Detail of the strandlines, with pond containing suspended sediment and glacier margin in the background. Variations of the lake level are the result of changing subglacial or englacial runoff from the lake (photo M. Hambrey, 3.9.2007). |
Detail of the strandlines, with pond containing suspended sediment and glacier margin in the background. Variations of the lake level are the result of changing subglacial or englacial runoff from the lake (photo M. Hambrey, 3.9.2007). |