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

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发表于 2025-3-21 17:56:50 | 显示全部楼层 |阅读模式
书目名称Landscapes and Landforms of the Czech Republic
编辑Tomáš Pánek,Jan Hradecký
视频video
概述Presents high geomorphic diversity of the Central European landscape.Detailed modern information on geomorphosites.Enables comparison of landforms of the Bohemian Massif and the Western Carpathians.In
丛书名称World Geomorphological Landscapes
图书封面Titlebook: Landscapes and Landforms of the Czech Republic;  Tomáš Pánek,Jan Hradecký Book 2016 Springer International Publishing AG, part of Springer
描述.The book aims to present the unique geomorphological landscapes of the Czech Republic. The geomorphic uniqueness of this country benefits from the proximity to two distinct European geological domains: the old cratonized Bohemian Massif and the relatively young Tertiary fold and thrust belt of the Western Carpathians..Landscapes and Landforms of the Czech Republic. introduces general physiographical characteristics of the landscape and presents the main driving factors leading to the evolution of the present landscape. The book contains twenty two chapters describing the most interesting geomorphic landscapes of the Czech Republic. The selection of individual landscapes was based on visual exceptionality (e.g. sandstone landscapes of the Northern Bohemia), scientific importance (e.g. patterned grounds in the Sudetic Mountains) and historical relevance (e.g. mining of the Nízký and Hrubý Jeseník Mountains). The final chapters of the book discuss the protection of geomorphic heritage in the Czech Republic..
出版日期Book 2016
关键词Bohemian Massif; Carpathian Mountains Geomorphology; Czech Republic; European Landforms; Geomorphic Proc
版次1
doihttps://doi.org/10.1007/978-3-319-27537-6
isbn_softcover978-3-319-80165-0
isbn_ebook978-3-319-27537-6Series ISSN 2213-2090 Series E-ISSN 2213-2104
issn_series 2213-2090
copyrightSpringer International Publishing AG, part of Springer Nature 2016
The information of publication is updating

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Climate in the Past and Present in the Czech Lands in the Central European Contextnental types of temperate climate. The climate changed during geological history and various climates played an important role in the evolution of landforms due to changes in type and intensity of weathering and earth surface processes. This chapter describes general trends in climate oscillations d
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Long-Term Geomorphological History of the Czech Republicgh diversity of landforms. Major geomorphological features of the Czech Republic are the result of Late Paleozoic Variscan orogenetic processes, Late Cretaceous marine transgression, Alpine tectonics since the Late Cretaceous and Cenozoic neovolcanic processes. Geomorphological history of the Bohemi
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The Bohemian Karst: A Condensed Record of Landscape and Living Nature Evolutionwer Paleozoic strata, folded and faulted during the Variscan Orogeny, have yielded thousands of fossil species. Well-exposed sedimentary rocks enabled definition of five international stratotype and/or parastratotype sections of geological boundaries. Most of the karst forms are inactive and largely
发表于 2025-3-22 15:54:14 | 显示全部楼层
Brdy Highland: A Landscape Shaped in the Periglacial Zone of Quaternary Glacialsand along the borders of the country. Because of the existence of a military training ground in its highest part, Brdy Highland is the least known of all the Czech mountains and highlands. Termination of military use of the area by January 2016 opened the area to the public. Quartz-dominated Cambria
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Bohemian Forest : Landscape and People on the Frontierrest. Three types of relief are typical. First, an extensive plateau covered with peat bogs spreading out in the central part of the area. Second, canyon valleys incised in the edge of the plateaus with torrential flows in rocky and stony riverbeds and finally, a rugged glacial relief with glacial c
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Elbe Sandstonesdscape with plateaus, deep canyons, rock cities and a wide range of small landforms developed on massive quartzose sandstone deposits mostly of Middle Turonian age. The region has special status compared to other similar areas by its large areal extent, its vertical diversity causing the high-energy
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