Figure 1. A, Potential for fluvial siliciclastic load as function of climate; B, Potential for fluvial dissolved load as a function of climate; C, Potential for peat formation as a function of climate; D, Potential for eolian transport as a function of climate; E, Formation of U.S. Department of Agriculture soil orders as a function of climate; and F, Climate classification based on the number of wet months per year. From Cecil and Dulong (2003). |