Analysis of the characteristics and causes of ground fissures in Kenya rift region
The Kenya Rift valley is located in the middle section of the eastern branch of the Great Rift valley in East Africa. Modern tectonic movement and volcanic activity are intense, and it is a hotspot in current geological research.The rift zone has developed ground fissure disasters due to its unique...
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Language: | zho |
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Editorial Office of The Chinese Journal of Geological Hazard and Control
2021-12-01
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Series: | Zhongguo dizhi zaihai yu fangzhi xuebao |
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Online Access: | https://www.zgdzzhyfzxb.com/en/article/doi/10.16031/j.cnki.issn.1003-8035.2021.06-07 |
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author | Peng TAN Yang LIU Fuqiang JIANG Xinlan WEN Feiyong WANG Zhijie JIA |
author_facet | Peng TAN Yang LIU Fuqiang JIANG Xinlan WEN Feiyong WANG Zhijie JIA |
author_sort | Peng TAN |
collection | DOAJ |
description | The Kenya Rift valley is located in the middle section of the eastern branch of the Great Rift valley in East Africa. Modern tectonic movement and volcanic activity are intense, and it is a hotspot in current geological research.The rift zone has developed ground fissure disasters due to its unique geological structure background, rock and soil characteristics, and meteorological and hydrological conditions. In this paper, we have studied the geological environment background, plane characteristics and shallow section structure characteristics of ground fissures in rift valley area through data collection, detailed field geological surveytrenching, drilling and indoor geotechnical tests. Internal dynamic geological processes such as rift extension and volcanic activity are the controlling factors for the formation of ground fissures in this area; the loose and easily eroded soil on the shallow surface is the material basis for the formation of ground fissures; strong rainfall provides hydraulic power for the formation of ground fissure Conditions: The "soft-hard-soft" stratum structure provides a favorable accumulation place for water-erosive substances. Finally, we divide the formation and evolution process of ground fissures in the Kenya Rift Valley into three stages, the incubation stage, the expansion stage and the disaster stage. |
first_indexed | 2024-04-09T23:15:44Z |
format | Article |
id | doaj.art-d42117aba6334741a0b3beaee3cee69d |
institution | Directory Open Access Journal |
issn | 1003-8035 |
language | zho |
last_indexed | 2024-04-09T23:15:44Z |
publishDate | 2021-12-01 |
publisher | Editorial Office of The Chinese Journal of Geological Hazard and Control |
record_format | Article |
series | Zhongguo dizhi zaihai yu fangzhi xuebao |
spelling | doaj.art-d42117aba6334741a0b3beaee3cee69d2023-03-22T09:12:34ZzhoEditorial Office of The Chinese Journal of Geological Hazard and ControlZhongguo dizhi zaihai yu fangzhi xuebao1003-80352021-12-01326536210.16031/j.cnki.issn.1003-8035.2021.06-07202101009Analysis of the characteristics and causes of ground fissures in Kenya rift regionPeng TAN0Yang LIU1Fuqiang JIANG2Xinlan WEN3Feiyong WANG4Zhijie JIA5China Road and Bridge Corporation, Beijing 100011, ChinaCollege of Geological Engineering and Geomatics, Chang'an University, Xi'an, Shaanxi 710054, ChinaCCCC Railway Consultants Group Co. Ltd., Beijing 100088, ChinaChina Road and Bridge Corporation, Beijing 100011, ChinaCollege of Geological Engineering and Geomatics, Chang'an University, Xi'an, Shaanxi 710054, ChinaCollege of Geological Engineering and Geomatics, Chang'an University, Xi'an, Shaanxi 710054, ChinaThe Kenya Rift valley is located in the middle section of the eastern branch of the Great Rift valley in East Africa. Modern tectonic movement and volcanic activity are intense, and it is a hotspot in current geological research.The rift zone has developed ground fissure disasters due to its unique geological structure background, rock and soil characteristics, and meteorological and hydrological conditions. In this paper, we have studied the geological environment background, plane characteristics and shallow section structure characteristics of ground fissures in rift valley area through data collection, detailed field geological surveytrenching, drilling and indoor geotechnical tests. Internal dynamic geological processes such as rift extension and volcanic activity are the controlling factors for the formation of ground fissures in this area; the loose and easily eroded soil on the shallow surface is the material basis for the formation of ground fissures; strong rainfall provides hydraulic power for the formation of ground fissure Conditions: The "soft-hard-soft" stratum structure provides a favorable accumulation place for water-erosive substances. Finally, we divide the formation and evolution process of ground fissures in the Kenya Rift Valley into three stages, the incubation stage, the expansion stage and the disaster stage.https://www.zgdzzhyfzxb.com/en/article/doi/10.16031/j.cnki.issn.1003-8035.2021.06-07kenya rift valleyground fissuresflat profile characteristicsundercuttinggenetic mechanism |
spellingShingle | Peng TAN Yang LIU Fuqiang JIANG Xinlan WEN Feiyong WANG Zhijie JIA Analysis of the characteristics and causes of ground fissures in Kenya rift region Zhongguo dizhi zaihai yu fangzhi xuebao kenya rift valley ground fissures flat profile characteristics undercutting genetic mechanism |
title | Analysis of the characteristics and causes of ground fissures in Kenya rift region |
title_full | Analysis of the characteristics and causes of ground fissures in Kenya rift region |
title_fullStr | Analysis of the characteristics and causes of ground fissures in Kenya rift region |
title_full_unstemmed | Analysis of the characteristics and causes of ground fissures in Kenya rift region |
title_short | Analysis of the characteristics and causes of ground fissures in Kenya rift region |
title_sort | analysis of the characteristics and causes of ground fissures in kenya rift region |
topic | kenya rift valley ground fissures flat profile characteristics undercutting genetic mechanism |
url | https://www.zgdzzhyfzxb.com/en/article/doi/10.16031/j.cnki.issn.1003-8035.2021.06-07 |
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