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Observations of Coastal Landslide-Generated Tsunami Under an Ice Cover: The Case of Lac-des-Seize-iles, Quebec, Canada

机译:冰盖下沿海滑坡产生的海啸的观测:以加拿大魁北克Lac-des-Seize-iles为例

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On April 15 2014, a landslide occurred on the east shore of a lake in the municipality of Lac-des-Seize-iles, about 100 km north of Montreal, Quebec, Canada. The coastal landslide, with a length of 94 m and a width of 55 m, had a volume of about 30,500 m3 of sandy to gravelly till. It was likely triggered by a significant amount of water infiltration caused by a heavy rain coincident with an accelerated snow melt. The displaced mass spread on the lake floor and triggered a tsunami that broke and partly lifted the ice cover. Water and ice damaged several seasonal residences and boathouses on the periphery of the lake, in an area extending 450 m north and 500 m south of the landslide debris location. Observations on aerial photographs taken shortly after the event revealed the existence of radial structures on the ice cover in the affected area resulting from the evolution of the tsunami wave. Investigations carried out on east and west shores showed evidences of net marks on tree trunks explained by a maximum inundation height which can be as much as 1.8 m directly in front of the landslide position on the west shore.
机译:2014年4月15日,Lac-des-Seize-iles市的一个湖东岸发生了山体滑坡,位于加拿大魁北克省蒙特利尔以北约100公里处。长度为94 m,宽度为55 m的沿海滑坡具有约30,500 m3的沙质至砾石积土。这可能是由于大雨引起的大量水渗透以及雪融化的加速而触发的。流离失所的群众在湖面上蔓延,引发了海啸,海啸破裂并部分抬起了冰盖。水和冰破坏了湖外围的数个季节性住宅和船屋,该地区在滑坡残骸位置以北450 m和以南500 m处延伸。事件发生后不久对航空照片的观察表明,海啸波的演变导致受灾地区冰盖上存在放射状结构。在东西海岸进行的调查显示,树干上有网状痕迹的证据可以解释为最大淹没高度,直接淹没高度可以在西岸滑坡位置的正前方高达1.8 m。

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