Neovulkanity Českého středohoří a jejich geovědně turistický potenciál

Abstract

This work is focused on the area of the České středohoří Mts. and its beauties, both tourists and geology. In the first part deal with the geologic and geomorphologic evolution of the whole whose relief is the result of tertiary volcanic activity and the effect of exogenous factors, especially the river Elbe. Along the fault trough called Eger Graben there is output of magma. Mountains are built up from subsurface and surface bodies tertiary volcanic rocks which strike through chalk ground sediments. The second part contains a list of my proposed characteristic peaks and the geological formations of the České středohoří Mts. formed by long-term process and describes their importance and especially attractive for tourism and geology.