Landslides, river incision and environmental change: the Ruzizi gorge in the Kivu Rift

Toussaint Mugaruka Bibentyo, A. Dille, Arthur Depicker, B. Smets, M. Vanmaercke, C. Nzolang, S. Dewaele, O. Dewitte
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Abstract

The understanding of the interplay between natural and human induced factors in the occurrence of landslides remains poorly constrained in many regions, especially in tropical Africa where data-scarcity is high. In these regions where population growth is significant and causes changes in land use/cover, the need for a sustainable management of the land is on the rise. Here, we aim to unravel the occurrence of landslides in the 40 km-long Ruzizi gorge, a rapidly incising bedrock river in the Kivu Rift in Africa that has seen its landscape disturbed over the last decades by the development of the city of Bukavu (DR Congo). Careful field observations, historical aerial photographs, satellite imagery and archive analysis are combined to produce a multi-temporal inventory of 264 landslides. We show that the lithological context of the gorge and its extremely high incision rate (> 20 mm year-1) during the Holocene explains the presence of a concentration of large landslides (up to 2 km²) of undetermined age (well before the first observations of 1959) whose occurrence is purely natural. They are mostly of the slide type and do not show morphologic patterns of recent activity. The landslides that occurred during the last 60 years are flow-like shallower slope failures of smaller size (up to 0.12 km²) and tend to disappear rather quickly (sometimes within a few years) from the landscape as a result of rapid vegetation growth, land reclamation and (human-induced) soil erosion. They are primarily related to threshold slopes and precipitation plays a frequent role in their onset. However, land use/cover changes also affect their occurrence. This study provides useful information for a more accurate evaluation of the landslide hazard in the area, particularly with respect to the growth of the city of Bukavu that has developed without the consideration of naturally instable slopes. It also stresses the need and added value of building accurate landslide inventories in data-scarce regions.

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滑坡、河流切割与环境变化:基伍裂谷中的鲁齐齐峡谷
在许多地区,特别是在数据严重缺乏的热带非洲,对发生山体滑坡的自然因素和人为因素之间相互作用的了解仍然很有限。在这些人口增长显著并导致土地利用/覆盖发生变化的区域,对土地可持续管理的需求正在增加。在这里,我们的目标是解开40公里长的Ruzizi峡谷山体滑坡的发生,Ruzizi峡谷是非洲基伍裂谷中一条快速上升的基岩河流,在过去的几十年里,由于布卡武(刚果民主共和国)城市的发展,它的景观受到了干扰。仔细的实地观察、历史航空照片、卫星图像和档案分析相结合,产生了264个滑坡的多时间清单。我们表明,峡谷的岩性背景及其在全新世期间的极高切割率(> 20毫米/年)解释了年龄未确定的大型滑坡(长达2公里)的集中存在(远早于1959年的第一次观测),其发生完全是自然的。它们大多为滑动型,不显示近期活动的形态模式。在过去60年里发生的滑坡是较小规模的流状浅坡破坏(最大0.12公里),由于植被快速生长、土地复垦和(人为引起的)土壤侵蚀,它们往往很快(有时在几年内)从景观中消失。它们主要与阈值坡度有关,降水在它们的发生中起着频繁的作用。然而,土地利用/覆盖的变化也会影响它们的发生。这项研究为更准确地评价该地区的滑坡危险提供了有用的资料,特别是关于布卡武市的发展,该城市的发展没有考虑到自然不稳定的斜坡。它还强调了在数据匮乏地区建立准确的滑坡清单的必要性和附加价值。
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