Figure 4. End moraine series in the Kichera River valley, northernmost Lake Baikal (after [Osadchii, 1989]): 1 - reliable (a) and tentative (b) boundaries of the maximum glaciation; 2 - stadial moraines preserved in the contemporary relief; 3 - alluvial-lacustrine plains in "flooded'' (a) and eroded (b) areas of stadial moraines; 4, 5 - glacial-lacustrine plains: dry (4) and swampy (5); 6 - lakes.