The sea covers 99% of the Maldives and inside its blue
depths lies the mysteries and riddles related to the formation of the Maldives.
The islands are formed around a ring shaped coral reef encircling a lagoon.
This reef structure, typical of Maldives, is called an Atoll. In fact, the
English word 'atoll' itself is derived from the Maldivian or Dhivehi word for
it - Atholhu. There are 26 natural atolls in the Maldives.
There are still ongoing debates about the formation of
atolls. According to Charles Darwin's theory, when submerged volcanoes rise
from the sea, a coral reef grew on its edge. When the volcanoes submerged, the
coral reefs encircling a water-filled basin remained. Consequently, islands
were formed on the reefs as the tides and currents brought dead coral onto
sandbars. These were in turn colonized by
plants.
A different view has been provided by Hans Hass.
According to him, layers of coral reefs might have built up on top of the
submerged mountains until they rose to the surface. The hardest and highest
corals remained while the weaker corals in the centre of the coral platforms
broke down. The remaining corals at the outer edges formed rings that were to
form the outer rims of atolls. Islands were formed as debris and sand
accumulated on to the remaining reefs.
The reef is cut by deep channels, which the locals have
mastered to navigate. Protective reefs safeguard the islands from the elements.
However, the islands are susceptible to erosion. The islands are low-lying;
emerging almost two meters above the sea level. It is frequent that one part of
the island to erode while onto another part the currents and tides deposit sand
expanding the island. Over the course of time, some islands may erode
completely, while others may be formed gradually on a sandbank. There are still
many islands and sandbanks at various stages of formation. Hence, the Maldives
is a dynamic country in the making.
Six inches deep humus forms the initial layers of the
soil. Sandstone of about 2 feet is found below and after it sand is accompanied
with fresh water. The salinity of the soil along the beach restricts the growth
to few plants. Normally, shrubs and small hedges occupy the area. More inwards,
banyan, mangroves, and other lush vegetation are found. For the coconut palms
there seems to be no restrictions. It is found almost everywhere and have
contributed significantly to the local lifestyle, even earning the status of
the national tree.
While vegetation in the islands is limited, it is
supplemented by the riches of the sea; varieties of corals, abundant colourful fish and other organisms
that makes the Maldives 'the home of the children of the sea'.
The ocean plays a major role in the climate of
the country. It acts as a heat buffer, storing and giving up heat at much
slower rate than solid ground. Temperature usually fluctuates between 23° C and
maximum 32° C. There is always a cooling breeze blowing in from the sea. The
Maldives straddles the equator and lies outside the India Ocean cyclone belt.
Some people find the Maldivian climate monotonous. Length of day never varies.
Normally in June and July the southwest monsoon is said to bring rain. In
reality, it can rain at any time.
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