Hillslopes record the growth and decay of landscapes

Hurst, M.D.; Mudd, S.M.; Attal, M.; Hilley, G.. 2013 Hillslopes record the growth and decay of landscapes. Science, 341 (6148). 868-871. https://doi.org/10.1126/science.1241791

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Official URL: http://dx.doi.org/10.1126/science.1241791

Abstract/Summary

Earth's surface archives the combined history of tectonics and erosion, which tend to roughen landscapes, and sediment transport and deposition, which smooth them. We analyzed hillslope morphology in the tectonically active Dragon’s Back Pressure Ridge in California, United States, to assess whether tectonic uplift history can be reconstructed using measurable attributes of hillslope features within landscapes. Hilltop curvature and hillslope relief mirror measured rates of vertical displacement caused by tectonic forcing, and their relationships are consistent with those expected when idealizing hillslope transport as a nonlinear diffusion process. Hilltop curvature lags behind relief in its response to changing erosion rates, allowing growing landscapes to be distinguished from decaying landscapes. Numerical modeling demonstrates that hillslope morphology may be used to infer changes in tectonic rates.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1126/science.1241791
ISSN:	0036-8075
Date made live:	20 Sep 2013 14:16 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/503294

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.1126/science.1241791

ISSN:

0036-8075

Date made live:

20 Sep 2013 14:16 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/503294