GRAND MARAIS · Landscape evolution in the Grand Marais of Limagne (Puy-de-Dôme, France), from the Iron Age to modern times. An archaeological and paleoenvironmental study in a long-lasting perspective
6РП — Действия „Мария Кюри“
- Период
- 2007-12-17 → 2009-08-16
- Финансиране от ЕС
- 142 866 €
- Участници
- 1
- Схема
- EIF
Линиите свързват координатора с партньорите. За проекти отпреди 2014 г. CORDIS не винаги дава точни координати. Тези точки са на ниво град или държава.
Накратко на български
Еволюцията на ландшафта в района Гранд Маре във Франция се проследява от железната епоха до днес чрез археологически данни и инфрачервени анализи. Това помага да се разберат дългосрочните тенденции в застрояването и разпределението на влажните зони в територията.
Кратко обяснение, генерирано от езиков модел по текста на CORDIS. Оригиналът е по-долу.
Резултати накратко
Final Activity Report Summary - GRAND MARAIS (Landscape evolution (...) from the Iron Age to modern times. An archaeological and paleoenvironmental study in a long-lasting perspective)
The principal aim of the GRAND MARAIS project was to define landscape evolution, from the late Iron Age until modern times, of the Grand Marais of Limagne, in Puy-de-Dôme, France, a plain of 150 km2 area that is located east of the town of Clermont-Ferrand. In particular, the essential question of the heritages and long-term trends in territorial patterns was considered. Based on archaeological researches carried on during the last ten years, we could say that, since the end of the Bronze Age, this region was affected by a high density of population in the form of a scattered settlement, which reached its main extent at the beginning of the Roman period, i.e. during the first and second centuries A.D. The first step of the research consisted of the collection of all available documentary sources, such as cartography (modern and contemporary), aerial photography (panchromatic, colour and infrared) and archaeological data. All data were prepared, i.e. digitised and delocalised, in order to allow for their insertion into a geographic information system (GIS). Recent geomorphologic researches showed that the plain of Grand Marais of Limagne, whilst generally considered as a wet area on the whole, should more correctly be intended as a sort of a puzzle, in which different zones are distinguished by a different degree of humidity. Therefore, a crucial step of this research consisted in detecting and spatialising wetlands inside Grand Marais. This result was achieved by means of an infrared analysis, in collaboration with the department of mechanical and civil engineering, University of Modena and Reggio, Italy, combined with a regressive analysis, which was conducted on photographic and cartographic representations with particular reference to the 19th century cadastral maps. I afterwards searched for regular agrarian patterns in modern Grand Marais plain. This part of the analysis was carried out on the cartographic and photographic representations of this plain. In particular, I looked for regular patterns corresponding to Roman units. They were in fact likely to be the result of a planned intervention dating back to Roman times. For instance, this was the case of Roman centuriation, a regular organisation of the countries, generally carried out with the aim of land reclaiming in accordance with a grid having a side of about 710 m, which corresponded to 20 Roman actus. I tested the pertinence of many centurial grids, according to the variations of the Roman feet, in order to verify the possible existence of a centurial system in the Grand Marais plain. Finally, I found the possible pertinence of a grid of 710 m, irregularly attested in almost the entire plain, oriented north-south and east-west and materialised on the ground by roads, canals and boundaries. The pertinence of this regular agrarian pattern to the Roman period was tested on the basis of data resorting from archaeological excavations, with a particular attention to linear structures connected with territorial organisations, such as roads and ditches for drainage and irrigation purposes. Archaeological data seemed to confirm the existence of a main north-south and east-west orientation, compatible with the territorial pattern that was recognised on cartographic and photographic representations and dated back to Roman times. In this way, I demonstrated the pertinence of the territorial model called paysage de fondation for the Grand Marais plain, which was represented by a landscape regularly planned during Roman times. This model could be opposed to the one called paysage de formation, in which the territorial pattern would form progressively and independently from any form of regular planning. From the historical pertinence point of view, the hypothesis of a centurial system (model of paysage de fondation) organising, at least partially, the Grand Marais plain, was perfectly plausible and coherent with the important transformations after the Roman conquest of this region. The foundation of the town of Augustonemetum, today referred to as Clermont-Fd, and the concomitant reorganisation of the road network around Agrippas way at the beginning of the first century A.D. could have been accompanied by a radical reorganisation of the plain.
Текст от CORDIS, на английски · Данни: CORDIS, © Европейски съюз
Цел на проекта
The aim of the project is to reconstruct the landscape evolution of the Grand Marais of Limagne (Puy-de-Dôme, France), a km2 100 plain that is located East of the town of Clermont-Ferrand, in the very centre of the region of the Arvernes, one of the most important peoples of ancient Gaul. It is a region that, from the end of the Bronze Age, was interested by a high density of population and for a thriving economy, mainly based on agriculture, whose prosperity was guaranteed by the so-called dark earth (terres noires), legendary for its fertility. Until the end of the 1960s, this area was considerably conditioned by the instability of the river network, as it is attested by the written sources, so that the anthropic exploitation of this region was only possible through an incessant fight against the water.Understanding the form and the aspect of the drainage system implemented from the late Iron Age (III century B.C.), in a long-lasting perspective, is undoubtedly a key to understand the type and the extent o f the social interventions carried out on the environment in the different periods, from the Antiquity until today. In order to obtain this result, the existing documentation and the new data both, archaeological/topographical and paleo environmental, will be crossed within a GIS (Geographic Information System), in order to distinguish the different chronologies of ancient territorial assessments (cadastre grids), having often different orientation and metric module, and to propose a general pattern of lands cape evolution. It is worth mentioning that this project will have further practical outputs.In practice a sort of numeric georeferenced archive of all archaeological and paleo environmental data for the Grand Marais area will be created: it is going to be come an instrument of great utility to local administrations, in order to assure a territorial planning completely respectful of the Cultural and Natural Heritage.
Оригинален текст от CORDIS (на английски).
Участници
- UNIVERSITE BLAISE PASCAL · CLERMONT-FERRANDКоординаторНиво градФранция
Връзки
Данни: CORDIS, © Европейски съюз
