Evidence
points to tectonic activity in Lanka
By S.U. Deraniyagala
Investigations conducted by the Archaeological Department
under the direction of the writer in 1969-72 revealed traces of
prehistoric human activity within coastal alluvia. Gravels and stone
tools had been deposited at levels corresponding with the then existing
sea levels.
The
gravels with artifacts are today at considerable heights above the
present sea level -15 metres at Bundala-Patirajawela dating back
to 125,000 years and 8 metres at Bundala-Wellegangoda dating back
to 80,000 years. Occurrences of ancient coastal gravels inland around
Mankulam and on Aruakallu at 60-80 metres and at Minihagalkanda
in Yala at 40 metres have yet to be scientifically dated. This phenomenon
of uplifted shores has been attributed principally to pressures
generated by tectonic factors within the past one million years
or so as indicated by the presence of man-made tools within the
gravels.
These
findings were presented in publications of the universities of Cornell
and Harvard in the U.S.A. and the Archaeological Department (Deraniyagala
1976, 1988, 1992). They were contrary to the prevailing view that
Sri Lanka is situated in a stable tectonic environment.
An
article by Professor C.B. Dissanayake on South Asian plate tectonics
(the Daily News of December 31, 2004) corroborated the geo-archaeological
evidence that was secured some thirty-five years ago and claimed
that Sri Lanka was indeed in a region of potential tectonic instability.
Study
of coastal uplift
In view of these indications, it is a matter of urgency
that the rates of coastal uplift in Sri Lanka be investigated scientifically,
using state-of-the-art methods. The locations for sampling have
already been mapped out by the Archaeological Department and Dr
Mohan Abeyratne, a scientist attached to the Central Cultural Fund
trained at the Australian National University in radiometrically
dating the sediments.
What
is needed at present is the equipment for 'optically stimulated
luminescence' testing. A project proposal has been submitted by
Dr. Abeyratne to the Atomic Energy Authority and an estimate prepared
for procuring the equipment. It is now necessary to implement an
enhanced version of it; and, since the dating techniques are being
regularly upgraded, a back-up from international scientific institutions
and consultants would probably be needed.
This
project could constitute an important component of the proposed
Indian Ocean-rim earthquake monitoring programme. Since the said
project is of direct relevance to risk assessment in developing
the coastal regions of Sri Lanka, its rapid implementation should
be a national priority.
(The
writer is a former Director- General of Archaeology.) |