CLAY MINERAL WEATHERING SEQUENCE IN A TROPICAL TERRACE PROGRESSION, COSTA RICA
Fluvial and marine terraces on the Pacific coast range in age from a lower limit of mid to late-Holocene (Pazzaglia et al., 1998) to an upper limit of 352 ka (Marshall et al., 2003). Given an uplift rate of 1m/ka (Fisher et al., 1998), terrace ages are as follows: Qt Z (approx. 210 masl) equals 220 ka; Qt Y (120-140 masl) equals125 ka; Qt X (50-80 masl) equals 75 ka; and Qt W (5 to10 masl) equals Holocene. Our estimates assume that the fill terraces formed during periods of relative high sea level associated with interglacial periods. Applying a parabolic diffusion limited model to weathering rind thicknesses studied by Sak et al. (2004) produces results consistent with our age estimates. Using the time constraints we will extrapolate rates of mineral formation and chemical evolution within the tropical terrace progression.
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