2019
DOI: 10.3280/pri2018-003002
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La comunicazione del rischio e la percezione pubblica dei disastri: il caso studio della frana di Maierato (Calabria, Italia)

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Cited by 2 publications
(5 citation statements)
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“…If we analyze the perception of exposure to extreme natural events, the perception of exposure to earthquakes by respondents from Lago and Amantea is high on both. These data, in the context of this geographical study area, confirm the high perception of risk exposure, also found in other studies carried out in different areas of Calabria-Pollino [63], Aiello Calabro [78], Costa degli Dei [60,79], Maierato [61,80]. As we have pointed out, the two municipalities are located in an area with high seismic hazard.…”
Section: Community Resilience To Extreme Natural Events and Climate Csupporting
confidence: 91%
“…If we analyze the perception of exposure to extreme natural events, the perception of exposure to earthquakes by respondents from Lago and Amantea is high on both. These data, in the context of this geographical study area, confirm the high perception of risk exposure, also found in other studies carried out in different areas of Calabria-Pollino [63], Aiello Calabro [78], Costa degli Dei [60,79], Maierato [61,80]. As we have pointed out, the two municipalities are located in an area with high seismic hazard.…”
Section: Community Resilience To Extreme Natural Events and Climate Csupporting
confidence: 91%
“…The mean annual rainfall is approximately 995 mm (Figure 3): generally, the rain is distributed on 90 rainy days per year, essentially between October and March, when approximately 77% of the annual precipitation falls. Generally, the rainiest months are November and December, during which several landslides occur [19,34], while June, July, and August are the driest months of the year. The maximum daily rainfall of 290 mm was registered on 16 November 1987 (Figure 3c).…”
Section: The Catanzaro Study Area Frameworkmentioning
confidence: 99%
“…This basin is filled by Neogene-Quaternary sedimentary units (Figure 4) consisting of marine and continental deposits, unconformably lying on the Hercynian crystallinemetamorphic units of the Calabrian Arc [37,40,41]. As a geo-structural setting, the SA is situated on the north-eastern edge of the Catanzaro basin (Figure 4) and is the linkage zone between the northern and southern sectors of the mountain belt named the Calabrian Arc [34,[36][37][38][39]. The Catanzaro basin, including the SA, is a graben-like structure placed between Sila and Serre Massifs, bordered to the north by NW-SE-trending faults and to the south by a WNW-ESE-oriented fault system [35,38].…”
Section: The Catanzaro Study Area Frameworkmentioning
confidence: 99%
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