“…There is a general trend from halloysite at depth towards kaolinite at the surface of profiles on residual rock materials (e.g., Eswaran and Wong, 1978;Calvert et al, 1980;Churchman and Gilkes, 1989;Churchman, 1990;Takahashi et al, 2001;Singer et al, 2004;Jongkind and Buurman, 2006). These studies together have covered a range of parent rock types and also climates, including tropical (Eswaran and Wong, 1978, and part of Churchman, 1990), temperate (Calvert et al, 1980;part of Churchman, 1990;Jongkind and Buurman, 2006), and Mediterranean, or xeric (Churchman and Gilkes, 1989;Takahashi et al, 2001;Singer et al, 2004). According to Papoulis et al (2004), these trends with depth were explained in the context of their morphological and compositional development sequence of halloysite and kaolinites.…”