日本北阿尔卑斯四马大石岭岩崩分布与地形变化

H. Hata, C. Narama, K. Fukui
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摘要

Shirouma-Daisekkei是日本阿尔卑斯山三大雪区之一。每年有一万多名登山者经过这片雪原。登山者遭遇了落石和滑石的事故。2005年8月,沙库什戴克岩壁发生滑坡,造成2人受伤。2008年8月,雪区上部发生岩石滑移,造成2名登山者死亡(Kariya et al., 2008)。本研究在2014-2015年期间开展了野外调查,以了解Shirouma-daisekkei周围的岩崩、滑岩状况和地形变化。间隔摄像机显示,2014年,由于雪面下降,雪中出现了许多岩石碎片。另一方面,2015年6月以后岩壁产生了大量岩屑。截至9月底,积雪区岩石碎片(>30cm)总数为570块。岩屑分布具有局部性,反映了研究区局部地质特征的差异性。
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The distribution of rockfall and topographical change in Shirouma Daisekkei, the Northern Japanese Alps
Shirouma-Daisekkei is one of the three largest snow patches in the Japanese Alps. More than 10,000 climbers pass on the snow patch every year. The climbers have suffered accidents of rockfall and rock slip. In August 2005, rock slip at the rock wall of Shakushi-dake causes injured two people. In August 2008, rock slip at upper part of snow patch causes two climbers sacrificed (Kariya et al., 2008). In this study, we carried out field survey during 2014-2015, to clarify the state of rockfall and rock slip, and topographical change around Shirouma-daisekkei. Interval camera showed many rock fragments appeared from inside of snow emerged by declining snow surface in 2014. On the other hand, many rock fragments were produced from rock wall after June 2015. The total number of rock fragments (>30cm) is 570 on the snow patch at the end of September. The distribution of rock fragments is local, and reflected the differences in the local geological feature of this study area.
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