Fig. 4.

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Fig. 4. Lateral moraine valley (◊) at the almost 2 km broad Batura glacier in S-aspect. Debris supply derives mainly from the tributary valleys (←) and the resedimentation of slope moraines (Δ). In the background the Batura massiv (7885 m) is visible. Photo: L. Iturrizaga 29.09.2000.

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