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- W2497432566 abstract "The area between the Jizera and Elbe rivers in north-central Bohemia features a southerly dipping package of sedimentary rocks of CretaceousCretaceous age, subjected to modest upliftUplift throughout the Quaternary. The Kokořín sandstone (Middle to Upper Turonian) comprises five superimposed bodies with generally high permeability and low-to-medium resistance to weathering. Most valleys are dry, shaped by occasional flash floodsFlash floods and gravitational processes. Disintegration of vertical cliffCliff faces is dominated by salt weatheringSalt weathering . Specific landforms develop on sandstones cemented by iron oxyhydroxides of hydrothermal origin. These form thin (centimetres to metres), sheet-like bodies, either subvertical or bedding-parallel, and give rise to structural plateausStructural plateaus and mesas, steep erosional ridges and mushroom rocksMushroom rocks . The variety of small-scale relief forms on ferruginous sandstoneFerruginous sandstone is unique at a global scale. The highest elevations in the landscape are formed by exhumed subvolcanic bodiesSubvolcanic bodies . The Kokořín AreaKokořín Area is a perfect example of a sandstone-dominated erosional landscape whose high relief complexity is largely due to the contrasting resistance of rocks to weatheringWeathering ." @default.
- W2497432566 created "2016-08-23" @default.
- W2497432566 creator A5070573923 @default.
- W2497432566 date "2016-01-01" @default.
- W2497432566 modified "2023-10-18" @default.
- W2497432566 title "The Kokořín Area: Sandstone Landforms Controlled by Hydrothermal Ferruginization" @default.
- W2497432566 cites W1982161908 @default.
- W2497432566 cites W2000486060 @default.
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- W2497432566 doi "https://doi.org/10.1007/978-3-319-27537-6_13" @default.
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