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Susceptibility assessment of small, shallow and clustered landslide

Earth Science Informatics, 2021
Susceptibility assessment of landslides over a large area depends on the basic spatial unit of mapping, usually by using grid cell or slope unit. Both units are used in this study for the assessment of small shallow and clustered landslides in vegetated slopes in Malipo, southwest China.
Xuemei Liu   +4 more
openaire   +1 more source

Snowmelt influence in shallow landslides

2020
<p>Mass wasting is a major landform shaping process in mountainous and steep terrains, and Italy is among the most affected countries in Europe. Lombardia region has 130.450 landslides mapped, covering an area of 3.300 km<sup>2</sup> (i.e. 7.2% of the regional area).
Renzo Rosso   +4 more
openaire   +1 more source

The impact of shallow landslides on primary productivity

2021
CEC Research, Volume 5, Issue ...
Addison Eftekhari   +3 more
openaire   +1 more source

Modeling of Rainfall-Induced Shallow Landslides of the Flow-Type

Journal of Geotechnical and Geoenvironmental Engineering - ASCE, 2010
The paper deals with the modeling of failure and postfailure stage of shallow landslides of the flow-type that often affect natural shallow deposits of colluvial, weathered, and pyroclastic origin. The failure stage is frequently associated to rainfall that directly infiltrates the slope surface and to spring from the underlying bedrock.
Sabatino Cuomo   +2 more
exaly   +3 more sources

Multiple Load Case on Flexible Shallow Landslide Barriers: Shallow Landslide and Rockfall

2015
Commonly a number of different gravity driven hazards (shallow landslide, rock slide, rockfall, small snow slides) will act at same location, threatening the safety of people, buildings and infrastructure. In this case protection barriers have to be designed to cope with the different load cases of multiple natural hazards (Fig. 77.1).
Wendeler, Corinna, Glover, James
openaire   +1 more source

Impact Pressure Measurements in Shallow Landslides

2013
We reproduce shallow landslides by releasing 50 m3 of debris mixture down a 40 m long and 30° steep slope. The slope is instrumented in order to measure front and surface velocities, flow height and impact pressure on small obstacles. The mixture properties are determined from analysis of material samples.
Bugnion, Louis, Wendeler, Corina
openaire   +2 more sources

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