Debris Flow Activity and Specific Features of Debris Flow Formation in the Geysernaya River Valley (Kamchatka)

IF 0.9 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
E. V. Lebedeva, S. S. Chernomorets
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Abstract

Debris flow activity in the Geysernaya River basin was mapped. Large-scale debris flow processes due to the collapse of fragments of the valley’s left wall were observed in this area three times over the past 40 years. Three independent debris flow areas of the river basin were identified and described: the upper reaches of the river, the Levaya Geysernaya basin; the middle reaches of the river, below the dammed lake that formed in 2014; and the lower downstream part, below the dammed lake that existed in 2007–2014. Debris flow processes are typical of most tributaries of the Geysernaya River. Moreover, debris flows can be aseasonal in the left tributaries, because they are formed under constant heating and active gas–hydrothermal influence within the thermal fields. The landslide dam formed in 2014 is resistant to erosion, and an independent outburst of the dammed lake is unlikely. With further erosion of the 2007 dam and expansion of the breach in the dam body, collapse of its sides and debris flow in the lower part of the Geysernaya River valley should not be ruled out. Risks of rockfall, landslide, and debris flow processes, most likely on the left wall of the valley, should be taken into consideration in planning the development of recreation facilities.

Abstract Image

盖谢尔纳亚河谷(堪察加半岛)的泥石流活动和泥石流形成的具体特点
摘要 绘制了盖谢尔纳亚河流域的泥石流活动图。在过去 40 年中,该地区观测到三次因山谷左壁碎片崩塌而造成的大规模泥石流过程。确定并描述了该流域三个独立的泥石流区域:河流上游,列瓦亚格耶瑟纳亚流域;河流中游,2014 年形成的堰塞湖下方;下游部分,2007-2014 年存在的堰塞湖下方。盖谢尔纳亚河的大部分支流都有典型的泥石流过程。此外,左侧支流的泥石流可能是季节性的,因为它们是在热场内持续加热和活跃的气体-水热影响下形成的。2014 年形成的滑坡坝具有抗侵蚀能力,坝上湖泊不太可能独立溃决。随着 2007 年大坝的进一步侵蚀和坝体缺口的扩大,不排除坝体两侧坍塌和盖瑟纳亚河谷下游泥石流的可能性。在规划娱乐设施的开发时,应考虑到落石、滑坡和泥石流过程的风险,这些风险最有可能发生在河谷左壁。
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来源期刊
Russian Journal of Pacific Geology
Russian Journal of Pacific Geology 地学-地球科学综合
CiteScore
1.30
自引率
37.50%
发文量
34
审稿时长
>12 weeks
期刊介绍: Russian Journal of Pacific Geology publishes the results of research on the Earth crust and mantle composition and provides articles on the geological structure and patterns of distribution of mineral deposits in the Pacific Ocean, marginal seas and continental margins. It discusses the topics of stratigraphy, sedimentology, magmatic activity, and seismicity. The journal deals with the problems of lithosphere plates tectonics, and offers the results of neotectonic, geomorphological, geodesic, environmental and mining studies in the Pacific region. The journal accepts theoretical, methodical and philosophical articles covering general issues of geology, geophysics, geochemistry, geoecology and mining. The journal also publishes critical notes and comments, and reviews.
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