“…Land subsidence afflicts many areas of the world, in particular the ones located along transitional environments, such as coastal areas, deltas, wetlands, and lagoons, which are becoming increasingly vulnerable to flooding, storm surges, salinization, and permanent inundation [6][7][8][9]. In these areas, subsidence can be usually considered as a consequence of a complex combination of natural and anthropogenic factors: the compaction of Holocene sediments, tectonic movements, sinkholes formation, volcanism, thawing permafrost, and the Glacial Isostatic Adjustment (GIA), are generally considered as the main natural sources of land subsidence [10][11][12]; aquifer-system compaction associated with groundwater/oil/natural gas depletion and storage, drainage of organic soils, underground mining, hydro-compaction and stress given by new constructions, are the principal drivers of the anthropogenic land subsidence [13][14][15][16][17][18][19]. Moreover, the effects of climate change can dramatically increase the subsidence-related problems due to the rising of sea levels: the 2012 Intergovernmental Panel on Climate Change (IPCC, www.ipcc.ch, (accessed on 9 April 2021)) report, in fact, highlight an increasing occurrence of coastal and fluvial flooding, extreme weather events and sea-level rise as a consequence of climate change during the XXI century.…”