Slip surfaces and the inferred basal slip surface in the head scarp

Influence of slip-surface geometry on earth-flow deformation, Montaguto earth flow, southern Italy - ScienceDirect

Propagation of frontally confined subaqueous landslides: Insights from combining geophysical, sedimentological, and geotechnical analysis - ScienceDirect

The submarine fault scarp of the 2011 Tohoku-oki Earthquake in the Japan Trench

Oblique contraction along the fastest ocean-continent transform plate boundary focuses rock uplift west of the Fairweather fault, southeast Alaska

Oblique contraction along the fastest ocean-continent transform plate boundary focuses rock uplift west of the Fairweather fault, southeast Alaska

Full article: Investigation of an unusual landslide at Sai Kung Sai Wan Road, Sai Kung, Hong Kong

The submarine fault scarp of the 2011 Tohoku-oki Earthquake in the Japan Trench

Soft-sediment deformation structures recognised in a reverse-drag associated with normal faulting (Lake Ifrah, Northwest Africa): Palaeoseismic assessment and neotectonic implications - ScienceDirect

Deformation characteristics and multi-slab formation of a deep-seated rock slide in a high alpine environment (Bliggspitze, Austria)

Tectonic geomorphology with relevant morphotectonic markers in (A)

Slip surfaces and the inferred basal slip surface in the head scarp

Down-ice dipping faults with recently formed angular fault scarps

The Mam Tor Creeping Landslide

Water softening-induced retrogressive landslides: Experiments and theoretical calculations of back scarp inclination - ScienceDirect

Two types of possible slip surface

GeoStudio Geotechnical Analysis on X: The Entry-Exit method is currently one of the more popular methods for defining slip surfaces in SLOPE/W. See this example for a full description of the Entry-Exit

Bayesian back analysis of landslides considering slip surface uncertainty

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