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首页> 外文期刊>Landslides >Partial breaching of Hattian Bala Landslide Dam formed in the 8th October 2005 Kashmir Earthquake, Pakistan
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Partial breaching of Hattian Bala Landslide Dam formed in the 8th October 2005 Kashmir Earthquake, Pakistan

机译:于2005年10月8日在巴基斯坦克什米尔地震中形成的Hattian Bala滑坡大坝部分遭到破坏

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摘要

The 8th October 2005 Kashmir Earthquake of magnitude 7.6 triggered a huge landslide 3.5 km upstream of Hattian Bala town in the state of Azad Jammu Kashmir of Pakistan. The debris mass blocked two tributaries of the Karli branch of the Jhelum River and was breached on 9th February 2010. This debris dam provided us with a rare opportunity to keep careful and continuous eyes on its post-earthquake behavior especially as it was a serious threat to people living along the lower reaches of both the Karli and Jhelum Rivers. This paper describes post-formation behaviors of the debris mass, breaching-inflicted changes of not only the debris mass but also both upstream and downstream reaches based upon laser-scanned images of landforms and Differential Global Positioning System survey results.
机译:2005年10月8日,克什米尔大地震7.6在巴基斯坦Azad Jammu克什米尔邦Hattian Bala镇上游3.5公里处引发了巨大的山体滑坡。泥石流阻塞了耶鲁姆河卡利支流的两个支流,并于2010年2月9日被破坏。这座泥石坝为我们提供了难得的机会,可以持续不断地关注其震后行为,尤其是在严重威胁中居住在卡里河和耶鲁姆河下游的人们。本文基于激光扫描的地貌图像和差分全球定位系统的调查结果,描述了泥石块的形成后行为,泥石块的破坏引起的变化以及上游和下游河段的变化。

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