Transition of a small Himalayan glacier lake outburst flood to a giant transborder flood and debris flow.

Results GLOF trigger and breach outflow The precipitation trend in the Zhangzangbo valley shows minimal rainfall at the beginning of June 2016 (pre-GLOF), but an increasing trend from mid-June with intense precipitation between June 29 to July 3 (2 days before the GLOF) (Fig. 4 a).

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The deposits show a clear trend when compared to the landslide density map calculated for the major (≥ M6) epicenters (epicenter and locations marked) of the Gorkha earthquake and its aftershocks (Fig. 1 b).

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