Search results for " geomorfologia"

showing 4 items of 284 documents

Landslide susceptibility assessment in the upper Imera river basin (central Sicilian chain)

2009

validationLandslidesusceptibility assessmentItalySettore GEO/04 - Geografia Fisica E GeomorfologiaSicilySettore GEO/05 - Geologia Applicata
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Susceptibility assessment for flows landslide in the upper Salso river basin (Sicily)

2009

validationSicily ItalyLanslidesusceptibility assessmentSettore GEO/04 - Geografia Fisica E GeomorfologiaSettore GEO/05 - Geologia Applicata
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Holocene sea level change in Malta

2013

A multidisciplinary approach has been applied to study sea level changes along the coast of Malta using data collected from underwater archaeological remains. The elevation of archaeological markers have been compared with predicted sea level curves providing new bodies of evidence that outline the vertical tectonic behaviour of this region, allowing estimation of the relative sea level changes that occurred in this area of the Mediterranean since the Bronze Age. During the Roman Age, sea level was at −1.36 ± 0.1 m, while in the Midde Age it was at −0.56 ± 0.2 m, in agreement with previous estimations for the Mediterranean region. Data indicate that Malta was tectonically stable during the …

vertical movementMediterranean climateClimatic changes -- MaltaSea level -- MaltaSettore GEO/02 - Geologia Stratigrafica E SedimentologicaPleistoceneMaltaSettore GEO/03 - Geologia StrutturaleSettore GEO/04 - Geografia Fisica E GeomorfologiaElevationLast Glacial Maximumrelative sea level changePaleoecology -- Maltarelative sea level change; Late Holocene; MaltaLate HoloceneTectonicsPaleontologyPalynology -- MaltaBronze Agesealevel changeHoloceneGeologySea levelEarth-Surface Processes
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Monitoring of erosion on two calanchi fronts – Northern Sicily (Italy)

2011

In the present research, two neighbouring calanchi fronts have been monitored by means of repeated readings on erosion pins, that were carried out between November 2006 and October 2008. During the monitoring period, a gauge station has been recording rainfalls, allowing us to compute the Rainfall-Runoff Erosivity Factor of the USLE model. The research highlighted: i) a general correspondence between rainfalls temporal trends and surface variation rhythms; ii) alternating erosion and deposition phases result in a retreat of the “calanchi” fronts.

water erosion calanchi monitoring SicilySettore GEO/04 - Geografia Fisica E Geomorfologia
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