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WCoE/IPL projects in West Africa: application of Landsat ETM plus and ASTER GDEM data in evaluating factors associated with long runout landslides in Benue hills, North-central Nigeria

机译:西非的WCoE / IPL项目:Landsat ETM plus和ASTER GDEM数据在评估与尼日利亚中北部Benue丘陵的长径滑坡相关的因素中的应用

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Under the WCoE/IPL project, Landsat Enhanced Thematic Mapper plus (ETM+) and ASTER GDEM data were used to analyze factors associated with frequent debris flow and rock-debris avalanche on the Nigeria-Cameroon mountain range. Detailed processing of the ETM+ imageries of the vulnerable portions on the western part of Adamawa plateau was carried out to identify structural trends relatable to the slope failures. The processing identified the structural characteristics of the study area and clearly distinguished the lineaments associated with the debris flow and rock-debris avalanches. The strongly weathered and fragmented gneissic rocks, shallow groundwater table, as well as the distribution of faults and joint sets were significant factors predisposing the slopes to rapid movements. Recent landslides occurred at the locations with high lineament density and in areas close to major faults and long lineaments. The interaction among the moving mass, slope geometry, local geology, topography, and drainage then resulted in a long runout and a high degree of spreading. Analysis of the ASTER-GDEM delineated landforms, slope morphology, and drainage patterns, which was not possible with conventional mapping techniques. Integration of these results yielded reasonable interpretation of the predisposing factors for the long runout failures and provided logical basis for future landslide susceptibility analysis in the area. Accurate investigation of the predisposing factors and characteristics of landslides in environments that have experienced past failures is therefore important in understanding areas that may be susceptible to landsliding in future.
机译:在WCoE / IPL项目下,Landsat增强主题地图器(ETM +)和ASTER GDEM数据用于分析与尼日利亚-喀麦隆山脉上频繁的泥石流和岩石碎屑雪崩相关的因素。对Adamawa高原西部脆弱部分的ETM +图像进行了详细处理,以确定与斜坡破坏有关的结构趋势。处理过程确定了研究区域的结构特征,并清楚地区分了与泥石流和岩石碎屑雪崩有关的构造。强烈风化和破碎的片麻质岩石,浅层地下水位以及断层和节理的分布是促使斜坡快速运动的重要因素。新近发生的滑坡发生在沿线高密度的地区以及靠近主要断层和沿线长的地区。移动质量,边坡几何形状,局部地质,地形和排水之间的相互作用导致了较长的跳动和高度的扩展。分析ASTER-GDEM描绘的地貌,坡度形态和排水模式,这是常规测绘技术无法实现的。综合这些结果可以合理解释长期跳动失败的诱因,并为该地区未来的滑坡敏感性分析提供逻辑依据。因此,在经历过以往破坏的环境中,对滑坡的诱发因素和特征进行准确的调查对于了解将来可能易发生滑坡的地区非常重要。

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