“…). This syncline (axial surface dips to the SW, 200–250°/45–50°) is one of several large‐scale folds and associated thrusts that form an imbricate thrust stack, or duplex, deforming both the Upper Cretaceous (Maastrichtian) chalk bedrock and overlying unconsolidated Pleistocene glacigenic deposits (Credner, ; Gripp, ; von Bülow, ; Groth, ; Ludwig, ). The large‐scale and structural characteristics of the Jasmund thrust‐fold complex are comparable to many of the large glacitectonic complexes described in areas of former glaciated terrain, such as Møns Klint in south‐east Denmark (Pedersen, ; Pedersen and Gravesen, ; Pedersen, ).…”