“…Cooke (1970), for example, noted that the best-developed pavements in Chile occurred on the oldest and highest fluvial terraces. Pavement characteristics have been used to map a number of Quaternary surficial deposits, including alluvial fans (Shlemon, 1978;Christenson and Purcell, 1985;Al-Farraj and Harvey, 2000), stream terraces, shorelines and beach ridges (Sauer, Schellmann and Stahr, 2007;Al-Farraj, 2008), and lava flows (Wells et al, 1985;McFadden, Wells and Jercinovich, 1987;Williams and Zimbelman, 1994). Changes in the chemical composition of varnish and the presence of organic carbon in varnish coating gravel of pavements have been employed to estimate the age of the underlying materials on which the pavement formed (McFadden, Wells and Jercinovich, 1987;Dorn, 1988;Liu and Broecker, 2008).…”