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Geomorphology of the Ceyhan River lower plain (Adana Region, Turkey)

机译:杰伊汉河下游平原的地貌(土耳其阿达纳地区)

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摘要

We present a geomorphological map (Main Map) of the lower plain of the Ceyhan River (Adana province, Turkey). Data from three field campaigns and remote sensing observations were managed in a GIS to produce a 1:25,000 scale map. The area, mostly formed by alluvial sediments, is characterized by intense fluvial dynamics with superimposed agricultural activity. Erosional processes prevail on rocky ridges partially bordering the plain on the north-eastern side. The alluvial plain is flanked by large alluvial fans on its eastern side, whereas the western limit consists of a smoothed and undistinguishable watershed. Alluvial and deltaic deposits close to the river mouth are bordered southward by nested coastal dunes, lagoons, swamps and marshes punctuating the coastal belt. This area was an important historical site, as documented by evidence of settlements from the Neolithic. The map is a useful tool to support further archaeological research.
机译:我们介绍了切汉河(土耳其阿达纳省)下平原的地貌图(主图)。在GIS中管理了来自三个野战活动和遥感观测的数据,以生成1:25,000比例尺的地图。该地区主要由冲积物形成,其特征是强烈的河流动力学和叠加的农业活动。在东北侧部分与平原接壤的岩石山脊上普遍存在侵蚀过程。冲积平原的东侧是大型冲积扇的侧面,而西部边界则由一个平滑且无法区分的分水岭组成。靠近河口的冲积和三角洲沉积物向南与嵌套的沿海沙丘,泻湖,沼泽和沼泽相连,刺穿了沿海带。正如新石器时代的定居证据所证明的那样,该地区是重要的历史遗址。该地图是支持进一步考古研究的有用工具。

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