Characterising the Ongole Coastal Dunefield of SE India: Formation and Temporal Constraints
Authors
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CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad - 500 007
Devender Kumar -
CSIR-National Geophysical Research Institute, Uppal Road, Hyderabad - 500 007
Dontireddy Venkat Reddy
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Department of Geography, Environment and Geomatics, University of Guelph, ON
Robin Davidson-Arnott
DOI:
https://doi.org/10.1007/s12594-020-1603-0Keywords:
No Keywords.Abstract
The Ongole coastal dunefield (OCD) is about 20 km long and 2.5 to 3 km wide, and is located to the east of Ongole town between the mouth of the Paleru river in the south and a small creek in the north. Much of the dunefield lies 3-5 m above sea level with some large dune ridges reaching 10-12 m. The area landward of the dune field consists of an extensive marsh. Optically stimulated luminescence (OSL) dating of 12 sub-surface sediments from three sites near the western edge of the dunefield gives almost concurrent age of 5.1 ± 0.4 ka. Radiocarbon dating of one shell from a similar location also corroborates the OSL age while the age of another shell taken closer from the modern shoreline gives a date of 3.29 ± 0.5 ka. The age of the deposits and morphology of the dunefield indicate that it was probably initiated on some form of barrier system at the end of the Holocene transgression.
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