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The large fortifi cation of Corneşti-larcuri is located on the Mureş River in Romania and comprises four rings of defensive ramparts. With the outermost rampart encircling a total area of 17.65 km2, Corneşti-larcuri is thus considered the largest Bronze Age fortification in Europe. New intensive research began in 2007 with the six-year project “Investigations on settlement structures and the chronology of the Late Bronze Age fortification of Corneşti-larcuri in Romanian Banat”, funded by the German Research Foundation (DFG). The project terminated in the autumn of 2017. Now the goal is to evaluate the data collected during the last eleven years and to develop the first syntheses. As part of the new excavations, a total of 109 radiocarbon datings from diff erent contexts (ramparts, ditches, pits, house structures, etc.) were obtained. The subsequent phase model based upon these data essentially refers to the dating of ramparts I and II and to pits associated with house contexts. Thus, it enables a site biography for Corneşti-larcuri to be outlined for the first time and four settlement phases to be distinguished.
For the environs of the Late Bronze Age fortification enclosure Iarcuri the hydro-morphological relief characteristics are combined with archaeological evidences. Target of the study is to evaluate the impact of settlement activities in the surroundings of Iarcuri on the development of the channel network. Data analysis is based on topographic map-derived and high resolution DEMs provided by LiDAR scanning; derivatives of the DEMs are used to characterize the different sub-catchments that show varying influences by the fortification ramparts. The tributaries reaching the receiving stream close to the central settlement area source close to the gates in the ramparts in the Late Bronze Age built-up areas. Additionally, also the geometry of these tributaries differs from that of other tributaries. The distinct character of the channel network with repeatedly occurring rectangular bends indicates the capture of channels, which developed as gullies along paths by retrogressive erosion.