XVI INQUA Congress
Paper No. 92-1
Presentation Time: 1:30 PM-4:30 PM

QUATERNARY SEA LEVEL CHANGES ALONG THE COAST OF TAMILNADU,INDIA

KUMARESAN, Anbarasu Sr, Department of Geology, National College, Karumandapam, Dindigul Road, Tiruchirapalli, 620001, India, anbarasu_gk@yahoo.com and KHAN, Feroze

Introduction : East coast of India –emergence type – mostly littoral low lands- living corals in two places – suitable for the study of sea level changes.

Study area : Tamilnadu- southern part of east coast of India

Geomorphology: Width of the Coastal plains ranges from few meters to 80 Km- beaches, beach ridges, cheniers, terraces, mudflat, lagoons, raised corals, spits and bars etc. Tectonism: Evidences for neotectonism are present in the form of cymatogenic downwarping

Sea level indicators :

Geomorphic -

Beach ridge plains around Vedaranyam – 1,25,000 years BP (TL Date) Beach ridge plains around Chidambaram -Marine terraces around Pondicherry-Raised corals in Rameshwaram island- Barrier ridges around Marakkanam - 6000yearsBP

Archealogic - Submerged Roman fort in Arikamedu – 1,850 - 1,700 BP Submerged town of Kaveripatnam - 1,900 - 1,700 BP Quaternary sea level history:

Events Age Indicator

Transgression I maximum 1,25,000 years BP Cheniers

Transgression II maximum 6,000 years BP Younger beach ridges Regression minimum 1,900 – 1,700BP Developmentofancient cities and ports in reclaimed land area. On going transgression From 1500 years BP submergence of the developed cities and ports under water

XVI INQUA Congress
General Information for this Meeting
Session No. 92--Booth# 65
Quaternary Sea Level Changes and Their Physical Biological and Oceanic Impacts (Posters)
Reno Hilton Resort and Conference Center: Pavilion
1:30 PM-4:30 PM, Wednesday, July 30, 2003

Geological Society of America Abstracts with Programs, , p. 238

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