Activity of flow-like landslides on the escarpment cuesta (tree-ring–based study on the eastern margin of the Bohemian Cretaceous Basin)
Author:
Funder
Grantová Agentura České Republiky
Publisher
Springer Science and Business Media LLC
Subject
Geotechnical Engineering and Engineering Geology
Link
https://link.springer.com/content/pdf/10.1007/s10346-023-02189-2.pdf
Reference61 articles.
1. Ahnert F (1960) The influence of Pleistocene climates upon the morphology of cuesta scarps on the Colorado plateau. Ann Assoc Am Geogr 50:139–156. https://doi.org/10.1111/j.1467-8306.1960.tb00341.x
2. Alestalo J (1971) Dendrochronological interpretation of geomorphic processes. Fennia 105:1–139
3. Blott SJ, Pye K (2001) GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments. Earth Surf Process Landf 26:1237–1248. https://doi.org/10.1002/esp.261
4. Borgatti L, Tosatti G (2010) Slope instability processes affecting the Pietra Di Bismantova Geosite (Northern Apennines, Italy). Geoheritage 2:155–168. https://doi.org/10.1007/s12371-010-0023-8
5. Borgatti L, Guerra C, Nesci O et al (2015) The 27 February 2014 San Leo landslide (northern Italy). Landslides 12:387–394. https://doi.org/10.1007/s10346-015-0559-4
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