Figure 13. Neptunian dikes in the loose fluvial-glacial, lacustrine sand, gravel and in the lahar horizon on the northern Elbrus slope near the end of the Ulluchiran Glacier (Site 3 in Figure 1): (1) moraine; (2, 3) lahar material: (2) fine clastics, (3) large blocks; (4) bedded fluvioglacial sand and gravel; (5) large neptunian dikes in fissures and the direction of the displacement of the layers along the fissures; (6) neptunian dikes in thin fissures.