With the undoubted exception of CBT and IPT, most of
the literature on termination derives from long - term work, particularly psychodynamic, which like systemic work is relationship based.
The glaciological community has for decades harbored the widespread belief that the thermal evolution of the ice sheet, and the effect of this evolution
on ice flow, are central in the ice - age cycling (not all communities agree, but there is plenty of
literature on this from the land - ice crowd), so use of a temperature - independent rheology for the ice leaves out one favored explanation for
termination of extensive glaciation.