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Valeria Rago

Researcher at National Research Council

Publications -  14
Citations -  165

Valeria Rago is an academic researcher from National Research Council. The author has contributed to research in topics: Landslide & Slope stability. The author has an hindex of 6, co-authored 12 publications receiving 117 citations. Previous affiliations of Valeria Rago include University of Calabria.

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"Landslide inventory map of north-eastern Calabria (South Italy)"

TL;DR: In this paper, the authors reported the reconnaissance and the characterization of landslides of north-eastern Calabria (south Italy) by combining field surveys with the analysis of topographic maps and multi-temporal air photos, taken in the period ranging from 1954 to 2006.
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Integrated Physically based system for modeling landslide susceptibility

TL;DR: In this paper, an integrated system for early warning of rainfall induced shallow landslides is presented based on a hydrological model for solving 3D-Richards equation, a component for safety factor maps computation under infinite slope hypothesis and a GIS for model outputs visualization.
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Landslide inventory and main geomorphological features affecting slope stability in the Picentino river basin (Campania, southern Italy)

TL;DR: The landslide inventory of the Picentino basin was realized at 1:25,000, with focus on main geomorphological features affecting slope stability as discussed by the authors, based on different sets of air-photos.
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Soil loss assessment in the Turbolo catchment (Calabria, Italy)

TL;DR: In this article, the authors analyzed and mapped soil loss caused by water-induced soil erosion at the catchment scale using the revised universal soil loss equation (RUSLE) model implemented in a geographical information system.
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Geomorphic effects caused by heavy rainfall in southern Calabria (Italy) on 30 October–1 November 2015

TL;DR: A severe rainfall event occurred in southern Calabria between 29 October and 2 November 2015, causing two deaths and serious damage to transport infrastructure as discussed by the authors, where widespread slope erosion and thousands of shallow landslides were triggered on the slopes, combined with flooding and transport of debris along the streams.