Sea Caves, Flank Margin Caves and Tufa Caves Observed on Antalya Coastal Cliffs

Abstract

ABSTRACT DIPOVA, N and OKUDAN, E.S., 2011. Sea Caves, Flank Margin Caves and Tufa Caves Observed on Antalya Coastal Cliffs. In: Micallef, A. (ed.), MCRR3-2010 Conference Proceedings, Journal of Coastal Research, Special Issue, No. 61, pp. 382–386. Grosseto, Tuscany, Italy, ISSN 0749-0208. The caves on Antalya cliffs are of three origin; sea caves, tufa caves and flank margin caves. Sea caves are formed due to wave action on weak parts of the rock. Because the rocks of the Antalya cliffs are heterogeneous and strength varies in a wide range, weak parts of the cliffs are susceptible to cave formation. Tufa caves occurred as blind holes behind tufa curtains which deposited on tufa cascade environment of deposition. The obvious distinguishing features of tufa caves are primary sedimentary structures instead of corrosion morphologies. The flank margin caves occurred due to mixing corrosion at sea and groundwater interface. In this study more attention has been paid on porosity development and related cave form...