“…Dating techniques provide absolute chronologies and allow researchers to (i) model regional climate at a particular moment in time; (ii) compare regional and global glacier extents (Yi et al, 2005); and (iii) understand the duration of certain landscape formations from a geomorphological perspective. From the late twentieth century, new dating methods such as optically stimulated luminescence (OSL; e.g., Owen et al, 2002a;Spencer and Owen, 2004), cosmogenic radionuclide exposure (CRN; e.g., Owen et al, 2002b;Finkel et al, 2003;Owen et al, 2006), electron spin resonance (ESR; e.g., Yi et al, 2002;Zhou et al, 2002;Zhao et al, 2006), and accelerating mass spectrometry (AMS; e.g., Yi et al, 2004), have been refined and applied widely to dating glacial sediment.…”