Figure 6. Long profile of the Tersky Keiva lateral moraines (bold lines) and their reconstructed continuations (dotted lines) between Ponoy River and Varzuga River. On the left, the Tersky Keiva moraine overlaps a lateral moraine of the Kandalaksha outlet glacier of the Scandinavian Ice Sheet. Note that the Tersky Keiva moraine is inclined in the NE-to-SW direction. Also note that the ice lobe was very thin, and its slope was extremely gentle.