The depression of Ravni dabar with a mountain hut and the Čelina rock formation (914 m). Ravni dabar can be interpreted as an uvala, a karstic depression which is intermediate in size and shape between a doline and a polje, but differs from both in its evolution. The term is, however, disputed, as it is sometimes argued that the characteristics of uvalas are not specific enough to justify considering them a separate landform. Viewpoint: upslope from Dabarska kosa, panoramic view in E direction.