
C -25
0
C
•Depth of Sea –The ideal depth of sea water for
the growth of coral reef is 45-55 m but it can also
develop till a depth of 90 m. The reefs cannot
develop if the depth of the water is less than 10
m. The reef can develop till the depth where the
sun light is able to penetrate the water and
where planktons can grow.

7. •Salinity –Sea water
having a salinity of 27%
0
to 40%
0creates ideal
conditions for the growth
of coral polyps. High
saline water is injurious &
uncongenial for coral
growth due to the lack of
carbonate of lime in it
which is the main food of
these organisms. Fresh
water is also harmful and
kills the coral polyps
Source : googleimages

8. •Sediment free water –The living corals
demand a sediment free water as turbidity is
an important factor limiting their growth.
Sediments clog the mouth of the coral polyps
killing them which stunts the growth of the
reef.
•Presence of Plankton –Planktons are food for
coral polyps, thus their availability is
important for the growth of coral reefs.

9. •Existence of Sub-marine benches or platforms-
Another condition for the growth of a coral
reef is the existence of a sub-marine bench or
a platform at an ideal depth on which corals
start their colonies.
Source : googleimages

10. •Those polyps which find ideal conditions of
growth & ideal resting places start their colonies.
They then grow in two ways –
➢Upwards till they reach the low tide level
➢Outwards from the land due to the abundance
of food gained in the open sea. This outward
growth determines the width of the coral reef
•Consequently, a shallow water lagoon develops
in between the land and the reef as the coral
polyps on the landward side of the reef are
killed due to excess of sediments in the
motionless water of the lagoon
•The width of the lagoon increases with the
growth of the coral reef & the erosion of the
landward side of the reef

12. Fringing Reef
•The reef that develops
along the coast is called a
fringing reef
•They are narrow in width
•Their thickness is between
50-55 m & their seaward
edge is slightly higher than
their landward portion
•They have gentle landward
& seaward slopes
Source : googleimages

13. •They are separated from the land by a narrow lagoon
which has a depth of 0.3-1.5 m. This is known as a
boat channel
•The surface of the lagoon contains pieces of coral
rocks along with a mixture of clay & soil and
gradually become shallower with time
•Examples of such reefs are found along the coast of
Southern Florida (U.S.A) & Andaman & Nicobar
islands

14. Barrier Reef
•Barrier reefs also develop along the coasts but at a
greater distance from it as compared to the fringing
reef

15. •The thickness of a barrier reef is greater than
that of a fringing reef. On an average it is more
than 50m and can be as high as 150m. The
maximum thickness of Great Barrier Reef is 180
m.
•Its lagoon is also comparatively deeper &
broader. The depth of the lagoon can be till 50 m.
•Both the seaward & landward slope of a barrier
reef are steep.
•The best example of a barrier reef is ‘Great
Barrier Reef’

16. Great Barrier Reef
•Largest barrier reef in the
world
•Located off the east coast
of Australia between 9
0
S
to 22
0
S latitudes &
stretches for a length of
1920 km
•The average depth of the
lagoon is 240’ while its
width ranges between 11-
128 km
Source : googleimages

17. Atoll
•A ring of narrow growing corals of horse-shoe
shape is called an atoll

18. •They generally develop around an island or on
a sub-marine platform in an elliptical shape
•These are the thickest of all the reefs. At Tahiti
island their thickness is in thousands of
meters
•They have the deepest of lagoons. The depth
of the lagoon ranges between 240-420’.
•Both their seaward & landward slopes are
steep
•Examples are Funafuti atoll & Bikini island in
South Pacific Ocean

19. Types of Atolls
•Atolls are divided into 3 categories:
1.True atoll characterisedby circular reef
enclosing a shallow lagoon but without island
Source : googleimages

20. 2. Island atoll having an island in the central part
of the lagoon enclosed by circular reef
Source : googleimages

21. 3. Coral island or atoll island which does not
have an island in the beginning but later on
island is formed due to erosion & deposition
by sea waves
•Chains of small atolls having shallow small
lagoons are called faros

22. •Except the island atolls
all types of coral reefs
become submerged
during high tide.
•Coral reefs are usually
broken at many places
through which the
lagoon have contact with
the open seas & oceans.
These breaks are called
tidal inlets
Source : googleimages

24. REFERENCES:
•Sharma, R.C. & Vatal, M. : Oceanography for
Geographers, ChaitanyaPublishing House,
Allahabad, 1995
•Singh. S : Physical Geography, PrayagPustak
Bhawan, Allahabad,2012