Titlebook: Landscapes and Landforms of the Czech Republic; Tomá? Pánek,Jan Hradecky Book 2016 Springer International Publishing AG, part of Springer

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Long-Term Geomorphological History of the Czech Republicajority of its area and changing climatic pattern resulting in the evolution of a staircase of river terraces, continental and mountain glaciation, loess accumulation and the development of various periglacial landforms. Holocene landscape evolution is under the dominance of fluvial and slope proces

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Lacunar-Stroke

Brdy Highland: A Landscape Shaped in the Periglacial Zone of Quaternary Glacialsblic, Brdy Highland receives less precipitation and fluvial processes have had a less pronounced effect on its morphology. The relics of pre-Quaternary planated surface forming the summit of the highland were dissected into structural-erosional ridges mainly by processes operating in the periglacial

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Morphology of the Youngest Little Volcanoes in Western Bohemian Massifnt earthquake swarms with frequent repetition and magnitudes up to M4.5 in the nearby region of the Cheb Basin and surroundings. The little volcanoes were, anyway, a subject of investigation for centuries. The most famous is the research performed by J.W. Goethe, a worldwide known poet and scientist

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The Kru?né Hory Mts.—The Longest Mountain Range of the Czech Republic activity. First, this activity was focused on mining of rich mineral deposits (silver, tin, lead, copper and other ores). Subsequently, the inhabitants of the mountain range changed their focus to manufacturing and agriculture, which is illustrated by technical monuments and agricultural landforms.

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Elbe Sandstonesthe typical rock city called the Tiské Stěny Cliffs belong to other interesting places here. The landscape is unique not only because of its geomorphic diversity but also because of the close relationship between the living and inanimate nature and the presence of relicts after ancient settlement. A

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Bohemian Paradise: Sandstone Landscape in the Foreland of a Major Faultd wilderness in an agriculturally utilized land. They became attractive for vacationers and tourists as early as in the mid nineteenth century, and for climbers from the early twentieth century. The Bohemian Paradise was proclaimed a Protected Landscape Area in 1955 and entered the network of Europe