The jaffna peninsula is situated in the extreme north of Srilanka
(map 1).it covers the entire jaffna District. Pachilapalli AGA Division
of the Kilinochchi District, which was temporarily attached to the jaffna
District earlier, has been transferred back. There are and large islands
around the peninsula. The peninsula is linked with the southern mainland
at Elephant pass. The total area of the peninsula is 1,129.9 sq. km of
which lagoons cover 45.7 sq. km.
Geographically
jaffna peninsula is divided into 4 sub-regions.
1. lslands
2. Vadamarachchi
3. Thenmarachchi and pachilapalli
4. Valikamam
T he
climate is tropical dry zone with temperatures ranging from 26C to 30
C. The highest temperature is normally recorded in the months of April
and May. Annual precipitation ranges from 696 mm to 1.125 mm. it is fairly
spread to 1,125 mm. it is fairly evenly spread over the area but the North
East Monsoon rains from October to December account for 90% of the annual
rainfalls.
The
dominant feature is a long stretch of water, forming an internal lagoon,
which divides the area almost into two, with the northern outlet at Thondamanaru
and the southern outlet at Ariyalai. The area is flat and of low elevation
except in the northern central part of the western sector,in the area
around Tellipalai, where the
elevation rises up to 10.5 M above M.S.L.
from here it slopes down gently twards the south and south-east, but to
the north the elevation tends to drop abruptly towards the sea.
The
soil pattern of the peninsula varies from reddish brown to sandy tracts.
The reddish brown soil, which dominates in North Western and North Eastern
areas, has the best potential for cultivation of up-land crops and fruits.
Sand dunes are generally found in the north and the south. Some of the
sand dunes reach even an elevation of 15 m above M.S.L Further to the
south the area between kodikamam and Elephant pass becomes low and flat
with sandy soils. the low land soil is gray. Areas bordering the lagoons
are cored with saline and alkaline soils..
Jaffna peninsula is divided into two agro-ecological
zones (panabokke and kannangara 1975). The main distinguishing characteristic
of each of these zones, that the land use for agricultural purpose, for
crops like paddy, vegetables, fruit trees, coconut and Palmyra, has declined
by 14 per cent between 1986 and 2001. lt was 44,160 hectares in year 1986
declined to 38,347 hectares in 2001. The notable feature is the land with
arable crops has been declined by 25 per cent, fruit crops by 22 percent
and coconut by 37%. Lt has been estimated that about 5.800 hectares of
lands have been abandoned due to unstable conditions over the last 15
years. Buildings and roads cover 21.3% of the land use in 1986 remains
more or less constant through out. the balance extent of land is composed
of sadly scrap jungle and barren lands. Although these lands have no economic
use, substantial investment is required to convert these lands for cultivation
by soil recondite toning and regenerating etc. and also choice of appropriate
crops of salt tolerance varieties.
There
is no river in the peninsula. Therefore, surface water for domestic and
agricultural purposes is scarce. However, there are over 1,000 ponds scattered
all over the peninsula, which are replenished during the rainy season.
Most of them serve agricultural purposes, but some
of them are also used
for domestic water supply and feeding livestock. These ponds also increase
the aquifer reserves (map 3) as water percolates through the limestone
into the underground. A distinctive feature of the peninsula is the underground
formation of limestone. Due to this natural geological formation ground
water is available at depths of 6 to 14 meters. The water is extracted
through open dug wells constructed by the inhabitants for their domestic
and agricultural purposes.
So
far no comprehensive hydrology cal survey has been carried out to assess
the quantity and quality of water available. in some areas water has been
extracted excessively, resulting in increased salinity seasonally in some
areas and permanently in others. Especially in areas close to the sea
there is a high risk of salt water intruding into the fresh water permanently.
Apart
from all the conflict related social and economic problems and constraints
water is or will be one of the most limiting factors of development in
the future if the status quo is maintained. The need is to get all water
user to a common forum and work out strategies to overcome shortages and
pollution of freshwater.
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