ABRÁZIÓS BARLANGOK KIALAKULÁSA ÉS FORMAKINCSE KÜLÖNBÖZŐ KŐZETSZERKEZETŲ BAZALTLÁVÁKBAN ÉS PIROKLASZTITOKBAN.

The aim of this study to demonstrate that how, and in which form sea caves develop in structurally different basaltic lavas and pyroclastites of these kinds. Also influenced by marine erosion, the dimensions and morphology of sea caves principally depend on the structural behaviour of the enclosing basaltic lavas and pyroclastics. In basalt volcanic areas sea caves can form in columnar and irregularly jointed basaltic lava; through opening up and further shaping of primarily existing caverns; in lava deltas; by the excavation of embedded volcanic agglomerate or slack structured aa lava from between thick and primarily existing caverns; in pillow lava; in basaltic dyke; along the border of a basaltic dyke and thick hydrovolcanic tuff and in basaltic tuff. The aim of this study is to demonstrate that how and in which form sea caves develop in structurally different basaltic lavas and pyroclastics. [ABSTRACT FROM AUTHOR]