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Rapid soil production and weathering in the Southern Alps, New Zealand

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Figure

Fig. 4. (regime wherewithwS1). The transition from isotropic to anisotropic growth occurs at about 100 min
Fig. 1. Study sites. Location of the field area on New Zealand’s South Island (A), sample locations, and watershed scale denudation rates (T1 SE) (B).
Fig. 2. Soil production rates, chemical depletion data, and chemicalversus physical denudation rates.R(with a worldwide compilation of soil production functions; see supplementary ma-terials for data sources

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