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Abstract
Unlike most rocks, calcium carbonate at geothermal hotsprings grows at a visible rate, thus enabling a comparison between time-lapse photography, mathematical models and simulations of the growth dynamics. Nature abounds with beautiful and striking landscapes, but a comprehensive understanding of their forms requires examples where detailed comparisons can be made between theory and experiment. Geothermal hot springs1 produce some of the most rapidly changing terrestrial landscapes, with reported travertine (calcium carbonate) growth rates as high as 5 mm per day2,3,4. Unlike most landscapes, the patterns of which are the result of erosion processes on timescales of millions of years, the hot-spring depositional landscapes exhibit a spectacular cascade of nested ponds and terraces5, for which the origins and quantitative characterization have remained elusive. Here, we take advantage of this millionfold difference in geological timescale to present a novel combination of data from time-lapse photography, computer simulation and mathematical modelling that explains the emergence of the large-scale pond and terrace patterns, predicts and verifies the dynamics of their growth and shows that these patterns are scale invariant.Cite this article
Veysey II, J., Goldenfeld, N. Watching rocks grow. Nature Phys 4, 310–313 (2008). https://doi.org/10.1038/nphys911 