The role of rock mass strength in landscape evolution

The influence of crustal strength fields on the patterns and rates of fluvial incision

From:

Roy, S.G., Koons, P.O., Upton, P., Tucker, G.E. (2015). The influence of crustal strength fields on patterns and rates of fluvial incision. Journal of Geophysical Research: Earth Surface 120, 275-299, doi 10.1002/2014JF003281.

S.G. Roy (a), P.O. Koons (a), P. Upton (b,a), G.E. Tucker (c)

a Earth and Climate Sciences, University of Maine, 111 Bryand Global Sci. Ctr., Orono ME 04469

b GNS Science, PO Box 30368, Lower Hutt 5040, New Zealand

c Cooperative Institute for Research in Environmental Sciences (CIRES) and Department of Geological Sciences, University of Colorado, UCB 399 Boulder, CO 80309-0399

Video: erosion of fault with 30 degree dip angle

Abstract

Gradients in the bedrock strength field are increasingly recognized as integral to the rates and patterns of landscape evolution. To explore this influence, we incorporate data from fault strength profiles into a landscape evolution model, under the assumption that erodibility of rock is proportional to the inverse square root of cohesion for bedrock rivers incised by bedload abrasion. Our model calculations illustrate how patterns in the crustal strength field can play a dominant role in local fluvial erosion rates and consequently the development of fluvial network patterns. Fluvial incision within weak zones can be orders of magnitude faster than for resistant bedrock. The large difference in erosion rate leads to the formation of a straight, high order channel with short, orthogonal tributaries of low order. In comparison, channels incising into homogeneous strength fields produce dendritic drainage patterns with no directional dependence associated with erodibility gradients. Channels that cross the strength gradient experience local variations in knickpoint migration rate and the development of stationary knickpoints. Structurally confined channels can shift laterally if they incise into weak zones with a shallow dip angle, and this effect is strongly dependent on the magnitude of the strength difference, the dip angle, and the symmetry and thickness of the weak zone. The influence of the strength field on drainage network patterns becomes less apparent for erodibility gradients that approach homogeneity. There are multiple natural examples with drainage network patterns similar to those seen in our numerical experiments.