Zoom on the lower right part of the panorama, where boulders have migrated furthest away from the moraine. In this part, the illumination is ideal for making the ice tails easily visible. boulders are migrating roughly upwards (S) in this view, despite the glacier surface being inclined towards the N, i.e. towards the camera. The line of greatest slope can be inferred from the small groves caused by meltwater running towards and slightly to the right of the camera (2018).