Fig. 18

Geological profile through the north-western part of the study area on the Schesaplana sheet (see Fig. 4). The sketch shows the Vilan-Klus-thrust bringing a stack of Bündnerschiefer series towards the observer over the Ruchberg Formation, which is in unconformable sedimentary contact with the Eggberg Formation. Later doming of the Prättigau caused the upward bulging of the thrust plane. Note that the distal Ruchberg Formation is present at the Pligugg locality and the variegated marlstones were mapped at Alpe Gilieila