A mixture of sediment directly deposited from the glacier (the hummocky terrain in the foreground) and stream-reworked sediment (forming the ridges on, and extending from, the ice) characterises the immediate proglacial zone of the glacier. |
A mixture of sediment directly deposited from the glacier (the hummocky terrain in the foreground) and stream-reworked sediment (forming the ridges on, and extending from, the ice) characterises the immediate proglacial zone of the glacier. |