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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Coastal cliff retreat rates at Beit-Yannay, Israel, in the 20th century
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Coastal cliff retreat rates at Beit-Yannay, Israel, in the 20th century

机译:20世纪以色列Beit-Yannay的沿海悬崖撤退率

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Research indicates that the aeolianite (Kurkar) cliffs along the Israeli Mediterranean coastline have continuously retreated eastward during the last few decades. There seems to be no dispute among Earth scientists regarding the general trend of cliff retreat. However the majority of papers displaying cliff retreat rates are based upon comparison of aerial photographs. Their lack of advanced geometric measurement methods causes a high margin of error. Public attention is focused upon the Beit-Yannay coastal cliff since private homes are located along the southern section of the cliff crest. The current research compares the historic location of the cliff crest edge at Beit-Yannay as observed in a series of aerial photographs taken during the period 1918-2000. Quantitative measurement methods included applications of satellite geodesy and digital photogrammetry and mapping. Research results offer quantitative, consecutive and highly accurate data regarding retreat rates over a relatively long period of 82 years. It is concluded that: 1. Annual average cliff retreat rates of the cliff crest is 20 cm/year. 2. Categorization of the study time span reveals periods displaying varying retreat rates such as 27 cm/year during 1918-1946, 21 cm/year during 1946-1973 and 10 cm/year during 1973-2000. 3. Maximum retreat distances of the cliff crest, over the study period were found to be approximately 25 m along the northern, lowest section of the cliff. Minimum distances of 11 m were identified at the highest, southern section of the cliff. 4. The eolianite (Kurkar) cliffs along the Israeli Mediterranean coast throughout the 20th century have been an important source of sediment, contributing approximately 24 * 106 m3 of sediments to the sediment balance of Israeli beaches.
机译:研究表明,以色列地中海沿岸的风成岩(Kurkar)悬崖在过去的几十年中一直向东退缩。对于悬崖退缩的总体趋势,地球科学家之间似乎没有争议。但是,大多数显示悬崖退缩率的论文都是基于航拍照片的比较得出的。他们缺乏先进的几何测量方法会导致较高的误差范围。由于私人住宅位于悬崖顶的南部,因此公众的注意力集中在贝特-扬内沿海悬崖上。当前的研究比较了在1918-2000年期间拍摄的一系列航拍照片中观察到的Beit-Yannay悬崖顶边缘的历史位置。定量测量方法包括卫星测地学和数字摄影测量与制图的应用。研究结果提供了有关82年相对较长时间的退缩率的定量,连续且高度准确的数据。得出以下结论:1.悬崖顶的年平均悬崖撤退速率为20厘米/年。 2.研究时间跨度的分类显示出退缩率各不相同的时期,例如1918-1946年为27厘米/年,1946-1973年为21厘米/年,以及1973-2000年为10厘米/年。 3.在整个研究期间,沿着悬崖的北部最低部分发现悬崖顶峰的最大后退距离约为25 m。在悬崖的最高南部确定了11 m的最小距离。 4.整个20世纪,以色列地中海沿岸的风成岩(Kurkar)悬崖一直是沉积物的重要来源,为以色列海滩的沉积物平衡贡献了约24 * 106 m3的沉积物。

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