We present here the results of the morpho-bathymetric analyses of the main submarine canyons along the upper slopeoff the north-western Sicily. This region developed during the Neogene as the transition area between the Sicilian foldand thrust belt and the Tyrrhenian basin realm. Along the upper slope, a dense network of submarine canyon developsfrom 80 m water depth up to more than 2000 m, showing a large variability of sizes and morphology. In this areasubmarine canyons play a crucial role related to the along-slope sedimentary transport and are among the most distinctivefeatures of the submarine seascape.This study is based on a quantitative analysis of a high resolution multibeam data set of the north-western Sicilyoffshore integrated with the topographic DEM of the adjacent continental region. Very different canyon-relatedmorphological features along the study area mainly suggest the occurrence of top-down gravitational processes alongcanyons likely originated through a bottom-up evolution. By means of high resolution bathymetric data, we: i) describedthe main morphological features of submarine canyons; ii) measured the main morphometric parameters along canyonlongitudinal profiles; iii) calculated the extension of different lithology outcropping on the river catchment areascorresponding to distinct river-fed canyons. For each analyzed canyon a chart was built in which bathymetric longitudinalprofile, catchment area extension and gradient longitudinal profile have been reported.Quantitative analyses of longitudinal profiles reveal that the morpho-sedimentary evolution of mapped canyons iscomparable to the corresponding fluvial environment, although presenting some differences.Integrated analysis of offshore data and river catchment areas suggest that the continental slope structural setting aswell as the outcropping lithologies could be relevant control factors on the morpho-sedimentary evolution of the NWSicilian canyons.
|Numero di pagine||1|
|Rivista||RENDICONTI ONLINE DELLA SOCIETÀ GEOLOGICA ITALIANA|
|Stato di pubblicazione||Published - 2016|