2023
DOI: 10.1007/s10346-023-02189-2
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Activity of flow-like landslides on the escarpment cuesta (tree-ring–based study on the eastern margin of the Bohemian Cretaceous Basin)

Karel Šilhán
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“…The northern slopes of the Borgustan Range are gentle, and its southern slopes are rather steep, with a well-developed scarp. By its shape and origin, this is a typical cuesta [49][50][51], which formed thanks to the low-angle, monocline distortion of Lower Cretaceous sedimentary rocks differently prone to erosion. The shape of the Ring Mountain is irregular, with slopes differing in steepness (Figure 6b,d).…”
Section: Ring Mountainmentioning
confidence: 99%
“…The northern slopes of the Borgustan Range are gentle, and its southern slopes are rather steep, with a well-developed scarp. By its shape and origin, this is a typical cuesta [49][50][51], which formed thanks to the low-angle, monocline distortion of Lower Cretaceous sedimentary rocks differently prone to erosion. The shape of the Ring Mountain is irregular, with slopes differing in steepness (Figure 6b,d).…”
Section: Ring Mountainmentioning
confidence: 99%