Abstract
During the monitoring campaign, small slope movements have been recorded by surface and subsurface measurements which are extremely-slow according to the definition by Cruden and Varnes (1996). In particular with regard to inclinometer Lic02, these displacements can be interpreted as a continuation of the displacement previously described by Bell (2007). In contrast to this earlier study, the research described in this thesis could employ geodetic measurements carried out by Aslan et al. (2010a) for interpretation of large scale movement trends.
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Thiebes, B. (2012). Discussion. In: Landslide Analysis and Early Warning Systems. Springer Theses. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27526-5_8
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