The Dynamics of Sedimentary Processes in Coastal Areas

A special issue of Geosciences (ISSN 2076-3263). This special issue belongs to the section "Sedimentology, Stratigraphy and Palaeontology".

Deadline for manuscript submissions: closed (1 June 2023) | Viewed by 1945

Special Issue Editor

Special Issue Information

Dear Colleagues,

Coastal areas are highly sensitive geological zones whose modification is a function of several geological processes. In this Special Issue, we acknowledge papers discussing the dynamics of sedimentary processes in coastal areas and adjacent offshore, focusing on both low sandy coasts and high coastal cliffs using different techniques and methods, including geological survey, sedimentology and seismic stratigraphy. Continental platform studies are also suitable. GIS and LIDAR studies are also mentioned to study the continuous modification of the shorelines. The regional controls on the sedimentary processes in the coastal areas are long-term geological processes (subsidence, isostasy), with a strong influence on controlling the short-term dynamics. As sea levels rise or fall, the geomorphology of coastal areas will further evolve, varying the boundary conditions of other coastal processes: circulation, waves, tides and the storage of sediment on flood plains. Other important control factors are climate, controlling coastal destabilization and beach erosion, the global flux of sediments (source-to-sink), and human development, particularly during the Holocene and the Anthropocene. 

Dr. Gemma Aiello
Guest Editor

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Published Papers (1 paper)

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30 pages, 13412 KiB  
Article
The Coastal Areas of the Bay of Naples: The Sedimentary Dynamics and Geological Evolution of the Naples Canyons
by Gemma Aiello and Mauro Caccavale
Geosciences 2023, 13(8), 226; https://doi.org/10.3390/geosciences13080226 - 27 Jul 2023
Cited by 3 | Viewed by 1493
Abstract
The sedimentary dynamics and geological evolution of the Naples canyons during the Late Quaternary have been studied based on sedimentological and seismo-stratigraphic data. Several factors, including the sedimentary environments, tectonic setting, and volcanic eruptions, have controlled the geological evolution of the coastal and [...] Read more.
The sedimentary dynamics and geological evolution of the Naples canyons during the Late Quaternary have been studied based on sedimentological and seismo-stratigraphic data. Several factors, including the sedimentary environments, tectonic setting, and volcanic eruptions, have controlled the geological evolution of the coastal and marine areas of the Bay of Naples. The main data and methods include the sedimentological data analysis, the seismo-stratigraphic techniques applied in the geological interpretation of seismic profiles, and the integrated analysis of core data that were previously published. The formation of the Dohrn canyon is controlled by fluvial processes, active in correspondence with the palaeo-Schiazzano River system and by the main eruptive events involving the submarine portion of Naples Bay, including the Campanian Ignimbrite (CI; 39 ky B.P.) and the Neapolitan Yellow Tuff (NYT; 15 ky B.P.). The formation of the Magnaghi canyon is controlled by erosional processes on the continental slope of Procida Island, which was active during the last eruptive phases of the island (Solchiaro Formation; 18 ky B.P.), triggering high rates of volcaniclastic supply. Full article
(This article belongs to the Special Issue The Dynamics of Sedimentary Processes in Coastal Areas)
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