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- W66855784 abstract "Important controlling factors of mass movements are soil water and geometric-topographic terrain factors such as inclination, curvature type and degree or the rel-ative position of instable slopes and embankments. In addition various geologic pa-rameters, that have a direct or indirect connection to the soil-mechanical propertiesof the slide masses, are of importance. Among others, these are the age (degree ofconsolidation), the granulometric composition (e.g. clay content, cohesiveness) andthe permeability of the loose rock. However, the importance of these parameters isstrongly dependent upon the specific geo-factors of the investigated regions.Few studies also emphasise tectonic parameters, such as the bedding dip, in the contextto the susceptibility of mass movements. Hereby, the ‘apparent dip’ plays an essentialrole for the slope stability, i.e. the dip angle of the bedding in the slope direction.However, these contributions focus largely on the susceptibility to sliding within thelayers. In contrast, the aim of the present study is to identify the importance of thestratigraphic sequence for mass movements in the surface formations on top of thebedrock.The research area is part of the southern Solling anticline, a saddle structure in theMiddle Bunter Sandstone formation in Northern Hesse and Southern Lower Saxony(Germany). The Fulda, Werra and Weser rivers have cut 200 - 300 m deep into theanticline formation. The sandstone, clay, and siltstone layers are interbedded with thin" @default.
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- W66855784 date "2008-01-01" @default.
- W66855784 modified "2023-09-27" @default.
- W66855784 title "The impact of tectonic and structural parameters in Triassic bedrocks on the landslide susceptibility in Quaternary surface formations" @default.
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