Textural data of 60 samples of bottom sediments, from 20 transects (approxi
mately 0.5 km apart) collected from the Vellar estuary, indicate that sand
is predominant at the head of the estuary with silt and clay as subordinate
constituents. The proportion of sand decreases towards the confluence. The
silt content is comparatively fewer than the clay content in the downstrea
m direction. However, the central part of the estuary shows a decreasing tr
end of sand and an increasing trend of clay content. The log-probability pl
ots suggest that all the three segments (i.e. the northern, central and sou
thern sides), of the estuary show an average of one traction population, th
ree saltation and four suspension populations. The variations in textural c
haracters suggest that tidal activity has significantly affected the sedime
nt population and the minor disturbances of other transporting agencies mig
ht have affected the depositional process which are marked in the deposited
sediments.