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Gas hydrate has been concerned as a potential shallow hazard during deepwater drilling.
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Model results allow to quantify the influence of roads on shallow landsliding hazard across a landscape and to generate hypotheses about the broader geomorphic effect of roads.
The model is specifically designed for the analysis of shallow landslide hazard by combining a steady state hydrologic model with a deterministic infinite slope stability model.
The model is then applied to shallow landslide hazard assessment with the aid of GIS technology.
In the existing research, if the ground water rises up to the slope surface, and the slope safety factor F s ≥ 1, thus the slope is unconditionally stable for shallow landslide hazard assessment (Rosso et al. 2006; Chang and Chiang 2009).
This integrated approach provides a strategy for evaluating shallow seismic hazard-related targets for engineering concerns.
Within areas potentially subject to shallow landsliding, relative hazard was further stratified using a simple slope stability model.
The paper investigates the key parameters in designing such a SBW, aiming to mitigate the fault rupture hazard on shallow foundations.
This summer, nearly four years after those deaths in a Staten Island pool raised alarms about a little known hazard called shallow-water blackout or hypoxic blackout, New York City is putting up warning signs at all public pools prohibiting prolonged breath holding.
We use an existing classification of 21 natural hazards, organised into six hazard groups (geophysical, hydrological, shallow Earth processes, atmospheric, biophysical and space hazards).
The maximum expected ground motion in Greece is estimated for shallow earthquakes using a deterministic seismic hazard analysis (DSHA).
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