Bohemian Paradise: Sandstone Landscape in the Foreland of a Major Fault
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F16%3A00460126" target="_blank" >RIV/67985831:_____/16:00460126 - isvavai.cz</a>
Výsledek na webu
<a href="https://books.google.cz/books?id=Rui9CwAAQBAJ&printsec=frontcover&hl=cs&source=gbs_ViewAPI&redir_esc=y#v=onepage&q&f=false" target="_blank" >https://books.google.cz/books?id=Rui9CwAAQBAJ&printsec=frontcover&hl=cs&source=gbs_ViewAPI&redir_esc=y#v=onepage&q&f=false</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/978-3-319-27537-6_16" target="_blank" >10.1007/978-3-319-27537-6_16</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Bohemian Paradise: Sandstone Landscape in the Foreland of a Major Fault
Popis výsledku v původním jazyce
The region of Bohemian Paradise in NE Bohemia is the most varied sandstone landscape in the Bohemian Cretaceous Basin. This is caused by the complex stratigraphy of Cretaceous (Upper Turonian to Coniacian) sediments, abrupt lateral changes in the development of sandstone bodies, intrusions of volcanic rocks and, most of all, by the different response to stresses mediated by the Lusatian Fault in the NE. The effects of thrusting along the Lusatian Fault include rotation of blocks in its foreland, faulting and brecciation of Cretaceous sandstones, grain cataclasis and silica cementation, and deformation banding. Farther from the Lusatian Fault, stress resulted in the formation of an orthogonal system of vertical joints-a necessary prerequisite for the development of ruiniform relief within the so-called sandstone rock cities. A dozen of sandstone districts can be distinguished, representing patches of rugged 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 European Geoparks of UNESCO in 2005.
Název v anglickém jazyce
Bohemian Paradise: Sandstone Landscape in the Foreland of a Major Fault
Popis výsledku anglicky
The region of Bohemian Paradise in NE Bohemia is the most varied sandstone landscape in the Bohemian Cretaceous Basin. This is caused by the complex stratigraphy of Cretaceous (Upper Turonian to Coniacian) sediments, abrupt lateral changes in the development of sandstone bodies, intrusions of volcanic rocks and, most of all, by the different response to stresses mediated by the Lusatian Fault in the NE. The effects of thrusting along the Lusatian Fault include rotation of blocks in its foreland, faulting and brecciation of Cretaceous sandstones, grain cataclasis and silica cementation, and deformation banding. Farther from the Lusatian Fault, stress resulted in the formation of an orthogonal system of vertical joints-a necessary prerequisite for the development of ruiniform relief within the so-called sandstone rock cities. A dozen of sandstone districts can be distinguished, representing patches of rugged 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 European Geoparks of UNESCO in 2005.
Klasifikace
Druh
C - Kapitola v odborné knize
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název knihy nebo sborníku
Landscapes and Landforms of the Czech Republic
ISBN
978-3-319-27536-9
Počet stran výsledku
14
Strana od-do
195-208
Počet stran knihy
310
Název nakladatele
Springer
Místo vydání
Cham
Kód UT WoS kapitoly
—