Hydrogeomorphological and stability modeling of pyroclastic soils covering peri-vesuvian hillslopes (Campania - Southern Italy)
In the area surrounding the Campanian volcanic districts the greater natural risk, after the volcanic one, is represented by the debris flows that occur along the steep slopes of carbonate and volcanic mountains. These phenomena involve loose ash-fall pyroclastic mantle and impact with human lives a...
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Veröffentlicht in: | Geophysical research abstracts 2007-01 |
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Format: | Artikel |
Sprache: | eng |
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