Articles | Volume 7, issue 2
https://doi.org/10.5194/esurf-7-361-2019
https://doi.org/10.5194/esurf-7-361-2019
Research article
 | 
16 Apr 2019
Research article |  | 16 Apr 2019

Deep-seated gravitational slope deformation scaling on Mars and Earth: same fate for different initial conditions and structural evolutions

Olga Kromuszczyńska, Daniel Mège, Krzysztof Dębniak, Joanna Gurgurewicz, Magdalena Makowska, and Antoine Lucas

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Cited articles

Ambrosi, C. and Crosta, G. B.: Large sackung along major tectonic features in the Central Italian Alps, Eng. Geol., 83, 183–200, 2006. 
Anderson, E. M.: The dynamics of faulting and dyke formation with applications to Britain, Oliver and Boyd, Edinburgh, 1951. 
Andrews-Hanna, J. C.: The formation of Valles Marineris: 1. Tectonic architecture and the relative role of extension and subsidence, J. Geophys. Res., 117, E03006, https://doi.org/10.1029/2011JE003953, 2012. 
Angelier, J. and Colletta, B.: Tension fractures and extensional tectonics, Nature, 301, 49–51, 1983. 
Bachmann, D., Bouissou, S., and Chemenda, A.: Analysis of massif fracturing during deep-seated gravitational slope deformation by physical and numerical modeling, Geomorphology, 103, 130–135, 2009. 
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Deep-seated gravitational spreading features are spectacular on Mars on the hillslopes of Valles Marineris, both in terms of landform freshness and size. This paper compares their dimensions and those in terrestrial analogue sites in the Tatra Mountains. Gravitational spreading is thought to be inactive in both locations. We find that the height-to-width ratio, ~0.24, is similar in spite of much larger strain in Valles Marineris. We explore the implications.
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