Large meltstreams are a feature of Polarisbreen, extending for many kilometres down the middle of the glacier. As here on the east side of the glacier, they originate from saturated snow as slush flows (MH). |
Large meltstreams are a feature of Polarisbreen, extending for many kilometres down the middle of the glacier. As here on the east side of the glacier, they originate from saturated snow as slush flows (MH). |