“…Dowdeswell et al (2008b) and Ottesen and Dowdeswell (2009). Establishing links between lithostratigraphy and glacial geomorphology requires identifying the genesis of the sedimentary signal, which is most easily accomplished in currently glaciated settings. Interpreting the ice influence on strata formation depends on recognizing distinctive lithofacies and/or seismic-facies assemblages characteristic of glacial settings (e.g., Svendsen et al, 1992;Faleide et al, 1996;Dowdeswell et al, 1998;Licht et al, 1999;Anderson et al, 2002;Powell and Cooper, 2002;McKay et al, 2009;Cowan et al, 2010;Dowdeswell and Fugelli, 2012;Hambrey and Glasser, 2012;Hogan et al, 2012;Kirshner et al, 2012;Dowdeswell et al, 2014;Larter et al, 2014;Rebesco et al, 2014). Many diagnostic lithofacies criteria for recognizing glacigenic processes depend on examination of clast fabric, grain orientation, physical properties, and biofacies (Powell, 1983;Powell and Molnia, 1989;Eyles and Eyles, 1992;Dowdeswell et al, 1998;Wellner et al, 2001;Cofaigh et al, 2007;Garcia et al, 2011;Cowan et al, 2012Cowan et al, , 2014Hambrey and Glasser, 2012;Kirshner et al, 2012;Larter et al, 2014).…”