The study looked at how a push-moraine was formed by the Scandinavian Ice Sheet on the Głubczyce Plateau in Poland. The researchers found that the glacial deposits were pushed in front of the advancing ice sheet due to the resistant bedrock underneath. The deformation of the sediments was caused by compression forces from the ice sheet moving against the sloped bedrock. The topography of the area influenced the distribution of the ice, with more ice flowing in lower lying areas. This study helps us understand how glaciers shape the landscape and how they respond to different geological features.