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The 54m (177ft) deep landslide destroyed 30 houses near the town of Oso, about 90km north of Seattle.
It may represent possible future sliding plane of a shallow (approximately 6 m deep) landslide (Fig. 6).
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Incoherent materials favour shallow landslides with no limitation in size; cohesive materials favour deep landslides and show a limitation for small sizes.
In this paper, referring to the case study of a medium-deep landslide that occurred in Calabria (Southern Italy) during the winter of 2009 2010, a method and means of defining an emergency geotechnical model (smart geotechnical model) using a geological model are proposed.
Conversely, in the western Southern Alps, tectonic forces produce pervasive fracturing with depth that results in larger, and deeper landslides.
The most abundant types of landslides triggered in earthquakes are fairly shallow, disrupted falls and slides in rock and soil; larger, deeper landslides are less common but contribute significantly to total landslide volumes.
Designing and constructing of road embankments, deep excavations, landslide and snow avalanche predictions or profiling construction sites in slanting terrain need slope stability evaluations.
Studying long term-evolution of gravitational slope evolution is a key to understanding deep-seated landslide processes.
In addition, these residuals may result from deep-seated landslide and active folding or mud diapir in a mudstone area.
Downslope, Mt. Lama back limb is affected by a large deep-sited landslide whose scarp bound the flatirons and mimics a Holocene fault scarp.
The depositional record of two generations of former near-scarp depressions revealed a multiple deep-seated landslide activity during the last Quaternary climatic cycle.
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