Extended Data Fig. 9: Distribution characteristics of current isostatic uplift rates.
From: Recent uplift of Chomolungma enhanced by river drainage piracy
a-c, Current isostatic uplift rate due to non-steady incision for different elastic thicknesses (Te). d, Isostatic uplift rate profile along section x-x′ in panel a, showing the position of Chomolungma and Makalu.
