Ceylon; an Account of the Island Physical, Historical, and: Topographical with Notices of Its Natural History, Antiquities and; Productions, Volume 1Tennent, James Emerson, Sir
History
Ceylon; an Account of the Island Physical, Historical, and: Topographical with Notices of Its Natural History, Antiquities and; Productions, Volume 1
Tennent, James Emerson, Sir
Natural history -- Sri Lanka; Sri Lanka
In addition to these, there are a number of large rivers which belong
entirely to the plains in the northern and south-eastern portions of the
island, the principal of which are the Arive and the Moderegam, which
flow into the Gulf of Manaar; the Kala-oya and the Kanda-lady, which
empty themselves into the Bay of Calpentyn; the Maniek or Kattragam, and
the Koombookgam, opposite to the Little Bass rocks and the Naveloor, the
Chadawak, and Arookgam, south of Batticaloa. The extent of country
drained by these latter streams is little short of thirteen thousand
square miles.
Very few of the rivers of Ceylon are navigable, and these only by canoes
and flat-bottomed paddy boats, which ascend some of the largest for
short distances, till impeded by the rapids, occasioned by rocks in the
lowest range of the hills. In this way the Niwalle at Matura can be
ascended for about fifteen miles, as far as Wellehara; the Kalu-ganga
can be traversed from Caltura to Ratnapoora; the Bentotte river for
sixteen miles to Pittagalla; and the Kalany from Colombo to the foot of
the mountains near Ambogammoa. The Mahawelli-ganga is navigable from
Trincomalie to within a short distance of Kanda[1]; and many of the
lesser streams, the Kirinde and Wellawey in the south, and the Kaymel,
the Dedroo-oya, and the Aripo river on the west of the island, are used
for short distances by boats.
[Footnote 1: For an account of the capabilities of the Mahawelli-ganga,
as regards navigation, see BROOKE'S _Report, Roy. Geog. Journ._ vol.
iii. p. 223. and _post_, Vol. II. p. 423.]
All these streams are liable, during the fury of the monsoons, to be
surcharged with rain till they overflow their banks, and spread in wide
inundations over the level country. On the subsidence of these waters,
the intense heat of the sun acting on the surface they leave deserted,
produces a noxious and fatal malaria. Hence the rivers of Ceylon present
the curious anomaly, that whilst the tanks and reservoirs of the
interior diffuse a healthful coolness around, the running water of the
rivers is prolific of fevers; and in some seasons so deadly is the
pestilence that the Malabar coolies, as well as the native peasantry,
betake themselves to precipitate flight.[1]
[Footnote 1: It has been remarked along the Mahawelli-ganga, a few miles
from Kandy, that during the deadly season, after the subsidence of the
rains, the jungle fever generally attacks one face of the hills through
which it winds, leading the opposite side entirely exempted, as if the
poisonous vapour, being carried by the current of air, affected only
those aspects against which it directly impinged.]
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