The River Thames at Cholsey
We live about a 30 minute walk away from the River Thames in Oxfordshire. It is a beautiful stretch of water as it flows serenely through the meadows, fields and rolling hills making its way to London and the open sea. Despite its splendour it somehow lacks the supreme majesty of the Periyar river. We can spend hours just sitting and watching as the waters flow by.
The Periyar River framed by the Western Ghats
Paniyeli Poru near Malayattoor
With
its unique geography, monsoon climate, variable land use pattern, Kerala is
endowed with a highly diverse and plentiful bounty of aquatic habitats. None
more so than the Periyar which is the longest river in Kerala and is often
described as its ‘life line’. Its source is at an elevation of about 1830m in
the Sivagiri peaks of the Western Ghats on the border between the states of Kerala and
Tamil Nadu.
Periyar
means ‘big river’ which is entirely appropriate as it has a total length of about 244km, a maximum width of 405m and a catchment area of 5,398 km2. The total
annual flow is estimated to be 11607m3 and the average rainfall is
around 3000mm. In most of the areas of the river, about 60% of the rainfall is
experienced during the South West Monsoon and 25% during the North East monsoon
period. Along its journey to the Arabian Sea at Cochin the river is fed by many
tributaries rising across the Ghats.
From
its source the river flows north a short
distance to the Periyar Lake. This is an artificial
reservoir created by damming the river and stretches across an area of 31km2
at an elevation of about 850m. It is ringed by mountain peaks, and is
surrounded by the Periyar Tiger Reserve and wildlife sanctuary, famous for
its wild elephants and tigers.
The Periyar Lake at Thekkady within the Periyar Tiger Reserve
(note the elephant emerging from the trees)
From the lake the River continues to flow
generally north to where it is impounded by an arch dam at Idukki forming
another large reservoir that is a major source of hydroelectric power for
Kerala. The river continues northwest, descending out of the high plateau of
the mountains and the Cardamom Hills onto the coastal plain of the midlands, characterized
by an undulating topography with small hills separated by valleys. From here
the river turns west and crosses the narrow belt of the lowlands that runs almost
parallel to the shoreline. The lowlands are broad valleys, submerged lands with
swamps and marshes and sand dunes, many parts of which are directly connected
to the famous backwaters. Finally the river empties into the Arabian Sea about
24 km north of Kochi.
Bhoothathankettu Dam on the Periyar
The forests adjoining the river are comprised of wet-evergreen, semi-evergreen, moist deciduous, dry-deciduous and pure reed species. There are also areas of grass land, forest plantation and dense vegetation or ‘jungle’. Although about 35% of the area around the Periyar is forest, some of these areas have already been cleared for various developmental activities. In the highlands the major human activities are connected with plantation, hydroelectric projects, new settlements and building activities. While the plantation in the very high reaches are cardamom, tea and pepper, the foothills are cultivated with rubber, coconut and pepper. The midland belt has mainly fields of rice paddy, coconut and plantains.
The River at the high plateau amid tea bushes and running through the midlands
The
Periyar performs a pivotal role in shaping the economic prospects of Kerala, as
it helps in power generation, domestic water supply, irrigation, tourism,
industrial production, collection of various inorganic resources and fisheries.
Along its course the Periyar provides drinking
water for several major towns and generates a significant proportion of its
electrical power. It flows through the major region of industrial and
commercial activity as 25% of Kerala's industries lie along its banks, mostly to
the north of Kochi harbour.
However,
as in the case of many other inland bodies of water, the Periyar is gradually
undergoing eco-degradation due to various stresses that include indiscriminate
deforestation, domestic-agricultural-industrial water pollution, excessive
exploitation of resources, large scale sand mining, and various other interferences
in the flow of water.
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