Il territorio di Ospedaletto Euganeo tra tarda antichita e medioevo20200609 75403 31almi (original) (raw)
Related papers
The territory of the suburbs of Rome between Via Prenestina and Via Appia and up to the slopes of the quiescent volcano of the Alban Hills has been the focus of extensive archaeological investigations carried out by the Soprintendenza Speciale per i Beni Archeologici di Roma, in particular in 1999Roma, in particular in -2007. This research found evidence of the presence of Final Neolithic and Eneolithic settlements as well as Eneolithic necropolises. At the same time the Dipartimento di Scienze Geologiche of the Università di Roma Tre carried out a territorial survey that, thanks to the stratigraphic sections discovered by the archaeological investigations, led to a revision of the knowledge about the primary volcanic deposits and lahars arising from the crater of the Albano Lake, referable to the Holocene.
This paper presents the research method applied to the Archaeological Map of Italy -Forma Italiae project, comprising to date the Ager Venusinus project (completed) and the Ager Lucerinus project (ongoing). The methodology of the project is based on the extensive and systematic survey of the entire selected district. The countryside is systematically searched by groups of students and researchers in different seasons, time of the day, weather and visibility conditions, and status of cultivation of the ground. The GPS georeferenced data are integrated in a GIS specifically realised. The results of the research projects relating to the territory of the Luceria's colony, in Apulia, starting from the area of the medieval site of Montecorvino, in the Daunian district is presented. So far the part of the vast territory of Lucera studied concerns the area North-East of the ancient Latin colony. Discussed here are studies conducted on the western area, towards the Daunian subappennine and in particular focused on the territory of the municipalities of Lucera, Pietramontecorvino, Motta Montecorvino, and Volturino. This area, in fact, is the object of research that includes the whole of the Fortore River valley. The data emerging from recent surveys show a large population over the time-span from prehistory to the High Middle Ages. The settlements of the Neolithic and Bronze ages, so far identified, are placed on vast plains; on the northern sector of the territory, it is possible to catch a glimpse of traces of a village characterised by the typical C shaped ditch, with huts located inside. A very interesting part of our project regards Dauni and Samnite settlements in the period preceding the arrival of the Romans and the Romanisation of the area. The most notable transformations in the ancient landscape were undoubtedly produced by the Roman intervention that gave birth to the new colony and the planning of the village centre, which consequently led to the reorganisation of a vast territory and the division of the rural area into a dense network of small properties assigned to the settlers.
Communities and landscape(s) of North-eastern Apulia during the 2nd millennium BC
in Gravina A. (a cura di), Atti del 43° convegno nazionale sulla Preistoria, Protostoria e Storia della Daunia, 2023
systems, attempts their integration into an overarching discussion, embracing data uncertainty within a contextual analytical perspective. The focus of exploration is on the timespan of the 18 th to the 12 th centuries BC: the goal being to analyse the lived-in landscape(s) and assess the impact of the emergence and growth of fortified centres in the cultural landscape formation. Geographical and paleoenvironmental setting The area under scrutiny (fig.1) encompasses the Northeastern part of the Apulia region (WGS84-UTM33N; unit-in metres; range from limits at NW Long. 542055,38, Lat. 4648995,50 to the SE Long. 600277,19, Lat. 4587426,00). It is characterised by the presence of four environmental components: the Adriatic Sea, the coastal wet areas, the flat northern part of the Tavoliere plain (the second largest plain of the Italian peninsula) and the mountainous backdrop of the Gargano promontory, that merge into each other. They contribute to make this geographical area one of the most naturally diversified regions of the Central Mediterranean. Furthermore, since the Neolithic period, the particular shape of the Gargano promontory, projecting into the Adriatic Sea, as well as the presence of small islands (e.g. Tremiti and Pelagosa), has served as a bridge for contacts between Southeastern Italian and Western Balkan societies (Forenbaher et alii 2018; Gori et alii 2018; Arena 2020). Recent research has shed new light on the paleoenvironmental conditions throughout the Mid-Late Holocene, including changes in coastlines and wetlands (susini et alii 2022; calDara, siMone 2012; Boenzi et alii 2006; lucchi et alii 2006), as well as changes in climate and vegetation cover (caroli, calDara 2007; Di rita, Magri 2012; fiorentino et alii 2013; susini et alii 2022). Notably, fresh paleoenvironmental data are available from a recent paper (susini et alii 2022) focused on changes seen in coastal lagoons located along the southwestern shore of the Manfredonia gulf, historically known by the names of Lago Salso and Lago Salpi. Here, this paper takes into consideration the extension of the northern part of the lagoon (Lago Salso) and the surrounding marsh areas as reconstructed by Susini et al. for the Early-Middle Meghalayan (i.e. 4.2ka-2.4Ka B.P.), which partially modifies the previous hypothesis by Caldara and Simone (calDara, siMone 2012) and better combines with the available archaeological evidence. Northern bodies of water though, Lago di Lesina and Lago di Varano, have been mapped using present shorelines, since they are expected to be broadly comparable to those in Late Prehistory (Pennetta 2007). But throughout the second millennium BC, another body of waterthe now-extinct Battaglia Lake-influenced the eastern side of the Gargano promontory (fig.14 Pennetta 2007). It has also been incorporated into the map (fig.1) at its hypothesised extent and position at around 5180±40 BP (fig. 14b Pennetta 2007). During the 2 nd mill. BC, lowlands were mainly characterised by an open land
