Kamenice - Tobogán, author: Jan Mertlík

Water has always been a significant geological agent perpetually affecting the surface of our planet. It markedly contributes to chemical and mechanical weathering of minerals and rocks, their transport to other locations, and finally to their re-deposition in the form of sedimentary rocks. The activity of water is also responsible for the origin of many geotouristically attractive sites, such as caves and rock cities.


The territory of the Geopark features a number of springs, and also hosts the headwaters of several minor streams.

18.2.2020 14:53:09 | read 1549x | sprokesova | Full article


Erosional activity of water has been always of great significance in shaping the landscape and creation of specific geomorphology in the Geopark.

18.2.2020 14:53:25 - updated 28.2.2020 22:48:18 | read 3482x | sprokesova | Full article

Stream Deposits

Depositional activity of water is a logical counterpart to its erosional activity.

18.2.2020 14:53:42 - updated 28.2.2020 22:49:08 | read 1298x | sprokesova | Full article
Created 20.6.2019 14:02:42 | read 2002x | tana
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