2021
DOI: 10.1038/s41598-021-92939-w
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New evidence of a Roman road in the Venice Lagoon (Italy) based on high resolution seafloor reconstruction

Abstract: This study provides new evidence of the presence of an ancient Roman road in correspondence to a paleobeach ridge now submerged in the Venice Lagoon (Italy). New high resolution underwater seafloor data shed new light on the significance of the Roman remains in the lagoon. The interpretation of the data through archive and geo-archaeological research allowed a three-dimensional architectural reconstruction of the Roman road. The presence of the ancient Roman road confirms the hypothesis of a stable system of R… Show more

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Cited by 9 publications
(4 citation statements)
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“…Lyzenga followed the fundamental principle derived from the Beer-Lambert law. Lyzenga developed a linear method which assumes that the reflection at the bottom is a linear function of the reflectance of the seabed with the exponential function of the depth of water [5,6,30,43]. The estimation of the depth from a single band depends on the albedo and can be made using the following equation:…”
Section: Resultsmentioning
confidence: 99%
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“…Lyzenga followed the fundamental principle derived from the Beer-Lambert law. Lyzenga developed a linear method which assumes that the reflection at the bottom is a linear function of the reflectance of the seabed with the exponential function of the depth of water [5,6,30,43]. The estimation of the depth from a single band depends on the albedo and can be made using the following equation:…”
Section: Resultsmentioning
confidence: 99%
“…This section presents the overall results generated from the different methods and datasets described above. The Equations ( 4)- (6) were implemented to all different multispectral datasets. Due to the specificity of the study area, the combinations of all visible bands with all algorithms mentioned above were analyzed using the three optical images.…”
Section: Resultsmentioning
confidence: 99%
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“…Overall, this missing bathymetry information limits our ability to understand and predict coastal evolution which on its own inherently leads to large uncertainties in predicting hazards such as coastal sea states, storm surges, and wave-induced surges and flooding [4][5][6]. The availability of fast, inexpensive, and efficient methods is also needed for studies of bottom variability, such as sandy shoreface or underwater dune dynamics but also some environmental applications such as benthic habitat mapping [7], seabed geomorphology [8], underwater archaeology [9], and exploration of unexploded ordnance [10]. There is currently a growing demand for coastal monitoring, where coastal bathymetry is of critical importance [11,12].…”
Section: Introductionmentioning
confidence: 99%