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ACCOUNT OF THE LAND, in brief...
The Island of Sri Lanka or Ceylon, as it
was known till 1972, is situated off the south eastern tip of the Indian
subcontinent between the longitudes 80 and 82 degrees east and the
latitudes 6 and 10 degrees north. Its maximum length is 432 kilometers
from north to south and its maximum width is 224 kilometers from east to
west; it has an area of 65,525 square kilometers. Its exclusive maritime
economic zone extends over an area of 517,400 square kilometers of Indian
Ocean rich in living and non living resources.
She possesses tropical beaches, ancient
monuments, rain forests, gorgeous waterfalls and many places to delight
any person. The typically tropical climate with an average temperature of
270C fluctuates between 150 C in the highlands to 350C
in certain areas of the lowlands.
Its relief is characterized by a south
central hill country and by lowlands stretching away from the hills to the
coasts right round the island. There are 14 peaks rising more than 2000
meters above mean sea level the most famous of which is Sri Pada or Sacred
Foot Print (of Gautama Buddha); westerners call it Adam’s Peak.
The island is visited by the south west
monsoon from May to September and the north east monsoon from December to
February while there are two inter-monsoon periods in March-April and
October-December. The land is drained by a number of rivers of which 16
are more than 100 metres long, the longest being the Mahaweli Ganga (335
kilometers).
The monsoons and the relief create a
rainfall pattern which divides the island into three agro-ecological zones
viz. The wet zone, the dry zone and the intermediate zone. The south west
quadrant of the island approximates to the wet zone where agriculture is
possible throughout year on rainfall alone but this zone is not as
suitable as the dry zone, if irrigation is provided, for the cultivation
of rice, the staple food of the people. Most of Badulla District, the
northern half of Moneragala District and the easternmost areas of Kandy
and Nuwara Eliya are in the intermediate zone as are substantial areas in
the south of Puttalama, Kurunegala and Matale Districts. The rest of the
country, other than the peninsula of Jaffnapatnam in the north, is the dry
zone proper with a period of severe drought from May to September and
where (surface) irrigation is needed for agriculture on a sustained basis;
Jaffnapatnam is an exception in that it is underlain by miocene limestone
with aquifers which store rainfall (and therefore not part of the dry
zone) that give the Peninsula an abundance of ground water supporting
intensive farming and a dense population.
All the above factors have determined
human settlement and land use in the island during the whole course of its
recorded history. This commences with an account of an Indo-Aryan
immigration from North India in the sixth century B.C., who in the course
of time assimilated pre-historic tribes known as Yakkhas, the remnants of
whom are known now as Veddas.
The Sinhalese exploited climate and
topography to develop an irrigation system of a magnitude and complexity
never known in any part of the Indian sub-continent.
The account in the Mahavamsa, the
principal historical chronicle of the Sinhalese, of this Indo-Aryan
immigration and occupation thereafter is corroborated by the discovery at
Anuradhapura of Prakrit writing in the Brahmi script which has been
reliably dated to a period between 600 and 500 B.C. These immigrants were
the first Sinhalese; they gave the island its first historically known
government and its historically best known name Sinhaladipa or "the
Island of the Sinhalese". All the Sinhalese were converted to
Theravada Buddhism in the years after its formal introduction in the 3rd
century B.C. Even today, the Sinhalese are 74% of the total population
(1993 estimate :17.6 million) while 69.3% of the total are Buddhist by
religion despite nearly 5 centuries of conversion and proselytising.
The Greeks called the island Taprobane
which is derived from the Sanskrit Tamraparni. The Pali form was
Tambapanni. In India it was also called Lanka ("beautiful").
"However, the European name of Ceylon derives from the ancient name
of the Sinhalese The Portugese Ceilao, our Ceylon and the Arabic Serendib
all stem from the Pali Sihala or Sihaladipa ‘the Island of the Sinhalese’,
and until 1815 the kingdom was known as Simhala or Tri-Simhala"
(Prof. Heinz Bechert, Wilhelm Geiger – His life and Works, 2nd
Edition, p.1; see also H.W.Codrington, A Short History of Ceylon
p.1) The Tamil name for the island Ilam or Eelam is also derived from the
name Sinhala (The Tamil Lexicon of the University of Madras, p.382;
Codrington, op.cit.p.1.)
Land Use
The following table shows the extents
under the principal forms of land use:
| USE |
|
EXTENT (hectares) |
| Paddy |
|
500,000 |
| Coconut |
|
417,000 |
| Tea |
|
190,000 |
| Rubber |
|
163,000 |
| Forest |
|
2,119,000 |
MINERALS
High quality crucible steel was made by
the Sinhalese in mediaeval times. Steel from Sri Lanka was used to make
the blade of the famous Damascus sword of the Arabs. There is very little
exploitation of iron ore now though there are reserves of over 2.2 million
tons. The well known mineral sands deposits north of Trincomalee bear
reserves of 4 million tons with 70% ilmenite. There are also recently
discovered reserves of 3 million tons of ilmenite, 6 million tons of
rutile and 4 million tons of zircon in another belt north of Trincomalee.
Sri Lanka has the best graphite in the world with 97-99% carbon. There are
vast reserves but only 8000 to 10000 tons are exported annually. Other
than a limited production of pencils there are no graphite industries.
There are also large reserves of mica, kaolin, feldspar, quartz and silica
sands, all of high quality. Miocene limestone is the base of the cement
industry in the island. A large reserve of apatite near Anuradhapura could
be exploited for the production of rock phosphate. There are large
reserves of dolomite and marble.
Sri Lanka is one of the first five gem
bearing countries in the world, the other being Brazil, Myanmar, South
Africa and Thailand. The principal gems are rubies and sapphires while
alexandrite, though not so profuse, is found only in Sri Lanka and in the
Ural mountains of the former Soviet Union.
The Coast and the Ocean
Until the Dutch took possession of the
entire sea board consequent to the Sinhala-Dutch Treaty of 14th
February 1766, the Kandyan Sinhala Kingdom had as its major ports
Puttalama in the north west and Trincomalee, Kodiyarama (both on
Trincomalee Bay) and Batticaloa (Sinh. Mada Kalapuwa or "muddy
lagoon") in the east. Trincomalee is one of the largest and safest
natural harbours in the world. The principal modern ports are Colombo,
Galle and Trincomalee. Sri Lanka’s location on the globe with a harbour
such as Trincomalee gave it an unparalleled strategic importance in the
past and gives it an even greater importance today. Strategically the
island holds the key to the Indian sub-continent to the north and the
Indian Ocean to the east, south and the west. Sinhaladipa is an attraction
to subversion by external and internal forces.
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