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Fish tanks of eastern Crete (Greece) as indicators of the Roman sea level

机译:克里特岛东部(希腊)的鱼缸,作为罗马海平面的指示器

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The ancient fish tanks and fish traps of Crete are relics of the Roman domination of the island; they were usually constructed near the major urban centers of that period. The direct relationship of their various functional characteristics with past sea levels and the relatively accurate determination of their construction dates establish them as sensitive indicators of sea level change through space and time.The fish tanks presented in detail in this study, namely those of Matala, Chersonissos, Mochlos and Sitia and the fish trap in the gulf of Zakros, have all been reported, recorded and/or interpreted in regard to their operation by previous researchers. In the absence of a comprehensive interdisciplinary approach to the issue, uneven methodologies, inaccurate data and wrong measurements have led to erroneous conclusions about sea level during their operation and about the size and direction of vertical tectonic movements in eastern Crete during the Upper Holocene.The present study is based on a new underwater survey, in the course of which the architectural and functional features of the ancient constructions were reexamined precisely; their depth from modern sea level was measured and their relationship with coastal landforms, indicative of a past sea levels, was investigated.A review of their manner of operation and their modern submerged position allowed the definition of a Roman mean sea level 1.24 m ± 0.09 m below the present one. The submersion of the central and eastern parts of Crete - included in the same tectonic block with a total length of at least 150 km - at an average tectonic rate of 0.65 mm/year during the last 1900 ± 100 years occurred, as is shown by historical evidence, during a paroxysmal tectonic event, probably related to the strong earthquake of 1604.
机译:克里特岛的古代鱼缸和鱼塘是罗马统治该岛的遗迹;它们通常是在那个时期的主要城市中心附近建造的。它们的各种功能特性与过去的海平面的直接关系以及对它们的建造日期的相对准确的确定,使它们成为随时间和空间变化的海平面变化的敏感指标。本研究中详细介绍的鱼缸,即Matala, Chersonissos,Mochlos和Sitia以及Zakros海湾中的诱捕器都已被先前的研究人员报道,记录和/或解释过。在缺乏全面的跨学科研究方法的情况下,不统一的方法,不准确的数据和错误的测量结果导致关于操作期间的海平面以及上全新世期间克里特东部垂直构造运动的大小和方向的错误结论。目前的研究基于新的水下调查,在此过程中,对古代建筑的建筑和功能特征进行了精确的重新检查。他们测量了它们距现代海平面的深度,并研究了它们与沿海地貌之间的关系,表明过去的海平面。对其运行方式和现代水下位置的回顾使得可以定义罗马平均海平面1.24 m±0.09低于目前的米。克里特岛中部和东部的淹没-包括在同一构造块中,总长至少150 km-在过去的1900±100年中以0.65 mm /年的平均构造速率发生,如图所示。阵发性构造事件期间的历史证据,可能与1604年的强地震有关。

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