Mountain avens (Dryas octopetala)
Purple saxifrage
Fast sea ice in Eclipse Sound. The greenish-blue areas are interconnected ponds of surface meltwater
Fast se ice breaking up. The cracks are obvious -- and slabs are starting to drift apart, with patches of open water shown by the dark blue colour
A meltwater "fountain" on Fountain Glacier -- hence the name. Here the meltwater is not being forced out of an englacial tunnel under hydrostatic pressure; the fountain effect is created when surface meltwater flowing downslope on the glacier suddenly hits an obstacle and is forced into the air.
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Abandoned meltwater tunnel near the snout of Stagnation Glacier.
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Abandoned meltwater tunnel near the snout of Stagnation Glacier.
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Debris-stained rainwater which fell higher up the glacier and then found its way to the glacier bed, picking up sediment before issuing again at the snout. Fountain Glacier.
A large erratic block of gneiss, stranded in the middle of Fountain Glacier. Probably it has come down onto the glacier surface as part of a rockfall.
Courtesy the Glaciers Online web site.
https://www.swisseduc.ch/glaciers/bylot
https://www.swisseduc.ch/glaciers/bylot
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