Waterfalls have fascinated human beings
from the beginning. They are of the most beautiful of natural phenomena. From
ancient times waterfalls have struck awe to those who see them and several have
various legends and historical events associated with them.
Sri Lanka in comparison to its size has
perhaps the largest number of waterfalls of any country in the world. They constitute
about a hundred' some of great height and others only' a few meters' Perhaps no
country has neglected its waterfalls as much that they are in jungles without even
a foot – path leading to them. The vegetation round many falls has been
denuded. Sri Lanka's highest waterfall. The Bambarakande Falls (263 m), a sight
of the most exquisite beauty is still known only to a few, even though it is a
bare 4 miles off the main road from Colombo to Bandarawela. Meny still believe
that Diyaluma (220 m) is the highest waterfall in Sri Lanka.
Several
geographical factors are necessary for there to be an abundance of waterfalls
in any Country. Sri Lanka is fortunate in that all these factors are found in
the central highlands of the island.
Firstly, the geological formation of the land has to be such that there is a sharp upthrust of the earth's surface resulting in several
clearly defined peneplains with precipitous edges. Secondly, there should be
plenty of rainfall so that the rivers with the, waterfalls are always carrying
a large amount of water. A fall is at its best when there is a large volume of
water rushing over its lip. Finally, a thick vegetation surrounding a waterfall
always adds to its beauty. These factors are dealt with in detail in the following paragraphs.
The geological
structure of Ceylon shows three distinct
peneplains a coastel penepl of about 1,500 feet above sea level. A second
peneplain at about 4,400 feet and a third peneplain about 6,000 feet. These
peneplains are very marked and have been caused by a series of upward thrusts
of the land surface millions of years ago. Two different theories have been
advanced as to how and when these upward thrusts took place. Whatever its
origins Sri lanka's tree peneplains are sharply divided from each other.
The division
between the second and third peneplains is sharply marked particularly on the
southern and eastern edges of the third peneplain. The is an almost wall like
escarpment rising to over 3,500 feet above the low lands of the second
peneplain on the southern part of the central highlands. This escarpment starts
at the foot of Adam's Peak (7,300 feet) and proceeds to Wellawaya at the foot
of the great Haputale scarp (5,000 feet). Some of our highest waterfalls are
over this cliff wall, e.g., Aberdeen. Laxapana,Kirindi Ella. Bambaralanda,
Diyaluma, Rawanella, etc. This horst or upward thrust land mass surrounded by
depressed land is also evident on the eastern border of the highlands at a
lesser height falling abruptly into the Uma Oya, a tributary of the Mahaweli.
The Dunhinda. Manawela. Kurundu and Victoria falls are features of this
escarpment. There are no waterfalls on the northern face of the horst. There is
also an internal faulting in the central horst in the watawala Ragala area on the
third or highest peneplain. Here we find the Devon Ramboda. Elgin, Parawella
and St. Claire falls.