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MARINE DRONE TECHNOLOGY FOR PHOENICIAN MOTYA

1Tusa S., 1Fresina A., 1Oliveri F., 2, *Lena G., 3La Motta C.

1Soprintendenza del Mare, Regione Sicilia, Palermo, Italy

2Int.Geo.Mod. srl, via Innamorati 7/a, 06123 Perugia (Italy);

3Thesaurus Service snc, Via dei Miracoli 46, 94014 Nicosia (EN), (Italy)

*g.lena@intgeomod.com, +39 3311305612

The underwater surveys that were carried out at Mozia island, in the basin of the Stagnone Lagoon of Marsala (Western Sicily) encountered various difficulties because of the very shallow water (depth range 50 - 170 cm) and the presence of thick algae fields. These environmental conditions hid the evidences of the flourishing city that was built on the island in the 8th century BC by the Phoenicians and destroyed by the Syracusans in the 4th century BC (Du Plat, 1964). In summer 2015 was performed the first archaeological and geophysical survey by means of USV marine drone Hydrometra (outlined by Siralab Robotics Ltd. and Int.Geo.Mod. Ltd.), with the additional aim of testing the new prototype (fig.1).

The project involved a working group consisting of public and private institutions under the scientific aegis and coordination of Soprintendenza del Mare (Sicilian Underwater Cultural Heritage Department) and with the logistic assistance of the Divers Group of the Guardia di Finanza.

The research project was entirely sponsored by private funds of the companies involved (Int.Geo.Mod. Ltd. and Siralab Robotics Ltd.) with the support and human resources of the institutions above mentioned and the Thesaurus Service snc. of sonic/morphobathymetric surveys in very shallow-water areas (both marine and inland) usually unreachable by conventional vessels.

Fig. 1: Hydrometra USV marine drone during the survey

The USV has an independent navigation system with a dedicated software able to follow predefined routes and correct the ship's course in case of wind and wave action, also thanks to the active differential propellers that make the helm unnecessary.

On board standard equipment includes a Single Beam (SBES), a Side Scan Sonar (SSS) with CHIRP technology and detection system ECHO and DOWNVISION and three cameras (two underwater IR and a surface one).

This research trip highlighted the presence of submerged structures known (Benassi et al., 2008 and references therein) and previously unknown: specifically the survey allowed the discovery of a 2 m channel at the Cothon of Motya (the ancient phoenician-punic basin), probably obtained by digging up the bedrock in front of the mooring area. The channel was presumably used as an easier approach for the boats to the already known phoenician docks.

References

DU PLAT TAYLOR, J. O. A. N., (1964): Motya: A Phoenician Trading Settlement in Sicily. Archaeology 17.2, 91-100.

BENASSI F., CERAULO A. AND PAPA M.A., (2008): Nuove ricerche archeologiche nello “Stagnone” di Mozia. Indagini e prospezioni presso la strada sommersa. FOLD&R FastiOnLine documents &

research 123, 1-6.

MEDFLOOD-MOPP, MODELLING PALEO-PROCESSES. TOWARDS A BETTER UNDERSTANDING OF THE PALEO COASTAL HAZARD AND THE ADAPTIVE STRATEGIES USED IN THE ANTIQUITIES TO SETTLE ON THE COAST

1Vacchi M., 2Biolchi S., 3Harris D., 3Rovere A., 4Scicchitano G. and the Medflood Team

1Aix-Marseille Université, CNRS-CEREGE, Aix en provence, France

2Università di Trieste, Dipartimento di Geoscienze

2University of Bremen, Marum, ZMT, Bremen, Germany

4Studio Geologi Associati T.S.T, Catania Italy

MEDFLOOD-MOPP is a new project launched in 2016 and funded by INQUA for the period 2016-2020.The project stems from the results of MEDFLOOD, which, in 2012, started bridging the communities of earth scientists and archeologists working on sea-level problems in the Mediterranean Sea (Rovere et al., 2012). Results of MEDFLOOD included several publications on geoarchaeology and paleo sea levels in the Mediterranean at different time scales. During the MEDFLOOD 4-year period, 4 workshops were organized including field activities aimed at fueling discussions and interdisciplinary exchanges between archeologists, physical geographers and geologists on sea level topics.

The MEDFLOOD project resulted in a significant improvement in the collaboration between Mediterranean geomorphologists and archaeologists. MEDFLOOD-MOPP, is the natural development of MEDFLOOD. As such, we want to enlarge the MEDFLOOD community and encourage the participation of experts in coastal geomorphology and geo-archaeology as well as engineers and hydrodynamic modellers. Our aims are to i) better define the strategies adopted since the antiquity to design coastal structures, taking into account not only the geomorphology of the coastal area but also the paleo-coastal hydrodynamics obtained through numerical modelling of paleo-nearshore processes; ii) better constrain the impacts of past catastrophic coastal events (such as major storms or tsunamis).

Only in the past twenty years, the archaeological community started to consider the importance of the environment in understanding the socio- economic and wider natural frameworks in which ancient societies lived, and multidisciplinary research has become a major focus of most large-scale Mediterranean archaeological excavations. Knowledge of the strategies used to build coastal structures in the past is presently based on the texts of ancient authors, often geographers or architects, such as Strabo, Pausanias, Pliny the Elder, Ptolemy. Even if these sources often provided very detailed descriptions, the conceptual framework for the architectural design of coastal structures with respect to palaeo- coastal processes, remains largely unexplored. The recent advances in palaeo-environmental reconstructions, the development of cost-effective techniques for high-resolution aerial photogrammetry (e.g. Unmanned Aerial Vehicles, UAV) and the recent development of freely available and versatile tools for coastal modelling (e.g. Delft3D, XBeach, FUNWAVE) offer us the possibility to assess - for the first time and in a quantitative manner - the strategies of coastal planning since the antiquity. Another emerging field of research at the boundary between geology and coastal engineering is the study of the effects of waves in paleo environments. As an example, a recently highly debated paper (Hansen et al., 2016) revisited the hypothesis, based on field data, that ‘superstorms’

characterized the Atlantic at the end of the Last Interglacial. To study in a more rigorous way the deposits and landforms that are at the base of this hypothesis, and to make inferences on the waves that might have characterized this period, a closer collaboration is necessary between coastal geomorphologists, sea level geologists and coastal hydrodynamic modellers. This will allow for the most accurate reconstruction of past extreme events in the Mediterranean thus far, and have direct links in reinterpreting the effects of large storms on coastal communities in the past and also allow for prediction of storminess and coastal hazard in the future.

MORPHOLOGY OF THE KARST SUBMARINE SPRING OF THE MAR GRANDE