Nature research paper: Medieval demise of a Himalayan giant summit induced by mega-landslide
Internal part of the breccia showing dyke injection of a fluid-rich phase that coloured the breccia and the post-injection multiple brittle to ductile faulting and shearing of this dyke and of its shoulders., Schematic section of the contact between the avalanche brecciatic deposit and the gneissic bedrock of the Seti valley flanks.
The gneiss-rich unit, which corresponds to local material dragged and entrained at the base of the avalanche, contained quantities of millimetric to submetric pieces of vegetal debris ) ripped from the sides of the valley and also whose density decreases rapidly away from the former valley wall.
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