首页> 外文期刊>Journal of Archaeological Science >Palaeoenvironments and palaeotopography of a multilayered city during the Etruscan and Roman periods: early interaction of fluvial processes and urban growth at Pisa (Tuscany, Italy)
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Palaeoenvironments and palaeotopography of a multilayered city during the Etruscan and Roman periods: early interaction of fluvial processes and urban growth at Pisa (Tuscany, Italy)

机译:伊特鲁里亚和罗马时期多层城市的古环境和古地形:比萨的河流过程和城市发展的早期相互作用(意大利托斯卡纳)

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A critical geoarchaeological approach, based on fully integrated archaeological, geomorphological and stratigraphic data, allowed for the identification of the palaeoenvironments, palaeotopography and urban growth patterns of Pisa (NW Italy) during the Etruscan (first half of the 5th century BC first half of the 1st century BC) and Roman (second half of the 1st century BC-2nd century AD) periods. This powerful methodology, based on aerial and satellite images, electrical resistivity tomography, LiDAR, and core analysis, led to the reconstruction of landscape evolution, highlighting human environment interactions. During the Etruscan and Roman periods, Pisa saw a fast urban expansion in a dense and unstable fluvial network. Wide portions of the city were characterised by poorly drained conditions until the 1st century AD, when the alluvial plain became well drained under increasing anthropogenic pressure (Roman Centuriatio). Poorly drained floodplains and channel-related backswamps represent the topographically lowest zones of the ancient Pisa. This city developed within an intricate pattern of palaeochannels, related to two main rivers: the palaeoAmo, which flowed in proximity of its present position, and the former palaeoSerchio river, known as Auser flowing in the northern part of the city. Since Etruscan times, a mounded relief was formed in the historical city centre of Pisa, becoming wider and more prominent (up to ca. 2 m a.s.l.) during the Roman period, concomitant with a southward rapid expansion of the urban tissue. Nevertheless, the urban growth patterns substantially followed the Etruscan city's fabric, with marked concentration of the urban structures (public and private buildings) and manufacturing sites on the northern relief, close to the Auser. The Auser River thus played a crucial role in the environmental and topographic evolution of the city area. (C) 2015 Elsevier Ltd. All rights reserved.
机译:基于完全综合的考古,地貌学和地层数据的一种关键的地质考古方法,可以识别出伊特鲁里亚(意大利西北部)(公元前5世纪上半叶)在比萨(意大利西北)的古环境,古地形和城市发展模式。公元前1世纪)和罗马(公元前1世纪下半叶至公元2世纪)时期。这种基于航空和卫星图像,电阻率层析成像,LiDAR和岩心分析的强大方法,导致了景观演化的重建,突出了人类与环境之间的相互作用。在伊特鲁里亚和罗马时期,比萨在密集而不稳定的河流网络中看到了快速的城市扩张。直到公元一世纪,冲积平原在不断增加的人为压力下变得排水良好(罗马世纪),该市的大部分地区的排水条件仍然很差。排水不畅的洪泛区和与河道有关的后沼泽代表了比萨的地形最低区域。这个城市以复杂的古河道模式发展,与两条主要河流有关:一条古河在其当前位置附近流动;另一条古河塞尔基奥河在城市的北部流淌,被称为阿瑟河。从伊特鲁里亚时代开始,在历史悠久的比萨市中心形成了一个丘陵式的浮雕,在罗马时期变得更宽,更显着(最高约2 m a.s.l.),伴随着城市组织向南的迅速扩张。尽管如此,城市的增长方式基本上遵循了伊特鲁里亚城市的结构,城市结构(公共和私人建筑)和制造场所集中在北部安塞特(Auser)附近。因此,阿瑟河在市区的环境和地形演变中起着至关重要的作用。 (C)2015 Elsevier Ltd.保留所有权利。

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