(Tables 1-2) Composition of red coloured tills from Schobuell, Schleswig-Holstein and Møn Island, Denmark

The stratigraphic position of the glacially transported 'Scholle' (large-size erratic block) at Schobüll near Husum (Schleswig-Holstein) is now considered to be Devonian rather than 'Rotliegendes'. The 'Scholle', consisting of red clay and dolomite, is overlain by red-colored till without any flint but with up to 90% carbonate clasts (containing 15% dolomite), which indicates an eastern Baltic origin. The relationship of the 'Scholle' with the glacial till also points to an eastern Baltic origin for it, with up to 1 000 km transport distance.

位于胡苏姆（石勒苏益格-荷尔斯泰因州）附近朔比勒（Schobüll）的冰川搬运型“Scholle”（大型漂砾），其地层归属目前被认定为泥盆纪，而非赤底统（Rotliegendes）。该“Scholle”由红色黏土与白云岩构成，其上覆为不含燧石但碳酸盐岩碎屑含量高达90%（其中白云岩占比15%）的红色冰碛物，该特征指示其物源来自波罗的海东部。“Scholle”与该冰碛物的共生关系同样佐证了其波罗的海东部的物源属性，其搬运距离可达1000千米。