A significant contention in the recent literature on dwell fatigue has been the modified Stroh model, that dwell fatigue initiating facets form at the interface between 'hard' grains that are poorly oriented for slip and 'soft' grains that are well oriented for slip. It has then been suggested that regions of common orientation, termed macrozones, arising from the prior beta grains, will promote such nearest neighbour pairs and therefore promote dwell fatigue cracking. Here, by sectioning back from a dwell fatigue crack initiation site we observe just such an initiation at a macrozone boundary, whereas we do not observe low cycle fatigue crack initiation at macrozone boundaries.