2013
The Piana Campana (Southern Italy) has recently revealed its potential for the recovery of detailed archaeological and environmental data, during the Late Holocene, due to the thickening of the deposits caused by the activity of the volcanic complexes of Somma-Vesuvius and Campi Flegrei. Settlements, burials, landscape and agrarian infrastructures (tracks, fields, wells, etc.) indicate an intense and continuous human presence since at least late Neolithic times (ca. 6.2 ka cal BP). This study derives from archaeological research supported by the Soprintendenza per i Beni Archeologici della Campania and the Soprintendenza al Museo Nazionale Preistorico Etnografico “L. Pigorini”, Roma (1995e2005). The comprehensive pattern of the protohistoric (Early Bronze Age) agrarian traces found at Gricignano d’Aversa/U.S. Navy support site (Caserta) is presented. An uninterrupted ploughed surface and field system of 60 ha is described, preserved directly below the Pomici di Avellino eruption (ca. 3900 cal BP). For the first time in Italy, such a wide protohistoric field system was reconstructed. The agrarian features (banks, gullies, one cart track) show a remarkable regularity, hinting at patterned landscape exploitation. The discussion is widened by setting these results in the context of the Piana Campana. Regional archaeological and pollen data confirm the marked agrarian impact over the landscape during this period. Arboreal pollen has generally low values under the Pomici di Avellino eruption, but it increases in the plain after this event, possibly due to the main settlement relocation in more defendable spots. The identified anthropic impact is due to the long-lasting shifting agricultural strategy adopted by human communities from the late Neolithic to the Early Bronze Age.
The study area is located in the mid Calore valley, between the Calore and the Ufita Rivers. From prehistoric times, the territory has constituted an important crossroad among Campania, Apulia and Lucania, ensuring a connection between the Tyrrenian and Adriatic coast. The importance of the area grew with the construction of the via Appia, in the third century BC. Along its route, as documented by itinerary sources, in the early first century BC the municipium of Aeclanum (Passo di Mirabella -Mirabella Eclano, AV) was founded. A significant part of the research project regards this city: archaeological field surveys were carried out in the urban area and along the city walls, still partially preserved, with the aim to clarify its route. The new collected data were georeferenced in an aerophotogrammetric map, together with the data deriving from 1960s archaeological excavations and systematic study of archival documents of the Superintendence of Salerno, Avellino, Benevento and Caserta Province. The map was realised in the LabTAF of the University of Salento and constitutes the first large scale archaeological map of the ancient city. Systematic archaeological field walking was carried out on the territory corresponding partially to the ager Aeclanensis. It aimed at the reconstruction of the ancient topography of the territory surrounding the Roman site thanks to the large number of settlements documented. These settlements attest to the inhabitation of the area since the prehistoric and proto-historic times to the Medieval period. All collected data are georeferenced in the archaeological map that also allows diachronic analyses of the territory.
2019
38th International Mediterranean Survey Workshop - Groningen Institute of Archaeology, Friday 29 – Saturday 30 November 2019 The main aim of this paper is to present new data collected by the Ravenna Landscape Project, which was started as Decimano Project (2002-2005), to study the southern hinterland of Ravenna (Italy) using mainly artefact survey as method to document changes in settlement dynamics across time around this ancient capital. Afterwards, the Bassa Romandiola Project was started (2009-present), in the north-western part of Ravenna province. In 2019, a rebranding of the project was carried out to include two new subprojects that focus on the countryside around the cities of Cervia and Faenza. Major differences exist in this large study area, both on the historical level and in the physical landscape, that influence the methods to use and the interpretation of the results. Briefly: 1. Bassa Romagna is a low plain where no Roman towns are known; 2. Cervia is situated along the coastline, where a city arose between the V-VIII centuries CE; 3. Faenza was a Roman municipium born along the Via Aemilia, at the edge between the Apennines and the Po plain. The results of these two new subprojects, presented here, allowed to document several sites, ranging between the Bronze Age until the Modern Age showing different local settlement dynamics.