Extended Data Fig. 2: The relationship between valley-floor width and channel steepness, separated by tectono-stratigraphic unit. | Nature Geoscience

Extended Data Fig. 2: The relationship between valley-floor width and channel steepness, separated by tectono-stratigraphic unit.

From: Himalayan valley-floor widths controlled by tectonically driven exhumation

Extended Data Fig. 2

The relationship between valley-floor width and k_sn separated by each stratigraphic unit, coloured by elevation. LHS = Lesser Himalayan Sequence, GHS = Greater Himalayan Sequence, THS = Tethyan Himalayan Sequence, SHZ = Sub-Himalayan Zone. The dashed grey line shows a linear least-squares regression through the data in log-log space: the equation of the regression line, R2^ and p value (two-sided) are noted. LHS: R2^ = 0.37, p = 4.86 x 10-^145; GHS: R2^ = 0.25, p = 8.76 x 10-^146; THS: R2^ = 0.44, p = 1.63 x 10-^157; SHZ: R2^ = 0.35, p = 6.58x10-^57.

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