Directional analysis of drainage network and morphotectonic features in the south-eastern part of Bükk Region

The fracture deformations often result in linear morphological elements (lineaments, valleys) on the surface. In many cases, direction of lineaments and valleys can be well followed by strike geological structural elements. Therefore, conclusions drawn from these directions for regional tectonic processes. Our work aimed to analyse relationship between valley lineament network south-eastern part Bükk Region. We prepared theoretical drainage map area. was examined separately eastern South-Eastern that is built up mainly Mesozoic limestone side Bükkalja area covered Neogene Quaternary sediments. Structural surveys were also performed seven sites measure joint sets. These results compared with valleys’ 2 km wide measurement sites. Based our results, it stated development influenced elements; however, there are local differences characteristics Bükkalja. study confirmed has great importance exploration