The sediments of the beaches along the central coast of Tamil Nadu from
Pondicherry to Vedaranyam were studied for their textural variation. 108 sediment
samples collected from the low-, mid-, and high-tidal zones, as well as the berms
and dunes of different beach morpho-units were analysed. The study area was
divided into three sectors (northern, central and southern) on the basis of prevailing
energy conditions and oceanographic parameters. The poorly sorted, negatively
skewed, coarser sediments of the northern sector are indicative of denudational
processes taking place there. Medium-to-fine, moderately-to-well sorted, positivesymmetrically
skewed sediments dominate the central sector, probably as a result of
the influence of palaeo-sediments deposited by rivers from inland as well as by waves
and currents from offshore. Fine, poorly sorted, positive-symmetrically skewed
sediments dominate the southern sector, highlighting depositional processes. Linear Discriminant Function Analysis (LDF) of the samples indicates a shallow
marine environment origin for all the three sectors. These results show that
reworked sediments, submerged during the Holocene marine transgression, are
being deposited on present-day beaches by waves, currents and rivers in the study
area.
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