首页> 外文期刊>Zeitschrift fur Geomorphologie >Effect of natural risk factors upon the evolution of Chalcolithic human settlements in Northeastern Romania (Valea Oii watershed). From ancient times dynamics to present days degradation
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Effect of natural risk factors upon the evolution of Chalcolithic human settlements in Northeastern Romania (Valea Oii watershed). From ancient times dynamics to present days degradation

机译:自然风险因素对罗马尼亚东北部(Valea Oii分水岭)的石器人类住区演变的影响。从远古时代到今天的退化

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This study concerns the analysis of the Valea Oii watershed and the dynamics of human settlement depending on the occurrence of natural risk factors and their evolution. These include climatic change fluctuations, and appearance of new hydrological resources like springs, from consequent landslides, the disappearance of forests as a direct effect from overexploitation of the land. Archaeological sites and current villages have been investigated, as well as their emplacement depending on natural hazards (such as floods, landslides and gully erosion). At the same time, we have also indexed the water sources which include streams, springs and man-made lakes. The first archaeological records date back to the Chalcolithic period. The entire catchment includes a total of 26 Chalcolithic archaeological sites which are continuously threatened by numerous natural or anthropic risks. The morpho-hydrographic, geologic, and pedologic particularities have determined an early occupation of the area situated in the upper part of the watershed. In ancient times, the lower sector of the valley and the floodplain was used for agricultural purpose or for pasturing. Throughout time, human settlements shifted gradually towards the lower area. This phenomenon was triggered by significant deforestation, which led to an extension of the pastures and of the agricultural land. In the modern period, most settlements moved towards areas that were submitted to flooding. This process was determined by the escalation of landslides and by gully erosion which began after deforestation. In order to protect the floodplain settlements, dams were built to reduce the effects of high waters. One of the main advantages of studying small catchments is that the results can be extrapolated for larger catchments (> 100 km(2)), the volume of analyzed data being smaller, but done with the same strictness. Therefore, the results of this study can surely provide important information and can save relevant archaeological and geographical data in a GIS which, in normal present conditions, would not be possible to be recovered in the future.
机译:这项研究涉及对Valea Oii流域的分析以及根据自然风险因素的发生及其演变而人类居住的动态。其中包括气候变化的波动,以及随之而来的滑坡引起的新的水文资源(如泉水)的出现,森林的消失是土地过度开发的直接影响。已对考古遗址和当前村庄以及根据自然灾害(例如洪水,山体滑坡和沟壑侵蚀)的位置进行了调查。同时,我们还索引了包括溪流,泉水和人造湖在内的水源。最早的考古记录可以追溯到石器时代。整个流域共有26个石器时代的考古遗址,这些遗址不断受到众多自然或人为危险的威胁。形态,水文,地质和生态的特殊性决定了流域上部地区的早期占领。在远古时代,山谷的下部和洪泛区被用于农业目的或牧场。长期以来,人类住区逐渐向较低地区转移。这种现象是由严重的森林砍伐引发的,这导致了牧场和农田的扩展。在现代时期,大多数定居点都移向了遭受洪灾的地区。这个过程是由滑坡的升级和毁林后开始的沟壑侵蚀所决定的。为了保护洪泛区居民区,修建了水坝以减少高水位的影响。研究小型流域的主要优势之一是,可以将结果推算到较大的流域(> 100 km(2)),分析的数据量较小,但是具有相同的严格性。因此,这项研究的结果肯定可以提供重要的信息,并且可以将相关的考古和地理数据保存在GIS中,而在正常的当前情况下,将来将无法恢复该数据。

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