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The Nanga Parbat Haramosh massif (NPHM) is located in the western syntaxis of the India–Eurasia collision zone and is subject to erosion rates that are so extreme as to impact the isostatic equilibrium of the massif. In order to investigate the interaction between large scale tectonic forces and local isostatic processes, we employ a Rayleigh wave tomography method to measure phase velocities with...

Surface wave velocity structure of the western Himalayan syntaxis