Slip surfaces and the inferred basal slip surface in the head

Download scientific diagram | Slip surfaces and the inferred basal slip surface in the head scarp region of the Acquara-Vadoncello earth flow. Boreholes I3, I4, and P3, the well-constrained slip surfaces 6, 8, and 9, the less-well-constrained slip surface 7, and the inferred basal slip surface are shown. No vertical exaggeration. Adapted from Wasowski and Mazzeo (1998). from publication: MECHANICS OF EARTH FLOWS | Earth flows are mass movements of fine-grained soils that range from slow flows with velocities on the order of meters or less per year to rapid flows that have velocities as high as several meters per second. Slow earth flows form in deposits of fine-grained plastic clay or | Earth, Non-Newtonian Fluids and Mass | ResearchGate, the professional network for scientists.

Shear margins in upper half of Northeast Greenland Ice Stream were established two millennia ago

Frontiers Thermal Structure Beneath the Tarim Craton and Its Tectonic Implications

Active Tectonics at UC Berkeley

Metals, Free Full-Text

Insights into some large-scale landslides in southeastern margin of Qinghai-Tibet Plateau - ScienceDirect

Active Tectonics at UC Berkeley

Millennial-scale coseismic landslide history inferred from topographic and stratigraphic features of a post-caldera cone of Aso Volcano in southwestern Japan - ScienceDirect

Effects of basal topography and ice-sheet surface slope in a subglacial glaciofluvial deposition model, Journal of Glaciology

Basal conditions at Engabreen, Norway, inferred from surface measurements and inverse modelling, Journal of Glaciology

How to A virtual classroom - Geological Digressions

Along-fault distribution of horizontal slip and moment release, from

Frontiers Effects of Erosion and Deposition on Constraining Vertical Slip Rates of Thrust Faults: A Case Study of the Minle–Damaying Fault in the North Qilian Shan, NE Tibetan Plateau

Slip (materials science) - Wikipedia

Effects of basal topography and ice-sheet surface slope in a subglacial glaciofluvial deposition model, Journal of Glaciology

TC - In situ 10Be modeling and terrain analysis constrain subglacial quarrying and abrasion rates at Sermeq Kujalleq (Jakobshavn Isbræ), Greenland