The end moraines in the Constance depression were formed along the edge of the ice during the Constance stage (see above). In the area of the old town of Constance, we find a moraine surrounded by Lake deposits. The section of the moraine in Kreuzlingen, however, is surrounded predominantly by Pleistocene talus. Sections of the end moraine are found further north east and south east, in the area of the Bodanrück and Seerücken, respectively. Sections od end moraine connecting these to the Constance section may have been eroded away, or they may never have existed due to water movement during the Constance stage.