Soil production limits and the transition to bedrock-dominated landscapes

Author:

Heimsath Arjun M.,DiBiase Roman A.,Whipple Kelin X.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference30 articles.

1. Ahnert, F. Brief description of a comprehensive three-dimensional process-response model of landform development. Z. Geomorph. N. F. 25, 29–49 (1976).

2. Anderson, R. S. & Humphrey, N. F. in Quantitative Dynamic Stratigraphy (ed. Cross, T. A.) 349–361 (Prentice-Hall, 1989).

3. Carson, M. & Kirkby, M. Hillslope Form and Process (Cambridge Univ. Press, 1972).

4. Heimsath, A. M., Dietrich, W. E., Nishiizumi, K. & Finkel, R. C. The soil production function and landscape equilibrium. Nature 388, 358–361 (1997).

5. Larsen, I. J., Montgomery, D. R. & Korup, O. Landslide erosion controlled by hillslope material. Nature Geosci. 3, 247–251 (2010).

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