Abstract
Sculpting of the Earth’s surface by flowing water is apparent even to a casual observer, yet we know surprisingly little in a quantitative way about how the process of erosion actually occurs over a wide range of length and time scales. Earth’s surface topography at any particular time represents the combined effects of tectonism on one hand, and erosion/depositional processes on the other. Given this situation, it makes sense to study erosion in settings where we can estimate the tectonic component of the topography.
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Weissel, J.K., Malinverno, A., Harding, D.J., Karner, G.D. (1995). Erosional Development of the Ethiopian Plateau of Northeast Africa from a Fractal Analysis of Topography. In: Barton, C.C., La Pointe, P.R. (eds) Fractals in Petroleum Geology and Earth Processes. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-1815-0_8
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